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<article xmlns:tp="http://www.plazi.org/taxpub" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" article-type="research-article" xml:lang="en">
  <front>
    <journal-meta>
      <journal-id journal-id-type="publisher-id">145</journal-id>
      <journal-id journal-id-type="index">urn:lsid:arphahub.com:pub:57116c35-e49b-50b9-b36f-df793733eb60</journal-id>
      <journal-title-group>
        <journal-title xml:lang="en">Swiss Journal of Palaeontology</journal-title>
        <abbrev-journal-title xml:lang="en">SJP</abbrev-journal-title>
      </journal-title-group>
      <issn pub-type="ppub">1664-2376</issn>
      <issn pub-type="epub">1664-2384</issn>
      <publisher>
        <publisher-name>Pensoft Publishers</publisher-name>
      </publisher>
    </journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.3897/sjp.145.196379</article-id>
      <article-id pub-id-type="publisher-id">196379</article-id>
      <article-categories>
        <subj-group subj-group-type="heading">
          <subject>Research Article</subject>
        </subj-group>
        <subj-group subj-group-type="scientific_subject">
          <subject>Dinosauria</subject>
        </subj-group>
        <subj-group subj-group-type="geological_era">
          <subject>Cretaceous</subject>
        </subj-group>
        <subj-group subj-group-type="geographical_area">
          <subject>China</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title>A new postcranial skeleton of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> (<tp:taxon-name><tp:taxon-name-part taxon-name-part-type="suborder" reg="Theropoda">Theropoda</tp:taxon-name-part></tp:taxon-name>, <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>) from the Jehol Biota of the Ningcheng Basin, Inner Mongolia, China</article-title>
      </title-group>
      <contrib-group content-type="authors">
        <contrib contrib-type="author" corresp="no">
          <name name-style="western">
            <surname>Yu</surname>
            <given-names>Dongxiang</given-names>
          </name>
          <uri content-type="orcid">https://orcid.org/0009-0002-9704-057X</uri>
          <xref ref-type="aff" rid="A1">1</xref>
          <xref ref-type="aff" rid="A2">2</xref>
          <role content-type="http://credit.niso.org/contributor-roles/writing-original-draft/">Writing - original draft</role>
          <role content-type="http://credit.niso.org/contributor-roles/writing-review-editing/">Writing - review and editing</role>
          <role content-type="http://credit.niso.org/contributor-roles/investigation/">Investigation</role>
          <role content-type="http://credit.niso.org/contributor-roles/validation/">Validation</role>
          <role content-type="http://credit.niso.org/contributor-roles/visualization/">Visualization</role>
        </contrib>
        <contrib contrib-type="author" corresp="no">
          <name name-style="western">
            <surname>Zhang</surname>
            <given-names>Honggang</given-names>
          </name>
          <uri content-type="orcid">https://orcid.org/0009-0008-2587-0770</uri>
          <xref ref-type="aff" rid="A3">3</xref>
          <role content-type="http://credit.niso.org/contributor-roles/writing-review-editing/">Writing - review and editing</role>
        </contrib>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="western">
            <surname>Zhou</surname>
            <given-names>Chang-Fu</given-names>
          </name>
          <email xlink:type="simple">zhoucf528@sdust.edu.cn</email>
          <uri content-type="orcid">https://orcid.org/0000-0002-3744-7573</uri>
          <xref ref-type="aff" rid="A1">1</xref>
          <role content-type="http://credit.niso.org/contributor-roles/conceptualization/">Conceptualization</role>
          <role content-type="http://credit.niso.org/contributor-roles/writing-original-draft/">Writing - original draft</role>
          <role content-type="http://credit.niso.org/contributor-roles/writing-review-editing/">Writing - review and editing</role>
          <role content-type="http://credit.niso.org/contributor-roles/data-curation/">Data curation</role>
          <role content-type="http://credit.niso.org/contributor-roles/funding-acquisition/">Funding acquisition</role>
          <role content-type="http://credit.niso.org/contributor-roles/investigation/">Investigation</role>
          <role content-type="http://credit.niso.org/contributor-roles/supervision/">Supervision</role>
          <role content-type="http://credit.niso.org/contributor-roles/validation/">Validation</role>
          <role content-type="http://credit.niso.org/contributor-roles/visualization/">Visualization</role>
        </contrib>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="western">
            <surname>Pei</surname>
            <given-names>Rui</given-names>
          </name>
          <email xlink:type="simple">peirui@ivpp.ac.cn</email>
          <uri content-type="orcid">https://orcid.org/0000-0002-5954-0728</uri>
          <xref ref-type="aff" rid="A4">4</xref>
          <role content-type="http://credit.niso.org/contributor-roles/conceptualization/">Conceptualization</role>
          <role content-type="http://credit.niso.org/contributor-roles/writing-original-draft/">Writing - original draft</role>
          <role content-type="http://credit.niso.org/contributor-roles/writing-review-editing/">Writing - review and editing</role>
          <role content-type="http://credit.niso.org/contributor-roles/data-curation/">Data curation</role>
          <role content-type="http://credit.niso.org/contributor-roles/funding-acquisition/">Funding acquisition</role>
          <role content-type="http://credit.niso.org/contributor-roles/investigation/">Investigation</role>
          <role content-type="http://credit.niso.org/contributor-roles/supervision/">Supervision</role>
          <role content-type="http://credit.niso.org/contributor-roles/validation/">Validation</role>
          <role content-type="http://credit.niso.org/contributor-roles/visualization/">Visualization</role>
        </contrib>
      </contrib-group>
      <aff id="A1">
        <label>1</label>
        <addr-line content-type="verbatim">College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, China</addr-line>
        <institution>College of Earth Science and Engineering, Shandong University of Science and Technology</institution>
        <addr-line content-type="city">Qingdao</addr-line>
        <country>China</country>
        <uri content-type="ror">https://ror.org/04gtjhw98</uri>
      </aff>
      <aff id="A2">
        <label>2</label>
        <addr-line content-type="verbatim">Hubei Qinglongshan National Nature Reserve of Dinosaur Egg Fossil Group, Shiyan, 442532, China</addr-line>
        <institution>Hubei Qinglongshan National Nature Reserve of Dinosaur Egg Fossil Group</institution>
        <addr-line content-type="city">Shiyan</addr-line>
        <country>China</country>
      </aff>
      <aff id="A3">
        <label>3</label>
        <addr-line content-type="verbatim">Paleontological Museum of Liaoning, Shenyang Normal University, Shenyang 110034, China</addr-line>
        <institution>Paleontological Museum of Liaoning, Shenyang Normal University</institution>
        <addr-line content-type="city">Shenyang</addr-line>
        <country>China</country>
        <uri content-type="ror">https://ror.org/04gtjhw98</uri>
      </aff>
      <aff id="A4">
        <label>4</label>
        <addr-line content-type="verbatim">Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, 100044, China</addr-line>
        <institution>Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences</institution>
        <addr-line content-type="city">Beijing</addr-line>
        <country>China</country>
        <uri content-type="ror">https://ror.org/034t30j35</uri>
      </aff>
      <author-notes>
        <fn fn-type="corresp">
          <p>Corresponding authors: Chang-Fu Zhou (<email xlink:type="simple">zhoucf528@sdust.edu.cn</email>); Rui Pei (<email xlink:type="simple">peirui@ivpp.ac.cn</email>)</p>
        </fn>
        <fn fn-type="edited-by">
          <p>Academic editor: Emanuel Tschopp</p>
        </fn>
      </author-notes>
      <pub-date pub-type="collection">
        <year>2026</year>
      </pub-date>
      <pub-date pub-type="epub">
        <day>02</day>
        <month>09</month>
        <year>2026</year>
      </pub-date>
      <volume>145</volume>
      <fpage>901</fpage>
      <lpage>926</lpage>
      <uri content-type="arpha" xlink:href="http://openbiodiv.net/FDC13B99-40DF-52DD-B6AC-C746E27B531D">FDC13B99-40DF-52DD-B6AC-C746E27B531D</uri>
      <uri content-type="zoobank" xlink:href="https://zoobank.org/08EC18A1-ED4E-4E88-B6BB-AA44FB6810FD">08EC18A1-ED4E-4E88-B6BB-AA44FB6810FD</uri>
      <history>
        <date date-type="received">
          <day>20</day>
          <month>04</month>
          <year>2026</year>
        </date>
        <date date-type="accepted">
          <day>04</day>
          <month>08</month>
          <year>2026</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>Dongxiang Yu, Honggang Zhang, Chang-Fu Zhou, Rui Pei</copyright-statement>
        <license license-type="creative-commons-attribution" xlink:href="http://creativecommons.org/licenses/by/4.0/" xlink:type="simple">
          <license-p>This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
        </license>
      </permissions>
      <self-uri content-type="zoobank" xlink:type="simple">https://zoobank.org/08EC18A1-ED4E-4E88-B6BB-AA44FB6810FD</self-uri>
      <abstract>
        <label>Abstract</label>
        <p>A new, well-preserved troodontid postcranial skeleton from the Jehol Biota of the Ningcheng Basin, Inner Mongolia, China, is described and assigned to <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> based on an autapomorphy: the presence of two pneumatic foramina on the lateral surface of the anterior cervical vertebrae. This specimen is inferred to be an adult based on the presence of an external fundamental system (<abbrev xlink:title="external fundamental system">EFS</abbrev>) in the ulna, as well as the complete fusion of the cervical neural arches and centra. This represents the first record of a troodontid dinosaur from the Jehol Biota in Inner Mongolia. The discovery of this new specimen reveals additional morphological details of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> and expands the paleogeographic range of this taxon. Notably, this new specimen bears a moderately developed pubic ambiens process, in contrast to the anteroposteriorly elongated condition in Late Cretaceous troodontids. This morphology may reflect an early evolutionary phase in the elongation of the ambiens process among troodontids and might suggest a comparatively constrained hindlimb locomotor capacity relative to that of their Late Cretaceous relatives. In addition, body size comparisons among deinonychosaurians reveal that dromaeosaurids exhibit much greater size disparity than troodontids, which may reflect greater diversity in dromaeosaurid locomotion, ecological niches, or growth strategies.</p>
      </abstract>
      <kwd-group>
        <label>Keywords</label>
        <kwd>Early Cretaceous</kwd>
        <kwd>Jehol Biota</kwd>
        <kwd>Ningcheng Basin</kwd>
        <kwd>postcranial skeleton</kwd>
        <kwd>
          <italic>
            <tp:taxon-name>
              <tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part>
            </tp:taxon-name>
          </italic>
        </kwd>
        <kwd>
          <tp:taxon-name>
            <tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part>
          </tp:taxon-name>
        </kwd>
      </kwd-group>
      <funding-group>
        <funding-statement>This work was supported by the International Partnership Program of Chinese Academy of Sciences (Grant no. 052GJHZ2024029GC), the Taishan Scholar Program of Shandong Province (Grant no. tstp20240514), and the National Natural Science Foundation of China (Grant nos. 42372031 and 42288201).</funding-statement>
      </funding-group>
    </article-meta>
  </front>
  <body>
    <sec sec-type="Introduction" id="sec1">
      <title>Introduction</title>
      <p><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name> is a clade of small- to medium-sized theropods, members of which are widely distributed in Cretaceous deposits across Asia and North America (<xref ref-type="bibr" rid="B20">Makovicky and Norell 2004</xref>). As some of the closest relatives of birds, troodontids play a crucial role in understanding the osteological transition from non-avialan dinosaurs to birds. In the last three decades, many exquisitely preserved troodontid fossils have been discovered in the Early Cretaceous Jehol Biota of northeastern China, including <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinusonasus">Sinusonasus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B53">Xu and Wang 2004</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Daliansaurus">Daliansaurus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B39">Shen et al. 2017b</xref>) from the Yixian Formation of western Liaoning; <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B14">Ji et al. 2005</xref>) from the Qiaotou Formation of Hebei Province; and potentially anchiornithines from the Tiaojishan Formation, whose phylogenetic position is still debated (<xref ref-type="bibr" rid="B32">Pei et al. 2017a</xref>, <xref ref-type="bibr" rid="B34">2020</xref>). These discoveries have greatly improved our understanding of troodontid evolution and the evolutionary origin of birds (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>, <xref ref-type="bibr" rid="B60">2017</xref>; <xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>). Among these taxa, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic>, one of the earliest-diverging troodontids (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>; <xref ref-type="bibr" rid="B35">Pei et al. 2021</xref>), is crucial for understanding the early evolution of troodontids because it possesses both troodontid synapomorphies and paravian plesiomorphies (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>; <xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>). However, previous studies of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> have predominantly focused on the cranium (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>; <xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>; <xref ref-type="bibr" rid="B62">Yu et al. 2024</xref>), whereas less attention has been paid to the morphology of the postcranial skeleton. <xref ref-type="bibr" rid="B65">Zhang et al. (2022)</xref> reported a new dinosaurian assemblage of the Jehol Biota from Ningcheng, Chifeng, Inner Mongolia, China (Fig. <xref ref-type="fig" rid="F1">1</xref>). Three eusauropod teeth and a symmetrodont mammal (<italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Ningchengodon">Ningchengodon</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="foxi">foxi</tp:taxon-name-part></tp:taxon-name></italic>) have been reported from this site (<xref ref-type="bibr" rid="B66">Zhang et al. 2024a</xref>, <xref ref-type="bibr" rid="B67">2024b</xref>). Most importantly, a troodontid postcranial skeleton (<abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062) was discovered in this assemblage and is described here in detail. It represents the first record of a Jehol troodontid from the Ningcheng Basin, Inner Mongolia. The discovery of this new specimen not only expands the geographic range of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> but also adds anatomical details to the postcranial osteology of this taxon.</p>
    </sec>
    <sec sec-type="materials|methods" id="sec2">
      <title>Material and methods</title>
      <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>, <xref ref-type="fig" rid="F5">5</xref>, <xref ref-type="fig" rid="F6">6</xref>, <xref ref-type="fig" rid="F7">7</xref>, <xref ref-type="fig" rid="F8">8</xref>, <xref ref-type="fig" rid="F9">9</xref>, <xref ref-type="fig" rid="F10">10</xref>, <xref ref-type="fig" rid="F11">11</xref>, <xref ref-type="fig" rid="F12">12</xref>, <xref ref-type="fig" rid="F13">13</xref>, <xref ref-type="fig" rid="F14">14</xref>) was collected from the fossil beds at Ningcheng, Chifeng, Inner Mongolia, during field expeditions in 2014. This specimen consists of an articulated and three-dimensionally preserved postcranial skeleton, including 10 cervical vertebrae, 9 dorsal vertebrae, and 16 caudal vertebrae; multiple rib fragments; partial left and right pectoral girdles and forelimbs; a partial right pelvic girdle; and nearly complete left and right hindlimbs.</p>
      <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 was prepared under a Leica M165C microscope using titanium-coated steel needles. The specimen was photographed using a Nikon D750 camera. The first seven cervical vertebrae were scanned using high-resolution X-ray computed tomography (<abbrev xlink:title="computed tomography">CT</abbrev>) at Zhejiang University with a Nikon XT H 320 device. No filters were applied during <abbrev xlink:title="computed tomography">CT</abbrev> scanning. A total of 2,501 TIFF slices, each 40 µm thick, were generated from <abbrev xlink:title="computed tomography">CT</abbrev> scans acquired at 90 kV and 297 μA. The 3D reconstruction was performed using VGSTUDIO MAX 3.0 (Volume Graphics, Heidelberg, Germany). Histological thin sections of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 were prepared in the histology laboratory of the Key Laboratory of Vertebrate Evolution and Human Origins, <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev>. Transverse sections 30 µm thick were taken from the right ulna (Fig. <xref ref-type="fig" rid="F2">2</xref>). They were photographed under normal and cross-polarized light using a Leica DM4 P microscope. A phylogenetic analysis was performed using TNT v. 1.5 (<xref ref-type="bibr" rid="B10">Goloboff et al. 2008</xref>; <xref ref-type="bibr" rid="B9">Goloboff and Catalano 2016</xref>). All images were processed using Photoshop CC 2018 (Adobe, California, USA). All anatomical terms for vertebral laminae and fossae follow the nomenclatural framework proposed by <xref ref-type="bibr" rid="B49">Wilson (1999)</xref> and <xref ref-type="bibr" rid="B50">Wilson et al. (2011)</xref>.</p>
      <sec sec-type="Institution abbreviations" id="sec3">
        <title>Institution abbreviations</title>
        <p><bold><abbrev xlink:title="Beijing Museum of Natural History (Beijing, China)">BMNHC</abbrev></bold>, Beijing Museum of Natural History (Beijing, China); <bold><abbrev content-type="institution" xlink:title="Dalian Natural History Museum (Dalian, China)">DNHM</abbrev></bold>, Dalian Natural History Museum (Dalian, China); <bold><abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev></bold>, Mongolian Institute of Geology (Ulaan Baatar, Mongolia); <bold><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev></bold>, Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China); <bold><abbrev content-type="institution" xlink:title="Long Hao Institute of Geology and Paleontology (Hohhot, China)">LH</abbrev></bold>, Long Hao Institute of Geology and Paleontology (Hohhot, China); <bold><named-content content-type="dwc:institutional_code" xlink:title="Museum of the Rockies" xlink:href="https://scientific-collections.gbif.org/institution/76111978-9203-46ba-96c7-61a87138c53a">MOR</named-content></bold>, Museum of the Rockies (Montana, USA); <bold><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev></bold>, Paleontological Museum of Liaoning (Shenyang, China); <bold><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev></bold>, Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China); <bold><abbrev content-type="institution" xlink:title="Shandong Tianyu Museum of Natural History (Linyi, China)">STM</abbrev></bold>, Shandong Tianyu Museum of Natural History (Linyi, China).</p>
      </sec>
    </sec>
    <sec sec-type="Systematic Paleontology" id="sec4">
      <title>Systematic Paleontology</title>
      <p>
        <bold><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="suborder" reg="Theropoda">Theropoda</tp:taxon-name-part></tp:taxon-name> Marsh, 1881</bold>
      </p>
      <p>
        <bold><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="infraorder" reg="Maniraptora">Maniraptora</tp:taxon-name-part></tp:taxon-name> Gauthier, 1986</bold>
      </p>
      <p>
        <bold><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name> Gilmore, 1924</bold>
      </p>
      <tp:taxon-treatment>
        <tp:treatment-meta>
          <kwd-group>
            <label>Taxon classification</label>
            <kwd>
              <named-content content-type="kingdom">Animalia</named-content>
            </kwd>
            <kwd>
              <named-content content-type="order">Saurischia</named-content>
            </kwd>
            <kwd>
              <named-content content-type="family">Troodontidae</named-content>
            </kwd>
          </kwd-group>
        </tp:treatment-meta>
        <tp:nomenclature>
          <tp:taxon-name><object-id content-type="arpha">77F36B80-FAF6-5FEF-94D8-BC2E137B5C43</object-id>
                		<tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part>
                	</tp:taxon-name>
          <tp:taxon-authority>Xu et al. 2002</tp:taxon-authority>
        </tp:nomenclature>
        <tp:treatment-sec sec-type="Holotype">
          <title>Holotype.</title>
          <p><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615, a disarticulated partial skull and partial skeleton.</p>
        </tp:treatment-sec>
        <tp:treatment-sec sec-type="Paratype">
          <title>Paratype.</title>
          <p><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583, an incomplete, articulated postcranial skeleton.</p>
        </tp:treatment-sec>
        <tp:treatment-sec sec-type="Referred specimens">
          <title>Referred specimens.</title>
          <p><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102, a partial skull and mandibles missing only the rostral portions, and six articulated cervical vertebrae (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>); <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V20378, a nearly complete skeleton (<xref ref-type="bibr" rid="B62">Yu et al. 2024</xref>); <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, a nearly complete, articulated postcranial skeleton (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>, <xref ref-type="fig" rid="F5">5</xref>, <xref ref-type="fig" rid="F6">6</xref>, <xref ref-type="fig" rid="F7">7</xref>, <xref ref-type="fig" rid="F8">8</xref>, <xref ref-type="fig" rid="F9">9</xref>, <xref ref-type="fig" rid="F10">10</xref>, <xref ref-type="fig" rid="F11">11</xref>, <xref ref-type="fig" rid="F12">12</xref>, <xref ref-type="fig" rid="F13">13</xref>, <xref ref-type="fig" rid="F14">14</xref>).</p>
        </tp:treatment-sec>
        <tp:treatment-sec sec-type="Locality and horizon">
          <title>Locality and horizon.</title>
          <p>All reported specimens of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> are recovered from Lujiatun, Shangyuan, Beipiao City, western Liaoning, China. <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>‑V1062 was discovered at the Duanjiagou site, Xidayingzi Village, Bisiyingzi Township, Ningcheng County, Chifeng City, Inner Mongolia, China, a new fossil site (Fig. <xref ref-type="fig" rid="F1">1</xref>). The absolute geological age has been constrained to 125.7 ± 1.5 Ma using U–Pb zircon dating analyzed by CA-ID-IRMS (<xref ref-type="bibr" rid="B19">Li et al. in press</xref>), and the lithological features of the fossil beds are also the same as those of the Lujiatun Unit of the Yixian Formation at Beipiao, western Liaoning, China (<xref ref-type="bibr" rid="B65">Zhang et al. 2022</xref>).</p>
          <fig id="F1">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure1</object-id>
            <object-id content-type="arpha">ABCC2426-A07B-5CA7-A484-98CCE823AEB0</object-id>
            <label>Figure 1.</label>
            <caption>
              <p>Area map showing the fossil locality of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in Duanjiagou, Xidayingzi, Bisiyingzi, Ningcheng, Chifeng, Inner Mongolia (red asterisk). The blue asterisk shows the main fossil-producing area of Jehol troodontids.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g001.jpg" id="oo_1763434.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763434</uri>
            </graphic>
          </fig>
        </tp:treatment-sec>
        <tp:treatment-sec sec-type="Description">
          <title>Description.</title>
          <p><bold><italic>Cervical vertebrate</italic></bold>. The cervical series is articulated and well exposed (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F3">3</xref>). The cervicodorsal transition can be clearly distinguished by the marked length disparity between the posteriormost cervical rib and the anteriormost dorsal rib. Considering that coelurosaurs typically possess 10 cervical vertebrae (<xref ref-type="bibr" rid="B32">Pei et al. 2017a</xref>; <xref ref-type="bibr" rid="B8">Gianechini et al. 2018</xref>), it is inferred that no vertebrae are missing and that all 10 cervical vertebrae are preserved in this specimen. The proatlas and most of the cervical vertebrae are completely preserved. The eighth cervical vertebra preserves only its posterior portion (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F3">3</xref>). The cervical vertebrae increase in length posteriorly, reaching their maximum length at the sixth vertebra, and then shorten posteriorly (Table <xref ref-type="table" rid="T1">1</xref>). The neural arches and centra are completely fused.</p>
          <fig id="F2">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure2</object-id>
            <object-id content-type="arpha">A894DF4B-2B8C-56BC-93BA-5C87C6A22131</object-id>
            <label>Figure 2.</label>
            <caption>
              <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in lateral view. <bold>A</bold>. Photograph; <bold>B</bold>. line drawing. The green arrow points to the sampling site for the histological thin section. Abbreviations: <abbrev xlink:title="axis">ax</abbrev>, axis; <abbrev xlink:title="cervical vertebrae">c</abbrev>, cervical vertebrae; <abbrev xlink:title="chevron">ch</abbrev>, chevron; <abbrev xlink:title="distal caudal vertebrae">dcv</abbrev>, distal caudal vertebrae; <abbrev xlink:title="dorsal rib">dr</abbrev>, dorsal rib; <abbrev xlink:title="dorsal vertebrae">dv</abbrev>, dorsal vertebrae; <abbrev xlink:title="left coracoid">lco</abbrev>, left coracoid; <abbrev xlink:title="left femur">lf</abbrev>, left femur; <abbrev xlink:title="left metatarsus">lmt</abbrev>, left metatarsus; <abbrev xlink:title="left pes">lpe</abbrev>, left pes; <abbrev xlink:title="left scapula">lsc</abbrev>, left scapula; <abbrev xlink:title="left tibiotarsus">lti</abbrev>, left tibiotarsus; <abbrev xlink:title="left ulna">lu</abbrev>, left ulna; <abbrev xlink:title="manual phalanx">m</abbrev>, manual phalanx; <abbrev xlink:title="pedal phalanx">p</abbrev>, pedal phalanx; <abbrev xlink:title="proximal caudal vertebrae">pcv</abbrev>, proximal caudal vertebrae; <abbrev xlink:title="right femur">rf</abbrev>, right femur; <abbrev xlink:title="right fibula">rfi</abbrev>, right fibula; <abbrev xlink:title="right humerus">rh</abbrev>, right humerus; <abbrev xlink:title="right ilium">ril</abbrev>, right ilium; <abbrev xlink:title="right ischium">ris</abbrev>, right ischium; <abbrev xlink:title="right metatarsus">rmt</abbrev>, right metatarsus; <abbrev xlink:title="right pubis">rpu</abbrev>, right pubis; <abbrev xlink:title="right radius">rra</abbrev>, right radius; <abbrev xlink:title="right scapula">rsc</abbrev>, right scapula; <abbrev xlink:title="right tibiotarsus">rti</abbrev>, right tibiotarsus; <abbrev xlink:title="right ulna">ru</abbrev>, right ulna; <abbrev xlink:title="sacral vertebrae">sv</abbrev>, sacral vertebrae.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g002.jpg" id="oo_1763435.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763435</uri>
            </graphic>
          </fig>
          <fig id="F3">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure3</object-id>
            <object-id content-type="arpha">B0AFA95A-F0D5-5B8D-BBB2-5A1CA1AD5105</object-id>
            <label>Figure 3.</label>
            <caption>
              <p>Cervical vertebrae and anterior dorsal vertebrae of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in lateral view. <bold>A, C</bold>. Photographs; <bold>B, D</bold>. line drawings. Abbreviations: <abbrev xlink:title="atlas">at</abbrev>, atlas; <abbrev xlink:title="axis">ax</abbrev>, axis; <abbrev xlink:title="cervical vertebrae">c</abbrev>, cervical vertebrae; <abbrev xlink:title="cervical rib">cr</abbrev>, cervical rib; <abbrev xlink:title="diapophysis">d</abbrev>, diapophysis; <abbrev xlink:title="depression">de</abbrev>, depression; <abbrev xlink:title="dorsal rib">dr</abbrev>, dorsal rib; <abbrev xlink:title="dorsal vertebrae">dv</abbrev>, dorsal vertebrae; <abbrev xlink:title="epipophysis">ep</abbrev>, epipophysis; <abbrev xlink:title="pleurocoel">pl</abbrev>, pleurocoel; <abbrev xlink:title="proatlas">pro</abbrev>, proatlas.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g003.jpg" id="oo_1763436.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763436</uri>
            </graphic>
          </fig>
          <table-wrap id="T1" position="float" orientation="portrait">
            <label>Table 1.</label>
            <caption>
              <p>Selected vertebral measurements of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (mm).</p>
            </caption>
            <table>
              <tbody>
                <tr>
                  <th rowspan="1" colspan="1">
                    <bold>Element</bold>
                  </th>
                  <th rowspan="1" colspan="1">
                    <bold>Value</bold>
                  </th>
                  <th rowspan="1" colspan="1">
                    <bold>Element</bold>
                  </th>
                  <th rowspan="1" colspan="1">
                    <bold>Value</bold>
                  </th>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Third cervical vertebra</td>
                  <td rowspan="1" colspan="1">16.0</td>
                  <td rowspan="1" colspan="1">Antepenultimate dorsal vertebra</td>
                  <td rowspan="1" colspan="1">17.0</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Fourth cervical vertebra</td>
                  <td rowspan="1" colspan="1">19.9</td>
                  <td rowspan="1" colspan="1">Penultimate dorsal vertebra</td>
                  <td rowspan="1" colspan="1">16.1</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Fifth cervical vertebra</td>
                  <td rowspan="1" colspan="1">28.0</td>
                  <td rowspan="1" colspan="1">Last dorsal vertebra</td>
                  <td rowspan="1" colspan="1">14.9</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Sixth cervical vertebra</td>
                  <td rowspan="1" colspan="1">28.3</td>
                  <td rowspan="1" colspan="1">Penultimate proximal caudal vertebra</td>
                  <td rowspan="1" colspan="1">17.0</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Seventh cervical vertebra</td>
                  <td rowspan="1" colspan="1">27.2</td>
                  <td rowspan="1" colspan="1">Last proximal caudal vertebra</td>
                  <td rowspan="1" colspan="1">19.7</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Ninth cervical vertebra</td>
                  <td rowspan="1" colspan="1">24.7</td>
                  <td rowspan="1" colspan="1">Fifth distal caudal vertebra</td>
                  <td rowspan="1" colspan="1">24.2</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Tenth cervical vertebra</td>
                  <td rowspan="1" colspan="1">24.6</td>
                  <td rowspan="1" colspan="1">Sixth distal caudal vertebra</td>
                  <td rowspan="1" colspan="1">26.0</td>
                </tr>
              </tbody>
            </table>
            <table-wrap-foot>
              <fn>
                <p>For all vertebrae, the measured length extends either from the prezygapophysis to the postzygapophysis or from the prezygapophysis to the posterior articular facet of the centrum.</p>
              </fn>
            </table-wrap-foot>
          </table-wrap>
          <p>The proatlas consists of two subtriangular, plate-like elements (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F3">3</xref>). The left element taphonomically overlies the right element on its anterodorsal side. Both elements are unfused (Fig. <xref ref-type="fig" rid="F3">3</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tsaagan">Tsaagan</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B25">Norell et al. 2006</xref>). The proatlas is dorsoventrally tall, similar to that in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tsaagan">Tsaagan</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B25">Norell et al. 2006</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Archaeopteryx">Archaeopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B27">O’Connor et al. 2025</xref>), but the caudodorsal expansion present in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Archaeopteryx">Archaeopteryx</tp:taxon-name-part></tp:taxon-name></italic> is absent in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. The proatlas is slightly deflected laterally. The medial surface of the proatlas is concave, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tsaagan">Tsaagan</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B25">Norell et al. 2006</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Archaeopteryx">Archaeopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B27">O’Connor et al. 2025</xref>). Ventrally, the proatlas articulates with the atlantal intercentrum. Within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>, the proatlas has only been reported in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>).</p>
          <p>The atlas comprises an intercentrum, a centrum, and two neural arches. The atlantal intercentrum is U-shaped in anterior view (Suppl. material <xref ref-type="supplementary-material" rid="S1">1</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>). The atlantal centrum, namely the odontoid, is co-ossified with the axis. The odontoid is oval and wider than tall in anterior view (Suppl. material <xref ref-type="supplementary-material" rid="S1">1</xref>). As in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>), the neural arch is triradiate in lateral view (Fig. <xref ref-type="fig" rid="F3">3</xref>). The postzygapophysis extends posteriorly and articulates with the axis (Fig. <xref ref-type="fig" rid="F3">3</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>). No remains of atlantal ribs could be observed.</p>
          <p>The axis is poorly preserved anteriorly. Preservation limitations preclude definitive confirmation of pneumatic foramina on the lateral surfaces of the centrum. The posterior articular facet of the centrum is slightly concave. The postzygapophysis is elongated. The epipophysis is blunt and extends posterolaterally, but not beyond the posterior margin of the postzygapophysis. This condition is similar to that of some troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>), and some dromaeosaurids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mahakala">Mahakala</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B44">Turner et al. 2011</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Buitreraptor">Buitreraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B8">Gianechini et al. 2018</xref>). In contrast, the epipophysis extends beyond the posterior margin of the postzygapophysis in some dromaeosaurids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Deinonychus">Deinonychus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B28">Ostrom 1969</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tsaagan">Tsaagan</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B25">Norell et al. 2006</xref>). The neural spine is high and plate-like, with its posterior edge being almost vertical (Fig. <xref ref-type="fig" rid="F3">3</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>). Unlike in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), the posterodorsal portion of the neural spine does not extend posteriorly in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. The neural spine is slightly expanded bilaterally along its dorsal margin (Fig. <xref ref-type="fig" rid="F3">3</xref>). A pair of spinopostzygapophyseal laminae are well developed, diverge posterolaterally from the base of the neural spine, and bound the spinopostzygapophyseal fossa.</p>
          <p>The postaxial centra are generally rectangular in lateral view (Fig. <xref ref-type="fig" rid="F3">3</xref>). The neural arches display an X-shaped profile in dorsal view. This profile is a common feature in paravians and is formed by the prezygapophyses and postzygapophyses extending anterolaterally and posterolaterally, respectively. In lateral view, the centra of the axis and the third and fourth cervical vertebrae extend posteriorly beyond the posterior margin of the neural arches (Figs <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>). This condition differs from that of dromaeosaurids, in which the centrum is level with or ends anterior to the posterior margin of the neural arch (<xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>).</p>
          <p>The third cervical vertebra is well preserved (Figs <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>). The ventral surface of the centrum is smooth (Fig. <xref ref-type="fig" rid="F4">4D</xref>). The lateral surface of the centrum bears two oval pneumatic foramina (pleurocoels; <xref ref-type="bibr" rid="B4">Currie and Dong 2001</xref>; <xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>; <xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>) (Fig. <xref ref-type="fig" rid="F4">4A, B</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>). These foramina are posteroventral and posterior to the diapophysis, respectively. As in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Paleontological Museum of Liaoning (Shenyang, China)">PMOL</abbrev>-AD00102 (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>), a depression is present and positioned more posteroventrally than the pneumatic foramina (Fig. <xref ref-type="fig" rid="F4">4A, B</xref>). The parapophysis is short and thick and is located at the anteroventral corner of the centrum (Fig. <xref ref-type="fig" rid="F4">4A, B</xref>). The articular facet of the parapophysis is oval and concave. The anterior articular facet of the centrum is saddle-like and transversely concave in ventral view (Fig. <xref ref-type="fig" rid="F4">4D, E</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Deinonychus">Deinonychus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B28">Ostrom 1969</xref>) and the troodontid <abbrev content-type="institution" xlink:title="Long Hao Institute of Geology and Paleontology (Hohhot, China)">LH</abbrev> PV39 (<xref ref-type="bibr" rid="B47">Wang et al. 2021</xref>). The posterior articular facet of the centrum is slightly concave and posteroventrally inclined (Fig. <xref ref-type="fig" rid="F4">4F</xref>). The prezygapophysis is large, and its articular facet slopes anteroventrally and articulates with the postzygapophysis of the axis (Figs <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>). The epipophysis is well developed and does not extend beyond the posterior margin of the postzygapophysis (Fig. <xref ref-type="fig" rid="F4">4B</xref>), as in the axis. The diapophysis is triangular in lateral view and located on the posteroventral side of the prezygapophysis (Fig. <xref ref-type="fig" rid="F4">4A, B</xref>). The neural spine is plate-like. Dorsally, the spine is damaged but has left a subrectangular impression in the matrix (Figs <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>). The area of the neural spine of the third cervical vertebra is smaller than that of the axis, as in other troodontids (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>; <xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>; <xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). Spinopostzygapophyseal and spinoprezygapophyseal laminae are present and diverge posterolaterally and anterolaterally from the base of the neural spine, respectively (Fig. <xref ref-type="fig" rid="F4">4E, F</xref>). The area of the spinopostzygapophyseal fossa is larger than that of the spinoprezygapophyseal fossa (Fig. <xref ref-type="fig" rid="F4">4E, F</xref>).</p>
          <fig id="F4">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure4</object-id>
            <object-id content-type="arpha">C4D81FD6-C960-579A-810D-7BC5EDA9F620</object-id>
            <label>Figure 4.</label>
            <caption>
              <p><abbrev xlink:title="computed tomography">CT</abbrev>-rendered images of cervical vertebrae 3 <bold>A–F</bold>. and 4 <bold>G–L</bold>. of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. <bold>A, B, G, H</bold>. Lateral views; <bold>C, I</bold>. dorsal views; <bold>D, J</bold>. ventral views; <bold>E, K</bold>. anterior views; <bold>F, L</bold>. posterior views. Abbreviations: <abbrev xlink:title="anterior articular facet of the centrum">aaf</abbrev>, anterior articular facet of the centrum; <abbrev xlink:title="diapophysis">d</abbrev>, diapophysis; <abbrev xlink:title="depression">de</abbrev>, depression; <abbrev xlink:title="epipophysis">ep</abbrev>, epipophysis; <abbrev xlink:title="parapophysis">pa</abbrev>, parapophysis; <abbrev xlink:title="posterior articular facet of the centrum">paf</abbrev>, posterior articular facet of the centrum; <abbrev xlink:title="pleurocoel">pl</abbrev>, pleurocoel; <abbrev xlink:title="postzygapophysis">po</abbrev>, postzygapophysis; <abbrev xlink:title="postzygodiapophyseal lamina">podl</abbrev>, postzygodiapophyseal lamina; <abbrev xlink:title="prezygapophysis">pr</abbrev>, prezygapophysis; <abbrev xlink:title="prezygodiapophyseal lamina">prdl</abbrev>, prezygodiapophyseal lamina; <abbrev xlink:title="neural spine">s</abbrev>, neural spine; <abbrev xlink:title="spinopostzygapophyseal fossa">spof</abbrev>, spinopostzygapophyseal fossa; <abbrev xlink:title="spinopostzygapophyseal laminae">spol</abbrev>, spinopostzygapophyseal laminae; <abbrev xlink:title="spinoprezygapophyseal fossa">sprf</abbrev>, spinoprezygapophyseal fossa; <abbrev xlink:title="spinoprezygapophyseal laminae">sprl</abbrev>, spinoprezygapophyseal laminae.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g004.jpg" id="oo_1763437.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763437</uri>
            </graphic>
          </fig>
          <p>The fourth cervical vertebra is well preserved (Figs <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F4">4</xref>) and is clearly slightly longer than the third cervical vertebra (Table <xref ref-type="table" rid="T1">1</xref>). Two oval pneumatic foramina and a depression occur on the lateral surface of the centrum, and their positions and morphologies are similar to those of the third cervical vertebra (Fig. <xref ref-type="fig" rid="F4">4G, H</xref>). The parapophysis is short, and its articular facet is subcircular (Fig. <xref ref-type="fig" rid="F4">4G</xref>). As in the third cervical vertebra, the anterior articular facet of the centrum is saddle-like, and the posterior articular facet is shallowly concave (Fig. <xref ref-type="fig" rid="F4">4K, L</xref>). The prezygapophysis and postzygapophysis show comparable lateral extension (Fig. <xref ref-type="fig" rid="F4">4I</xref>). The diapophysis is located on the lateral side of the neural arch and projects lateroventrally (Fig. <xref ref-type="fig" rid="F4">4G</xref>). Ventrally, the prezygapophysis bears a prezygodiapophyseal lamina that extends posteroventrally to connect with the diapophysis (Fig. <xref ref-type="fig" rid="F4">4G, H</xref>). A postzygodiapophyseal lamina is also developed between the postzygapophysis and the diapophysis. The epipophysis is slightly shorter than that of the third cervical vertebra. The neural spine is subrectangular in lateral view, and its anteroposterior length is greater than that of the third cervical vertebra. As in the third cervical vertebra, the spinopostzygapophyseal and spinoprezygapophyseal fossae are also developed (Fig. <xref ref-type="fig" rid="F4">4K, L</xref>).</p>
          <p>The fifth cervical vertebra is poorly preserved, and its neural spine is heavily damaged (Fig. <xref ref-type="fig" rid="F3">3</xref>). This cervical vertebra is elongate and is 1.4 times the length of the fourth cervical vertebra (Table <xref ref-type="table" rid="T1">1</xref>). The prezygapophysis is more developed than that of the fourth cervical vertebra, whereas the postzygapophysis is subequal in size to that of the fourth cervical vertebra.</p>
          <p>The sixth cervical vertebra is the longest vertebra in the cervical series (Table <xref ref-type="table" rid="T1">1</xref>). The anterior portion of the centrum is poorly preserved, and the parapophysis is missing (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). The ventral surface of the centrum is smooth, without the ventral keel seen in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B37">Russell and Dong 1993</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Troodon">Troodon</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B20">Makovicky and Norell 2004</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B23">Norell and Hwang 2004</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>; <xref ref-type="bibr" rid="B47">Wang et al. 2021</xref>). Posteriorly, the centrum exceeds the posterior end of the postzygapophysis (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). Owing to preservation limitations, only a suboval pneumatic foramen is visible on the lateral surface of the centrum (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). An oval depression is also present posteroventral to the pneumatic foramen (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>), as in the third and fourth cervical vertebrae. The prezygapophyseal articular facet is ovoid, faces anterodorsally, and slopes slightly medially. The postzygapophysis is comparable to the prezygapophysis in size (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>) and bears a weakly developed epipophysis dorsally. The diapophysis is located more anteriorly on the neural arch and extends laterally (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>) and the troodontid <abbrev content-type="institution" xlink:title="Long Hao Institute of Geology and Paleontology (Hohhot, China)">LH</abbrev> PV39 (<xref ref-type="bibr" rid="B47">Wang et al. 2021</xref>). As in the fourth cervical vertebra, the pre- and postzygodiapophyseal laminae are also developed. The neural spine is damaged dorsally and is located between the pre- and postzygapophyses (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>).</p>
          <p>The seventh cervical vertebra is preserved in its entirety (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). This vertebra is slightly shorter than the sixth cervical vertebra. Ventrally, the centrum bears a pair of weakly developed carotid processes between the parapophyses, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B4">Currie and Dong 2001</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Troodon">Troodon</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B20">Makovicky and Norell 2004</xref>). The shape and location of the pneumatic foramen and depression are similar to those of the sixth cervical vertebra, but the depression is slightly larger and deeper (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). The parapophysis is located at the anteroventral corner of the lateral side of the centrum and articulates with the cervical rib (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). The prezygapophysis is weakly developed and directed more dorsally than that of the sixth cervical vertebra, and the postzygapophysis extends posteriorly beyond the posterior margin of the centrum (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). The diapophysis is posterodorsal to the parapophysis. This diapophyseal location is comparable to that of the sixth cervical vertebra, but the process extends more ventrally than in the latter (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>). The pre- and postzygodiapophyseal laminae are developed between the diapophysis and the pre- and postzygapophyses, respectively. The neural spine is plate-like, and its anterior margin slopes slightly anteroventrally in lateral view (Fig. <xref ref-type="fig" rid="F3">3A, B</xref>).</p>
          <p>Only the posterior margin of the eighth cervical vertebra is preserved (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). A depression is present on the lateral surface of the centrum and is shallower than those of the preceding cervical vertebrae. The posterior articular facet of the centrum is exposed and relatively flat. The postzygapophysis extends beyond the posterior margin of the centrum.</p>
          <p>The ninth cervical vertebra is exposed on its right side (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). In lateral view, the centrum is subrectangular and ventrally concave. The parapophysis is located on the anterior side of the centrum and articulates with the corresponding rib. The pneumatic foramen of the centrum is obscured by the associated rib. The anterior articular facet of the centrum is flat. The prezygapophysis is short, approximately half the anteroposterior length of the postzygapophysis. The diapophysis is stout and lies posterodorsal to the parapophysis (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B51">Xu 2002</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>). The neural spine is reduced and much lower than those of the anterior cervical vertebrae (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>).</p>
          <p>The tenth cervical vertebra is subequal in length to the ninth cervical vertebra. The prezygapophysis is short, and the postzygapophysis is elongated (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The diapophysis also lies posterodorsal to the parapophysis and extends laterally and slightly posteriorly. Its neural spine and centrum are comparable in morphology to those of the ninth cervical vertebra.</p>
          <p><bold><italic>Dorsal vertebrae</italic></bold>. The anterior four and the last five vertebrae of the dorsal series are preserved (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F3">3</xref>, <xref ref-type="fig" rid="F5">5</xref>). The anterior four dorsal vertebrae articulate with the cervical series, and the third and fourth dorsal vertebrae are severely damaged (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The last five dorsal vertebrae are exposed on the right side, and the last three dorsal vertebrae are relatively well preserved (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F5">5</xref>). As in the cervical series, the neural arches are fully fused to their respective centra in the dorsal vertebrae.</p>
          <fig id="F5">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure5</object-id>
            <object-id content-type="arpha">F67DD7C5-E3C6-59D4-AF04-921B48F460F0</object-id>
            <label>Figure 5.</label>
            <caption>
              <p>Posterior dorsal vertebrae of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in lateral view. <bold>A</bold>. Photograph; <bold>B</bold>. line drawing. Abbreviations: <abbrev xlink:title="parapophysis">pa</abbrev>, parapophysis; <abbrev xlink:title="postzygapophysis">po</abbrev>, postzygapophysis; <abbrev xlink:title="prezygapophysis">pr</abbrev>, prezygapophysis; <abbrev xlink:title="right ilium">ril</abbrev>, right ilium; <abbrev xlink:title="sacral vertebrae">sv</abbrev>, sacral vertebrae; <abbrev xlink:title="transverse process">tp</abbrev>, transverse process.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g005.jpg" id="oo_1763438.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763438</uri>
            </graphic>
          </fig>
          <p>The first dorsal vertebra is well exposed (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The centrum is overlain by the first dorsal rib. The parapophysis is positioned at the anteroventral corner of the centrum, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Microraptor">Microraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B13">Hwang et al. 2002</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Buitreraptor">Buitreraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B8">Gianechini et al. 2018</xref>). Posterodorsal to the parapophysis, the diapophysis is well developed and extends posterolaterally (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). A lamina extends anteroventrally from the diapophysis to the centrum. Dorsally, the lamina borders a triangular prezygapophyseal-centrodiapophyseal fossa. As in the cervical series, the neural arch is X-shaped in dorsal view. The prezygapophysis is stout, with its articular facet directed anteromedially (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The anteroposterior length of the postzygapophysis is approximately twice that of the prezygapophysis. The neural spine is weakly developed. Moreover, the anterior part of the second dorsal vertebra is also well exposed. Its morphology is similar to that of the first dorsal vertebra, except that the diapophysis is more developed.</p>
          <p>The last five dorsal vertebrae are similar in morphology but decrease gradually in length. The antepenultimate dorsal vertebra is well exposed (Fig. <xref ref-type="fig" rid="F5">5</xref>). The centrum is dumbbell-shaped in lateral view (Fig. <xref ref-type="fig" rid="F5">5</xref>). Laterally, the centrum is not pneumatized. It is ventrally smooth and lacks a keel. In lateral view, the parapophysis is located anterodorsally on the centrum and projects laterally. The neural arch is formed by the anterodorsally directed prezygapophysis and the almost horizontally directed postzygapophysis (Fig. <xref ref-type="fig" rid="F5">5</xref>). Both are subequal in length. The postzygapophysis exceeds the posterior margin of the centrum. The transverse process is positioned more posteriorly on the neural arch relative to the parapophysis (Fig. <xref ref-type="fig" rid="F5">5</xref>). It is broadened and projects laterally. The neural spine is tall and rectangular in lateral view (Fig. <xref ref-type="fig" rid="F5">5</xref>). Its posterior edge is apparently smooth, and the scar for attachment of the interspinous ligament is absent.</p>
          <p><bold><italic>Sacral vertebrae</italic></bold>. The sacral vertebrae are poorly preserved and partially obscured by the right ilium and femur (Fig. <xref ref-type="fig" rid="F2">2</xref>). Virtually no anatomical details can be discerned.</p>
          <p><bold><italic>Caudal vertebrae</italic></bold>. In <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, an incomplete segment of the caudal series is preserved in articulation (Fig. <xref ref-type="fig" rid="F2">2</xref>). Sixteen caudal vertebrae are preserved, including the last three proximal caudal vertebrae and the first 13 distal caudal vertebrae. The well-defined transition point corresponds to the caudal region where the transverse processes terminate, represents the terminus of the M. caudofemoralis attachment (<xref ref-type="bibr" rid="B11">Hone et al. 2021</xref>), and demarcates the proximal from the distal caudal vertebrae (Fig. <xref ref-type="fig" rid="F6">6</xref>).</p>
          <p>Only the posterior portion of the antepenultimate proximal caudal vertebra is preserved, whereas the last two proximal caudal vertebrae are nearly complete (Fig. <xref ref-type="fig" rid="F6">6A, B</xref>). The penultimate proximal caudal vertebra is short and approximately two-thirds the length of the longest distal caudal vertebra (Table <xref ref-type="table" rid="T1">1</xref>). In lateral view, the centrum is concave ventrally. The transverse process is poorly preserved and anteroposteriorly elongated, showing marked lateral extension (Fig. <xref ref-type="fig" rid="F6">6A, B</xref>). The pre- and postzygapophyses extend anterodorsally and posterodorsally, respectively. The postzygapophysis is short and does not extend posteriorly beyond the posterior border of the centrum (Fig. <xref ref-type="fig" rid="F6">6A, B</xref>). The last proximal caudal vertebra is slightly elongated relative to the preceding proximal caudal vertebrae. The transverse process is weakly developed, leaving a low, anteroposteriorly extended ridge (Fig. <xref ref-type="fig" rid="F6">6A, B</xref>). The postzygapophysis is shorter than the prezygapophysis and does not extend beyond the posterior margin of the centrum.</p>
          <fig id="F6">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure6</object-id>
            <object-id content-type="arpha">95E889FD-C882-5805-8C02-4B53D25184C0</object-id>
            <label>Figure 6.</label>
            <caption>
              <p>Caudal vertebrae of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in lateral view. <bold>A, C</bold>. Photographs; <bold>B, D</bold>. line drawings. Abbreviations: <abbrev xlink:title="chevron">ch</abbrev>, chevron; <abbrev xlink:title="distal caudal vertebrae">dcv</abbrev>, distal caudal vertebrae; <abbrev xlink:title="proximal caudal vertebrae">pcv</abbrev>, proximal caudal vertebrae; <abbrev xlink:title="postzygapophysis">po</abbrev>, postzygapophysis; <abbrev xlink:title="prezygapophysis">pr</abbrev>, prezygapophysis; <abbrev xlink:title="transverse process">tp</abbrev>, transverse process.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g006.jpg" id="oo_1763439.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763439</uri>
            </graphic>
          </fig>
          <p>The first 13 distal caudal vertebrae are well preserved. The transverse process of the first distal caudal vertebra is absent (Fig. <xref ref-type="fig" rid="F6">6A, B</xref>). Along the series, the distal caudal vertebrae gradually elongate posteriorly, reaching their maximum length at the sixth distal caudal vertebra (Table <xref ref-type="table" rid="T1">1</xref>). The distal caudal vertebrae are similar in morphology. In lateral view, the centra are rectangular, and the lateral surfaces bear a longitudinal depression (Fig. <xref ref-type="fig" rid="F6">6C, D</xref>). The prezygapophyses are elongated on the first six distal caudal vertebrae and then become gradually more slender and shorter posteriorly. In contrast, all postzygapophyses of the distal caudal vertebrae are strongly reduced. As in other troodontids (<xref ref-type="bibr" rid="B20">Makovicky and Norell 2004</xref>), the distal caudal vertebrae are sulcate along the dorsal midline, and neural spines are absent.</p>
          <p>The anterior chevrons are poorly preserved, but the posterior chevrons are well preserved. The posterior chevrons are flattened dorsoventrally and elongated anteroposteriorly; this is a feature of derived coelurosaurians, such as dromaeosaurids, other troodontids, and basal birds (<xref ref-type="bibr" rid="B51">Xu 2002</xref>). These posterior chevrons are incomplete, except for the one between the tenth and eleventh distal caudal vertebrae. The anterior and posterior processes of this chevron are subequal in length (~10.5 mm; Fig. <xref ref-type="fig" rid="F6">6C, D</xref>). The anterior processes are slightly bifurcated, and the posterior processes are relatively blunt-ended in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B30">Pei 2015</xref>), unlike in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic>, which has relatively blunt-ended anterior processes and slightly bifurcated posterior processes (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). Moreover, in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B4">Currie and Dong 2001</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B14">Ji et al. 2005</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B30">Pei 2015</xref>), the chevrons of the distal caudal vertebrae are bifurcated on both the anterior and posterior processes. These chevrons are separated from each other (Fig. <xref ref-type="fig" rid="F6">6C, D</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B18">Li et al. 2021</xref>), but unlike <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinusonasus">Sinusonasus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B53">Xu and Wang 2004</xref>), whose chevrons contact each other and form a ventral band under the caudal centra.</p>
          <p><bold><italic>Ribs</italic></bold>. Cervical and dorsal ribs are partially preserved in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (Fig. <xref ref-type="fig" rid="F2">2</xref>). Some fragments of the cervical ribs are located near the third and seventh centra. The ninth and tenth cervical ribs are well exposed. They are double-headed, with a capitulum and tuberculum, and broad proximally (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The capitulum of the ninth cervical rib is short and closely articulated with the centrum. The tuberculum is broad and subrectangular in lateral view. The notch separating the tuberculum from the capitulum is shallow. Distally, the rib shaft narrows. The tenth cervical rib is nearly completely preserved (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The capitulum is elongated and tapers slightly anteriorly. The tuberculum is also subrectangular and is subequal to the capitulum in length but transversely wider than the latter (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The notch is deeper than that of the ninth cervical rib. The shaft is slender and elongated posteriorly, exceeding the posterior margin of the tenth cervical centrum (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>).</p>
          <p>As with the cervical ribs, the first dorsal rib is also double-headed. However, the first dorsal rib is distinctly longer than the tenth cervical rib. The capitulum of the first dorsal rib is elongate, with a slightly expanded end, and the tuberculum is stout (Fig. <xref ref-type="fig" rid="F3">3C, D</xref>). The notch is deeper than those of the cervical ribs. The proximal end of the second dorsal rib is preserved. As in the first dorsal rib, the capitulum is slender and elongate, and the tuberculum is short and broad. Six other dorsal ribs are identified; they are similar in morphology, and all are extremely elongate (Fig. <xref ref-type="fig" rid="F2">2</xref>). Their proximal ends are preserved underlying the femur, and their shafts are bowed and taper distally. As in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Archaeopteryx">Archaeopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B48">Wellnhofer 2009</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Microraptor">Microraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B13">Hwang et al. 2002</xref>; <xref ref-type="bibr" rid="B31">Pei et al. 2014</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Anchiornis">Anchiornis</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B32">Pei et al. 2017a</xref>), a longitudinal groove is present along the proximal shaft of these dorsal ribs. The groove is restricted to the proximal segment of each dorsal rib, tapers distally, and exhibits natural morphology. The cross-section of the mid-shaft is elliptical. As in other troodontids (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), the uncinate processes are not preserved. No attachment scars for uncinate processes have been identified on the dorsal ribs (Fig. <xref ref-type="fig" rid="F2">2</xref>).</p>
          <p><bold><italic>Pectoral girdle</italic></bold>. The pectoral girdle of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is preserved in articulation and is composed of the scapula and coracoid (Fig. <xref ref-type="fig" rid="F2">2</xref>). The scapula and coracoid are unfused, with a distinct suture between them. The glenoid fossa is not exposed, and its orientation is unclear.</p>
          <p>Both scapulae are exposed in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (Fig. <xref ref-type="fig" rid="F2">2</xref>). The right scapular blade is missing, and the acromion process of the left scapula is damaged. The complete scapular length was estimated based on the relatively well-preserved left scapula. The estimated length of the scapula is approximately 82% of the humeral length (Table <xref ref-type="table" rid="T2">2</xref>). This ratio is smaller than that in other Jehol troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (107%, <xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>; 100%, <xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (96%; <xref ref-type="bibr" rid="B14">Ji et al. 2005</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (98%; <xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (91%; <xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>). The left scapula is exposed medially and is elongate and slender (Fig. <xref ref-type="fig" rid="F2">2</xref>). The scapular blade is strap-like and mediolaterally compressed. It is nearly straight in medial view, unlike the bowed shape in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Buitreraptor">Buitreraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B8">Gianechini et al. 2018</xref>). A shallow groove is present on the medial surface near the proximal end and is subparallel to the ventral margin.</p>
          <table-wrap id="T2" position="float" orientation="portrait">
            <label>Table 2.</label>
            <caption>
              <p>Selected appendicular measurements of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (mm). <abbrev xlink:title="right">R</abbrev> and <abbrev xlink:title="left">L</abbrev> indicate right and left elements, respectively.</p>
            </caption>
            <table>
              <tbody>
                <tr>
                  <th rowspan="1" colspan="1">
                    <bold>Element</bold>
                  </th>
                  <th rowspan="1" colspan="1">
                    <bold>Value</bold>
                  </th>
                  <th rowspan="1" colspan="1">
                    <bold>Side</bold>
                  </th>
                  <th rowspan="1" colspan="1">
                    <bold>Data type</bold>
                  </th>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Scapula</td>
                  <td rowspan="1" colspan="1">80</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Coracoid</td>
                  <td rowspan="1" colspan="1">32.6</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Humerus</td>
                  <td rowspan="1" colspan="1">96.7</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Ulna</td>
                  <td rowspan="1" colspan="1">62.8</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Radius</td>
                  <td rowspan="1" colspan="1">62.6</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metacarpal I</td>
                  <td rowspan="1" colspan="1">13.5</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metacarpal II</td>
                  <td rowspan="1" colspan="1">31</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metacarpal III</td>
                  <td rowspan="1" colspan="1">31</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Manual phalanx I-1</td>
                  <td rowspan="1" colspan="1">31.4</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Manual phalanx II-1</td>
                  <td rowspan="1" colspan="1">21.7</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Manual phalanx III-1</td>
                  <td rowspan="1" colspan="1">9</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Manual phalanx III-2</td>
                  <td rowspan="1" colspan="1">8</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="left">L</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pubis</td>
                  <td rowspan="1" colspan="1">134.2</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Femur</td>
                  <td rowspan="1" colspan="1">143.0</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Tibiotarsus</td>
                  <td rowspan="1" colspan="1">205.7</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Fibula</td>
                  <td rowspan="1" colspan="1">190.5</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metatarsal I</td>
                  <td rowspan="1" colspan="1">14.4</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metatarsal II</td>
                  <td rowspan="1" colspan="1">109.6</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metatarsal III</td>
                  <td rowspan="1" colspan="1">123.8</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Metatarsal IV</td>
                  <td rowspan="1" colspan="1">116</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx I-1</td>
                  <td rowspan="1" colspan="1">10.5</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx I-2 (ungual)</td>
                  <td rowspan="1" colspan="1">11.6</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx II-1</td>
                  <td rowspan="1" colspan="1">20.1</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx II-2</td>
                  <td rowspan="1" colspan="1">17.7</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx II-3 (ungual)</td>
                  <td rowspan="1" colspan="1">25</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx III-1</td>
                  <td rowspan="1" colspan="1">24</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Estimated value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx III-2</td>
                  <td rowspan="1" colspan="1">20.9</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx III-3</td>
                  <td rowspan="1" colspan="1">16.7</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx III-4 (ungual)</td>
                  <td rowspan="1" colspan="1">14.4</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx IV-2</td>
                  <td rowspan="1" colspan="1">13.7</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx IV-3</td>
                  <td rowspan="1" colspan="1">11.2</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx IV-4</td>
                  <td rowspan="1" colspan="1">13.0</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
                <tr>
                  <td rowspan="1" colspan="1">Pedal phalanx IV-5 (ungual)</td>
                  <td rowspan="1" colspan="1">13.8</td>
                  <td rowspan="1" colspan="1">
                    <abbrev xlink:title="right">R</abbrev>
                  </td>
                  <td rowspan="1" colspan="1">Measured value</td>
                </tr>
              </tbody>
            </table>
            <table-wrap-foot>
              <fn>
                <p>Scapular length is estimated as the linear distance from the acromion process to the distal end of the scapular blade; coracoid height is measured as the dorsoventral straight-line distance; unguals are measured in a straight line from the center of the articular facet to the distal tip; all remaining elements are measured for proximodistal length.</p>
              </fn>
            </table-wrap-foot>
          </table-wrap>
          <p>The left coracoid is exposed in posterior view (Fig. <xref ref-type="fig" rid="F2">2</xref>). It is rectangular, with an extensive ventral blade, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B4">Currie and Dong 2001</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B51">Xu 2002</xref>). In posterior view, the coracoid is thickened dorsally and gradually thins ventrally. A circular coracoid foramen is present and located on the medioventral side of the glenoid fossa.</p>
          <p><bold><italic>Forelimb</italic></bold>. The right humerus is well preserved (Fig. <xref ref-type="fig" rid="F7">7</xref>). The humerus is 68% of the femoral length (Table <xref ref-type="table" rid="T2">2</xref>), much like that of some troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (68%; <xref ref-type="bibr" rid="B51">Xu 2002</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (70%; <xref ref-type="bibr" rid="B14">Ji et al. 2005</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (70%; <xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). In contrast, the humerus is proportionally short in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Linhevenator">Linhevenator</tp:taxon-name-part></tp:taxon-name></italic> (approximately 40% of the femoral length; <xref ref-type="bibr" rid="B57">Xu et al. 2011</xref>). Proximally, the deltopectoral crest is short, making up approximately 30% of the length of the humerus (Fig. <xref ref-type="fig" rid="F7">7</xref>). This condition of a short deltopectoral crest is also present in some other troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (23%; <xref ref-type="bibr" rid="B37">Russell and Dong 1993</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (22%; <xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (30%; <xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), but the proportion is greater than 50% in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Linhevenator">Linhevenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B57">Xu et al. 2011</xref>). An internal tuberosity is developed and projects transversely from the proximal margin of the humerus (Fig. <xref ref-type="fig" rid="F7">7</xref>). There is no obvious groove between the humeral head and the internal tuberosity, unlike in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic>, in which a groove is developed (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>). The humeral shaft is twisted approximately 90° (Fig. <xref ref-type="fig" rid="F7">7</xref>). In posterior view, a longitudinally extending, groove-like olecranon fossa is present on the distal end of the humerus (Fig. <xref ref-type="fig" rid="F7">7</xref>).</p>
          <fig id="F7">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure7</object-id>
            <object-id content-type="arpha">EDC37015-8233-5B67-BF3C-DBA57858670F</object-id>
            <label>Figure 7.</label>
            <caption>
              <p>Right forelimb of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in posterolateral view. <bold>A</bold>. Photograph; <bold>B</bold>. line drawing. Abbreviations: <abbrev xlink:title="deltopectoral crest">dc</abbrev>, deltopectoral crest; <abbrev xlink:title="humeral head">hh</abbrev>, humeral head; <abbrev xlink:title="internal tuberosity">it</abbrev>, internal tuberosity; <abbrev xlink:title="olecranon fossa">of</abbrev>, olecranon fossa; <abbrev xlink:title="right humerus">rh</abbrev>, right humerus; <abbrev xlink:title="right radius">rra</abbrev>, right radius; <abbrev xlink:title="right ulna">ru</abbrev>, right ulna.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g007.jpg" id="oo_1763440.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763440</uri>
            </graphic>
          </fig>
          <p>Both ulnae and both radii are preserved (Fig. <xref ref-type="fig" rid="F2">2</xref>). The left ulna and radius are nearly complete, whereas the distal ends of the right ulna and radius are missing. The shaft of the ulna is bowed posteriorly (Fig. <xref ref-type="fig" rid="F2">2</xref>), as in many other maniraptorans (<xref ref-type="bibr" rid="B51">Xu 2002</xref>). In contrast, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Anchiornis">Anchiornis</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B32">Pei et al. 2017a</xref>) possesses a straight ulna. The cross-section of the mid-shaft is subcircular. The distal end of the ulna is transversely expanded, and its articular facet is flat.</p>
          <p>The radius is straight (Fig. <xref ref-type="fig" rid="F2">2</xref>). It is approximately 65% of the humeral length (Table <xref ref-type="table" rid="T2">2</xref>), whereas in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>), the radius is approximately 90% of the humeral length. Its mid-shaft is subcircular in cross-section and has a constant diameter. The shaft of the radius is more slender than the ulnar shaft. The diameter of the mid-shaft is 2.9 mm in the left radius and approximately half that of the left ulna (5.9 mm), whereas the diameter is 3.3 mm in the right radius and only slightly less than that of the right ulna (3.8 mm), which may be an artifact of taphonomic distortion or ontogenetic variation (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F7">7</xref>). Distally, the left radius is slightly curved and articulates with the radiale.</p>
          <p>Two left carpals are preserved in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062: the semilunate and radiale (Fig. <xref ref-type="fig" rid="F2">2</xref>). The semilunate is larger and crescent-shaped in dorsal view, with its proximal surface being convex. Distally, it covers the proximal ends of metacarpals I and II, as in most maniraptorans (<xref ref-type="bibr" rid="B28">Ostrom 1969</xref>; <xref ref-type="bibr" rid="B59">Xu et al. 2014</xref>; <xref ref-type="bibr" rid="B30">Pei 2015</xref>; <xref ref-type="bibr" rid="B22">Napoli et al. 2025</xref>). It is closely associated with the metacarpals. The radiale is smaller and lies between the semilunate and radius.</p>
          <p>Metacarpals I, II, and III; manual phalanges I-1, II-1, III-1, and III-2; and the proximal portion of phalanx II-2 are preserved (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F8">8</xref>). Metacarpal I is the shortest of the preserved manual elements and is approximately 43% of the length of metacarpal II (Table <xref ref-type="table" rid="T2">2</xref>). Metacarpal I is relatively robust and has a diameter of approximately 3.5 mm at the mid-shaft. Proximally, metacarpal I is closely associated with metacarpal II. The distal end of metacarpal I expands dorsoventrally and appears to be ginglymoid, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>).</p>
          <fig id="F8">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure8</object-id>
            <object-id content-type="arpha">B99111B8-8C7C-5012-8E5A-C4F43BC23CE8</object-id>
            <label>Figure 8.</label>
            <caption>
              <p>Left manus of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in medial view <bold>A, C</bold>. and dorsal view <bold>B, D</bold>. <bold>A, B</bold>. Photographs; <bold>C, D</bold>. line drawings. Abbreviations: <abbrev xlink:title="blood groove">bg</abbrev>, blood groove; <abbrev xlink:title="manual phalanx">m</abbrev>, manual phalanx; <abbrev xlink:title="metacarpal">mc</abbrev>, metacarpal.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g008.jpg" id="oo_1763441.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763441</uri>
            </graphic>
          </fig>
          <p>Metacarpals II and III are exposed in dorsal view, except that their proximal ends are obscured by the tibia (Fig. <xref ref-type="fig" rid="F8">8</xref>). They are subequal in length. The shaft of metacarpal II has a mediolateral width of approximately 2.1 mm, similar to that of metacarpal III. Metacarpal III extends distally to the level of metacarpal II (Fig. <xref ref-type="fig" rid="F8">8</xref>). However, metacarpal III extends farther distally than metacarpal II in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>).</p>
          <p>Manual phalanx I-1 is long and robust. The cross-section of the mid-shaft is subcircular and has a diameter of 3.3 mm, which is greater than those of metacarpals II and III (Fig. <xref ref-type="fig" rid="F8">8B, D</xref>). The combined length of manual phalanx I-1 and metacarpal I is greater than that of metacarpal II, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). This condition differs from that of some dromaeosaurs, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Microraptor">Microraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B56">Xu et al. 2003</xref>; <xref ref-type="bibr" rid="B31">Pei et al. 2014</xref>), in which the combined length of phalanx I-1 and metacarpal I is shorter than that of metacarpal II. Proximally, phalanx I-1 bears a prominent ventral intercondylar tuberosity. The shaft of phalanx I-1 is slightly dorsally bowed in lateral view. The distal end is apparently ginglymoid. A collateral ligament pit is exposed on the medial surface of phalanx I-1 (Fig. <xref ref-type="fig" rid="F8">8</xref>). This ligament pit is deep and dorsally shifted on the medial face of the distal articular end. A partially preserved ungual, tentatively identified as phalanx I-2, lies on the dorsal side of the distal end of phalanx I-1, and the blood groove is visible (Fig. <xref ref-type="fig" rid="F8">8</xref>). A fragmented bony element lies isolated near the distal end of phalanx I-1, and it cannot be confidently attributed to any element of the manus (Fig. <xref ref-type="fig" rid="F8">8</xref>).</p>
          <p>The shaft and distal end of phalanx II-1 are partially exposed (Fig. <xref ref-type="fig" rid="F8">8</xref>). The shaft is slender, with a diameter of approximately 2.3 mm. Medially, the distal end is sculptured by a deep ligament pit that is positioned centrally (Fig. <xref ref-type="fig" rid="F8">8</xref>), whereas the medial ligament pit is absent in phalanx II-1 of the unnamed troodontid <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1042 (<xref ref-type="bibr" rid="B63">Yu et al. 2022</xref>). Phalanx II-2 is partially preserved, and its proximal part is well exposed. Proximally, phalanx II-2 bears well-developed ventral and dorsal intercondylar tuberosities (Fig. <xref ref-type="fig" rid="F8">8A, C</xref>), as in the unnamed troodontid <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1042 (<xref ref-type="bibr" rid="B63">Yu et al. 2022</xref>). The ventral tuberosity is larger than the dorsal one (Fig. <xref ref-type="fig" rid="F8">8A, C</xref>). The phalanges of digit III are comparable in diameter to those of digit II (Fig. <xref ref-type="fig" rid="F8">8B, D</xref>). Manual phalanx III-1 is subequal to phalanx III-2 in length (Table <xref ref-type="table" rid="T2">2</xref>), as in some troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Hypnovenator">Hypnovenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B15">Kubota et al. 2024</xref>), and the unnamed troodontids <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/1126 (<xref ref-type="bibr" rid="B30">Pei 2015</xref>) and <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1042 (<xref ref-type="bibr" rid="B63">Yu et al. 2022</xref>).</p>
          <p><bold><italic>Pelvic girdle</italic></bold>. The right ilium is laterally exposed in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, and the postacetabular process is missing (Fig. <xref ref-type="fig" rid="F9">9</xref>). The ilium is anteroposteriorly elongated. The preacetabular process has a convex anterior margin (Figs <xref ref-type="fig" rid="F5">5</xref>, <xref ref-type="fig" rid="F9">9</xref>), but this is possibly a taphonomic artifact. In contrast, the ilium of other troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Latenivenatrix">Latenivenatrix</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B46">Van der Reest and Currie 2017</xref>; <xref ref-type="bibr" rid="B36">Rhodes et al. 2021</xref>), has a nearly straight anterior margin. The ventral margin of the preacetabular blade slopes slightly anteroventrally, and the anteroventral process is drastically reduced (Fig. <xref ref-type="fig" rid="F9">9</xref>). The dorsal margin of the preacetabular process is roughly straight. The pubic peduncle is rectangular in lateral view and bears an articular facet that extends nearly horizontally (Fig. <xref ref-type="fig" rid="F9">9</xref>), which differs from the wedge-like pubic peduncle of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mahakala">Mahakala</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B44">Turner et al. 2011</xref>) and the unnamed troodontid <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/1126 (<xref ref-type="bibr" rid="B30">Pei 2015</xref>). A large, deep fossa is located on the lateral surface of the pubic peduncle (Fig. <xref ref-type="fig" rid="F9">9</xref>) for the attachment of the M. cuppedicus. Dorsally, a ridge defining the fossa is well developed. It terminates dorsal to the pubic peduncle and is not continuous with the acetabular rim.</p>
          <fig id="F9">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure9</object-id>
            <object-id content-type="arpha">963DF8C1-3693-5BA9-9B85-AB488F449A79</object-id>
            <label>Figure 9.</label>
            <caption>
              <p>Pelvic girdle of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in lateral view. <bold>A</bold>. Photograph; <bold>B</bold>. line drawing. Abbreviations: <abbrev xlink:title="anterior border of the preacetabular process">abpp</abbrev>, anterior border of the preacetabular process; <abbrev xlink:title="acetabulum">ac</abbrev>, acetabulum; <abbrev xlink:title="ambiens process">amp</abbrev>, ambiens process; <abbrev xlink:title="fossa">fo</abbrev>, fossa; <abbrev xlink:title="ischial peduncle of the pubis">ipp</abbrev>, ischial peduncle of the pubis; <abbrev xlink:title="pubic boot">pb</abbrev>, pubic boot; <abbrev xlink:title="pubic peduncle of the ilium">ppil</abbrev>, pubic peduncle of the ilium; <abbrev xlink:title="pubic peduncle of the ischium">ppis</abbrev>, pubic peduncle of the ischium; <abbrev xlink:title="right femur">rf</abbrev>, right femur.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g009.jpg" id="oo_1763442.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763442</uri>
            </graphic>
          </fig>
          <p>The right pubis is well preserved (Fig. <xref ref-type="fig" rid="F9">9</xref>). The pubis is nearly vertically oriented, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), unlike the posteroventrally oriented condition in some basal paravians, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Archaeopteryx">Archaeopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B29">Ostrom 1976</xref>; <xref ref-type="bibr" rid="B27">O’Connor et al. 2025</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithosaurus">Sinornithosaurus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B54">Xu et al. 1999</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), and the anteroventrally oriented condition in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B26">Norell et al. 2009</xref>) and the unnamed troodontid <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/1126 (<xref ref-type="bibr" rid="B30">Pei 2015</xref>). Proximally, the pubis projects anteriorly, forming an ambiens process (Fig. <xref ref-type="fig" rid="F9">9</xref>). The ambiens process is moderately developed, and its anteroposterior length is less than that of the ischial peduncle of the pubis, differing from the elongated condition in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B26">Norell et al. 2009</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Latenivenatrix">Latenivenatrix</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B46">Van der Reest and Currie 2017</xref>; <xref ref-type="bibr" rid="B36">Rhodes et al. 2021</xref>), in which the anteroposterior length is far greater than that of the ischial peduncle of the pubis. The pubis articulates dorsally with the pubic peduncle of the ilium along a nearly horizontal articular facet (Fig. <xref ref-type="fig" rid="F9">9</xref>). Posteriorly, the ischial peduncle of the pubis is trapezoidal in lateral view and narrows posteriorly to articulate with the ischium (Fig. <xref ref-type="fig" rid="F9">9</xref>). Distally, the pubic shaft is elongate and nearly straight but curves slightly posteriorly. It is mediolaterally flat in the proximal portion and twisted at the mid-shaft (Fig. <xref ref-type="fig" rid="F9">9</xref>). The pubic apron is transversely expanded, a characteristic of troodontids (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). The pubic apron is greater than half the length of the pubic shaft, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B51">Xu 2002</xref>), but unlike in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Talos">Talos</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B64">Zanno et al. 2011</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Troodon">Troodon</tp:taxon-name-part></tp:taxon-name></italic>, and <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/1126 (<xref ref-type="bibr" rid="B30">Pei 2015</xref>), in which the pubic apron is less than half the length of the pubis. The pubic boot is expanded posteriorly and has a slight anterior expansion (Fig. <xref ref-type="fig" rid="F9">9</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Almas">Almas</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B33">Pei et al. 2017b</xref>).</p>
          <p>Only the pubic peduncle of the right ischium is preserved (Fig. <xref ref-type="fig" rid="F9">9</xref>). The pubic peduncle is quadrangular in lateral view and articulates with the ischial peduncle of the pubis along an inclined articular facet.</p>
          <p><bold><italic>Hindlimb</italic></bold>. Both femora are preserved in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (Fig. <xref ref-type="fig" rid="F2">2</xref>). As in most theropods (<xref ref-type="bibr" rid="B24">Norell and Makovicky 1999</xref>; <xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>), the femoral shaft is anteriorly bowed. The femoral head projects medially at approximately 90° relative to the long axis of the shaft. The greater trochanter is located on the lateral side of the femoral head (Fig. <xref ref-type="fig" rid="F10">10</xref>). Anteriorly, the proximal end of the femur is poorly preserved. Consequently, the morphology of the lesser trochanter is uncertain. The posterior trochanter lies on the posterolateral side of the femur, near the base of the greater trochanter (Fig. <xref ref-type="fig" rid="F10">10B</xref>). The posterior trochanter is developed as a large mound, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), but in contrast to the ridge-like posterior trochanter seen in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B26">Norell et al. 2009</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Linhevenator">Linhevenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B57">Xu et al. 2011</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Talos">Talos</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B64">Zanno et al. 2011</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Philovenator">Philovenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B58">Xu et al. 2012</xref>). The trochanteric shelf is a knob-like process on the lateral surface of the proximal portion of the shaft (Fig. <xref ref-type="fig" rid="F10">10A–C</xref>). Distally, the shelf gradually becomes a low lateral ridge extending along the long axis of the femur to the lateral condyle of the distal end (Fig. <xref ref-type="fig" rid="F10">10B, E</xref>). On the posterior surface of the proximal end of the shaft, a low ridge extends longitudinally and represents a reduced fourth trochanter, the insertion position of the M. caudofemoralis longus (Fig. <xref ref-type="fig" rid="F10">10B</xref>). The cross-section of the mid-shaft is subcircular, with a diameter of 11.3 mm. Distally, the lateral and medial condyles are comparable in size (Fig. <xref ref-type="fig" rid="F10">10D</xref>). As in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B51">Xu 2002</xref>), the lateral condyle extends more distally than the medial condyle. In posterior view, the medial condyle clearly extends medially (Fig. <xref ref-type="fig" rid="F10">10D</xref>).</p>
          <fig id="F10">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure10</object-id>
            <object-id content-type="arpha">EB2F79FD-6F94-5D2A-ACB8-0572EFF78818</object-id>
            <label>Figure 10.</label>
            <caption>
              <p>Right femur of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. <bold>A</bold>. Lateral view; <bold>B</bold>. posterior view; <bold>C</bold>. proximal view; <bold>D</bold>. posterior view of the distal end; <bold>E</bold>. lateral view of the distal end. Abbreviations: <abbrev xlink:title="distal lateral condyle">dlc</abbrev>, distal lateral condyle; <abbrev xlink:title="distal medial condyle">dmc</abbrev>, distal medial condyle; <abbrev xlink:title="femoral head">fh</abbrev>, femoral head; <abbrev xlink:title="fourth trochanter">ftr</abbrev>, fourth trochanter; <abbrev xlink:title="greater trochanter">gt</abbrev>, greater trochanter; <abbrev xlink:title="lateral ridge">lr</abbrev>, lateral ridge; <abbrev xlink:title="posterior trochanter">pt</abbrev>, posterior trochanter; <abbrev xlink:title="trochanteric shelf">ts</abbrev>, trochanteric shelf.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g010.jpg" id="oo_1763443.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763443</uri>
            </graphic>
          </fig>
          <p>Both tibiotarsi are preserved. The right tibiotarsus is well exposed, with no taphonomic deformation (Fig. <xref ref-type="fig" rid="F2">2</xref>). The tibiotarsus is long and straight (Fig. <xref ref-type="fig" rid="F11">11</xref>). It is approximately 143% of the femoral length (Table <xref ref-type="table" rid="T2">2</xref>), similar to that of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (139%), <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (130%; <xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (131%; <xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>). Proximally, as in other troodontids, the tibiotarsus is anteroposteriorly expanded, unlike the more transversely expanded element in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>). The anterior cnemial crest is well developed, expands anteriorly, and curves slightly laterally (Fig. <xref ref-type="fig" rid="F11">11B, C</xref>), a feature common to many coelurosaurs (<xref ref-type="bibr" rid="B24">Norell and Makovicky 1999</xref>; <xref ref-type="bibr" rid="B21">Makovicky et al. 2003</xref>; <xref ref-type="bibr" rid="B8">Gianechini et al. 2018</xref>). The lateral and posterior condyles are well developed and separated by a shallow groove (Fig. <xref ref-type="fig" rid="F11">11A</xref>). In lateral view, the lateral condyle is rounded and contacts the proximal end of the fibula. In posterior view, the lateral condyle is slightly larger than the posterior condyle. In contrast to <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), the lateral cnemial crest is absent in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (Fig. <xref ref-type="fig" rid="F11">11C</xref>). The fibular crest is present on the lateral surface and is located approximately 25.0 mm from the proximal end of the tibia, which is approximately 12% of the total tibiotarsal length. It is slightly deflected anteriorly, bears a sharp edge, and gradually tapers distally into the shaft. The cross-section of the mid-shaft is subcircular. Distally, the tibiotarsus expands mediolaterally. The astragalus and calcaneum are fused (Fig. <xref ref-type="fig" rid="F11">11D, E</xref>). In posterior view, a shallow groove is present between the tibia and the proximal tarsals (Fig. <xref ref-type="fig" rid="F11">11A</xref>). The ascending process of the astragalus is broken; therefore, fine anatomical features of the astragalus cannot be observed (Fig. <xref ref-type="fig" rid="F11">11E</xref>).</p>
          <fig id="F11">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure11</object-id>
            <object-id content-type="arpha">1203E08B-0D40-5C38-8E4A-91875717F09E</object-id>
            <label>Figure 11.</label>
            <caption>
              <p>Right tibiotarsus and fibula of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. <bold>A</bold>. Posterior view; <bold>B</bold>. lateral view; <bold>C</bold>. anterior view of the proximal end; <bold>D</bold>. distal view; <bold>E</bold>. anterior view of the distal end; <bold>F</bold>. lateral view of the distal end. Abbreviations: <abbrev xlink:title="ascending process">ap</abbrev>, ascending process; <abbrev xlink:title="astragalus">as</abbrev>, astragalus; <abbrev xlink:title="calcaneum">ca</abbrev>, calcaneum; <abbrev xlink:title="cnemial crest">cc</abbrev>, cnemial crest; <abbrev xlink:title="fibular crest">fc</abbrev>, fibular crest; <abbrev xlink:title="iliofibularis tubercle">ilt</abbrev>, iliofibularis tubercle; <abbrev xlink:title="proximal lateral condyle">plc</abbrev>, proximal lateral condyle; <abbrev xlink:title="proximal posterior condyle">ppc</abbrev>, proximal posterior condyle; <abbrev xlink:title="right fibula">rfi</abbrev>, right fibula; <abbrev xlink:title="right tibiotarsus">rti</abbrev>, right tibiotarsus; <abbrev xlink:title="shallow groove">sg</abbrev>, shallow groove.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g011.jpg" id="oo_1763444.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763444</uri>
            </graphic>
          </fig>
          <p>The right fibula is exposed, and portions of the proximal end and shaft are missing in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (Fig. <xref ref-type="fig" rid="F11">11B</xref>). The fibula is a slender element extending along the lateral edge of the tibiotarsus. Proximally, the fibula is anteroposteriorly expanded and approximately 50% of the tibial width (Fig. <xref ref-type="fig" rid="F11">11B</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (<xref ref-type="bibr" rid="B51">Xu 2002</xref>). In proximal view, the articular facet of the fibula is nearly flat. An iliofibularis tubercle is developed on the lateral surface of the proximal portion of the fibula (Fig. <xref ref-type="fig" rid="F11">11A, B</xref>), approximately 30.0 mm from the proximal end of the fibula. The cross-section of the mid-shaft is subcircular, and its diameter is 2.2 mm. The distal end of the fibula articulates with the calcaneum (Fig. <xref ref-type="fig" rid="F11">11B</xref>), as in many paravians, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Archaeopteryx">Archaeopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B29">Ostrom 1976</xref>; <xref ref-type="bibr" rid="B27">O’Connor et al. 2025</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B4">Currie and Dong 2001</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Microraptor">Microraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B13">Hwang et al. 2002</xref>).</p>
          <p>Both tarsometatarsi are well preserved (Fig. <xref ref-type="fig" rid="F2">2</xref>). The right distal tarsals are exposed (Fig. <xref ref-type="fig" rid="F12">12</xref>). The distal tarsals cover most of the posterior portions of the proximal ends of metatarsals III and IV and overhang the metatarsus posteriorly (Fig. <xref ref-type="fig" rid="F12">12B, C</xref>). In proximal view, the proximal surface of the distal tarsals is nearly horizontal (Fig. <xref ref-type="fig" rid="F12">12C</xref>). A small notch on the posterior border of this bone possibly represents the fusion of the distal tarsals.</p>
          <fig id="F12">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure12</object-id>
            <object-id content-type="arpha">6125CBA1-3814-56F9-A28B-2A8D3EC06D6C</object-id>
            <label>Figure 12.</label>
            <caption>
              <p>Right metatarsus of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. <bold>A</bold>. Anterior view; <bold>B</bold>. posterior view; <bold>C</bold>. proximal view; <bold>D</bold>. cross-section of the shaft. Abbreviations: <abbrev xlink:title="distal tarsus">dt</abbrev>, distal tarsus; <abbrev xlink:title="right metatarsus">rmt</abbrev>, right metatarsus.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g012.jpg" id="oo_1763445.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763445</uri>
            </graphic>
          </fig>
          <p>The left metatarsus is nearly complete but slightly compressed medially (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F13">13</xref>). The right metatarsus is not deformed, but its distal end is missing (Fig. <xref ref-type="fig" rid="F12">12</xref>). Metatarsals I–IV are exposed on the left side, and metatarsals II–V are exposed on the right side. The metatarsus of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is long, approximately 123.8 mm, based on the length of metatarsal III. It is approximately 86% of the length of the femur, unlike that of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Philovenator">Philovenator</tp:taxon-name-part></tp:taxon-name></italic> (125%; <xref ref-type="bibr" rid="B58">Xu et al. 2012</xref>). Metatarsal II is narrower mediolaterally than metatarsal IV (Fig. <xref ref-type="fig" rid="F12">12</xref>). This condition is typically asymmetrical in troodontids (<xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>).</p>
          <p>Metatarsal I is short and narrow (Fig. <xref ref-type="fig" rid="F2">2</xref>), as in other coelurosaurians. Metatarsal I is roughly cone-shaped and narrows proximally (Fig. <xref ref-type="fig" rid="F13">13</xref>). Distally, it forms a single condyle (Fig. <xref ref-type="fig" rid="F14">14</xref>), as in some troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B4">Currie and Dong 2001</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Talos">Talos</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B64">Zanno et al. 2011</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Troodon">Troodon</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B6">Fowler et al. 2011</xref>). The distal end of metatarsal I is medially offset.</p>
          <p>Metatarsal II is straight and approximately 89% of the length of metatarsal III, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 and <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B51">Xu 2002</xref>). In proximal view, the proximal end of metatarsal II is subrectangular, and its mediolateral width is approximately 8.0 mm (Fig. <xref ref-type="fig" rid="F12">12C</xref>). The mid-shaft of metatarsal II becomes subrhombic in cross-section, with a ridged posterior margin (Fig. <xref ref-type="fig" rid="F12">12B</xref>). Metatarsal II is only slightly narrower than metatarsal IV, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B14">Ji et al. 2005</xref>). Distally, metatarsal II is closely associated with the medial surface of metatarsal III (Fig. <xref ref-type="fig" rid="F14">14</xref>). The distal end of metatarsal II is not ginglymoid, as in other troodontids (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). In medial view, the ligament pit is absent from the distal end (Fig. <xref ref-type="fig" rid="F14">14</xref>).</p>
          <fig id="F13">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure13</object-id>
            <object-id content-type="arpha">70B07BE3-8FB3-52FC-A8F0-DBD002A8B0A4</object-id>
            <label>Figure 13.</label>
            <caption>
              <p>Left metatarsus of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in medial view <bold>A, B</bold>. and cross-section <bold>C, D</bold>. <bold>A, C</bold>. Photographs; <bold>B, D</bold>. line drawings. Abbreviations: <abbrev xlink:title="left metatarsus">lmt</abbrev>, left metatarsus.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g013.jpg" id="oo_1763446.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763446</uri>
            </graphic>
          </fig>
          <fig id="F14">
            <object-id content-type="doi">10.3897/sjp.145.196379.figure14</object-id>
            <object-id content-type="arpha">6CC680CE-9982-50FB-A17B-3C23B7924768</object-id>
            <label>Figure 14.</label>
            <caption>
              <p>Left pedal digits of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 in medial view. <bold>A</bold>. Photograph; <bold>B</bold>. line drawing. Abbreviations: <abbrev xlink:title="blood groove">bg</abbrev>, blood groove; <abbrev xlink:title="left metatarsus">lmt</abbrev>, left metatarsus; <abbrev xlink:title="ligament pit">lp</abbrev>, ligament pit; <abbrev xlink:title="pedal phalanx">p</abbrev>, pedal phalanx; <abbrev xlink:title="proximodorsal lip">pdl</abbrev>, proximodorsal lip.</p>
            </caption>
            <graphic xlink:href="sjp-145-901_article-196379__-g014.jpg" id="oo_1763447.jpg">
              <uri content-type="original_file">https://binary.pensoft.net/fig/1763447</uri>
            </graphic>
          </fig>
          <p>Metatarsal III is constricted between metatarsals II and IV. The proximal end of metatarsal III is not strongly constricted and is visible in anterior view (Fig. <xref ref-type="fig" rid="F12">12A</xref>), representing a subarctometatarsalian condition, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>), and some dromaeosaurids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithosaurus">Sinornithosaurus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B54">Xu et al. 1999</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Microraptor">Microraptor</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>). Proximally, metatarsal III extends anteriorly to the same plane as metatarsals II and IV (Fig. <xref ref-type="fig" rid="F12">12A, C</xref>). In proximal view, the mediolateral width of metatarsal III is approximately 4.5 mm. The cross-section of the mid-shaft is subrectangular, and its mediolateral width is approximately 4.0 mm in anterior view. In posterior view, the shaft of metatarsal III does not extend posteriorly to the same plane as metatarsals II and IV (Figs <xref ref-type="fig" rid="F12">12</xref>, <xref ref-type="fig" rid="F13">13</xref>). Distally, metatarsal III extends beyond metatarsals II and IV, as in most troodontids, but in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tochisaurus">Tochisaurus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B16">Kurzanov and Osmólska 1991</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Talos">Talos</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B64">Zanno et al. 2011</xref>), the distal end of metatarsal III is almost level with that of metatarsal IV. At the distal end of metatarsal III, a distinct extensor fossa is developed on the anterior surface (Fig. <xref ref-type="fig" rid="F14">14</xref>). A lateral bony tab proximal to the distal condyles is absent, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B26">Norell et al. 2009</xref>), whereas the tab is developed in the unnamed troodontid <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/44 (<xref ref-type="bibr" rid="B2">Barsbold et al. 1987</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Talos">Talos</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B64">Zanno et al. 2011</xref>). A subcircular ligament pit is present on the medial side of the distal end (Fig. <xref ref-type="fig" rid="F14">14</xref>).</p>
          <p>Metatarsal IV is the most robust element of the metatarsus (Fig. <xref ref-type="fig" rid="F12">12A, B</xref>), as in other troodontids (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). It is longer than metatarsal II but shorter than metatarsal III. In proximal view, metatarsal IV is mediolaterally widened (Fig. <xref ref-type="fig" rid="F12">12C</xref>). The anterior surface is flattened proximally and gradually becomes ridged distally (Fig. <xref ref-type="fig" rid="F12">12A</xref>). A flange is present posteriorly on metatarsal IV (Fig. <xref ref-type="fig" rid="F12">12B</xref>), as in most deinonychosaurians. The mid-shaft of metatarsal IV is subtriangular in cross-section. In posterior view, the shafts of metatarsals IV and II are nearly parallel and do not contact each other (Fig. <xref ref-type="fig" rid="F12">12B</xref>), unlike the condition in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>) and Late Cretaceous troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tochisaurus">Tochisaurus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B16">Kurzanov and Osmólska 1991</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Philovenator">Philovenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B58">Xu et al. 2012</xref>), and <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/1126 (<xref ref-type="bibr" rid="B30">Pei 2015</xref>). The distal end of metatarsal IV reaches the level of the ligament pit of metatarsal III, as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>).</p>
          <p>The right metatarsal V is missing its distal margin (Fig. <xref ref-type="fig" rid="F12">12A, B</xref>). The preserved portion is a very slender bone. Proximally, metatarsal V is slightly expanded transversely and closely attached to the lateral surface of metatarsal IV (Fig. <xref ref-type="fig" rid="F12">12A, B</xref>). Distally, metatarsal V narrows gradually. It is oval in cross‑section and mediolaterally wider than anteroposteriorly tall.</p>
          <p>All digits of the left pes are well preserved (Figs <xref ref-type="fig" rid="F2">2</xref>, <xref ref-type="fig" rid="F14">14</xref>). In contrast, the right pes preserves only part of pedal digit III. As in other coelurosaurians (<xref ref-type="bibr" rid="B20">Makovicky and Norell 2004</xref>), the pedal phalangeal formula is 2-3-4-5-0 in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062.</p>
          <p>Pedal digit I is short and does not extend beyond the distal end of metatarsal III (Fig. <xref ref-type="fig" rid="F14">14</xref>), in contrast to <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). Phalanx I-1 is slender and is the shortest phalanx (Table <xref ref-type="table" rid="T2">2</xref>). The distal end of phalanx I-1 is ginglymoid (Fig. <xref ref-type="fig" rid="F14">14</xref>). Pedal ungual I is smaller than the other pedal unguals. The flexor tubercle is weakly developed. The blood groove is weakly developed and positioned relatively ventrally on the medial surface (Fig. <xref ref-type="fig" rid="F14">14</xref>).</p>
          <p>Pedal digit II is more robust than the other pedal digits (Fig. <xref ref-type="fig" rid="F14">14</xref>). Phalanx II-2 is approximately 88% of the length of phalanx II-1 (Table <xref ref-type="table" rid="T2">2</xref>). This ratio is larger than that in some early-diverging troodontids, such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic><abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 (67%) and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (69%), indicating a relatively unreduced phalanx II-2. The distal end of phalanx II-1 is ginglymoid, with two asymmetrical condyles, and the lateral condyle is larger than the medial condyle. A circular ligament pit is exposed on the medial surface of the distal end of phalanx II-1 and is positioned near the center of the distal portion of the phalanx (Fig. <xref ref-type="fig" rid="F14">14</xref>). Phalanx II-2 bears a prominent ventral intercondylar tuberosity (Fig. <xref ref-type="fig" rid="F14">14</xref>), as in other deinonychosaurians (<xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>; <xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). The shaft of phalanx II-2 is slightly constricted at its midlength, and its dorsoventral height is approximately 5.4 mm. The distal end of phalanx II-2 is subcircular in medial view, and the ligament pit is oval (Fig. <xref ref-type="fig" rid="F14">14</xref>). Pedal ungual II is damaged at the proximodorsal portion and distal tip. It is larger than the other unguals and strongly curved (Fig. <xref ref-type="fig" rid="F14">14</xref>), as in other deinonychosaurians (<xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>). A flexor tubercle is strongly developed, implying the presence of flexor muscles (<xref ref-type="bibr" rid="B28">Ostrom 1969</xref>). The blood groove is distinct and tapers distally (Fig. <xref ref-type="fig" rid="F14">14</xref>).</p>
          <p>Pedal digit III is the longest digit of the pes (Fig. <xref ref-type="fig" rid="F14">14</xref>). Phalanx III-1 is partially exposed. The ligament pit is well developed, circular, and centrally positioned on the medial surface of the distal end (Fig. <xref ref-type="fig" rid="F14">14</xref>). Proximally, the dorsoventral height of phalanx III-2 is 8.6 mm and gradually decreases distally. The distal articular end of phalanx III-2 is ginglymoid. The ligament pit is large and oval and is located in the center of the medial surface of the distal end (Fig. <xref ref-type="fig" rid="F14">14</xref>). Phalanx III-3 is shorter than phalanx III-2. The ligament pit is oval and dorsally shifted on the medial surface of the distal end (Fig. <xref ref-type="fig" rid="F14">14</xref>). Pedal ungual III is significantly smaller and less curved than pedal ungual II, as in other troodontids (<xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>). The flexor tubercle is weakly developed, and the blood groove is positioned relatively ventrally along the medial surface. The proximodorsal lip, a raised bony flange, is developed (Fig. <xref ref-type="fig" rid="F14">14</xref>), as in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Hypnovenator">Hypnovenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B15">Kubota et al. 2024</xref>).</p>
          <p>Pedal digit IV includes five phalanges, and phalanx IV-1 is covered by digit II. Phalanges IV-2, IV-3, and IV-4 are similar in morphology, and the ligament pits are well developed at their distal ends (Fig. <xref ref-type="fig" rid="F14">14</xref>). The distal end of phalanx IV-4 is ginglymoid, with two symmetrical condyles. Pedal ungual IV is slightly larger than ungual I but smaller than ungual III (Fig. <xref ref-type="fig" rid="F14">14</xref>). The morphologies of the flexor tubercle and blood groove are similar to those of ungual III.</p>
          <sec sec-type="Phylogenetic analyses" id="sec5">
            <title>Phylogenetic analyses</title>
            <p>To determine the phylogenetic position of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, the data matrix for coelurosaurians published by Pei et al. (<xref ref-type="bibr" rid="B34">2020</xref>, <xref ref-type="bibr" rid="B35">2021</xref>) was used, with <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 added (170 taxa and 853 characters). The phylogenetic matrix and tree files are deposited in and publicly accessible through MorphoBank. A total of 140 characters were treated as ordered, whereas all remaining characters were treated as unordered. Polymorphic character scoring was implemented throughout the matrix. Taxa exhibiting multiple morphological states for a single character were coded with combined-state notations (e.g., [0 1]) directly within the matrix instead of using the any-instance, missing-data, or three-state scaled coding schemes. The operational taxonomic unit (OTU) of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> was scored based on the holotype <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615 and paratype <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583.</p>
            <p>To cross-validate the results and improve the reliability of the inferences, separate phylogenetic parsimony analyses under equal weighting and implied weighting were performed on the character matrix. Both analyses were conducted using the “traditional search” in TNT version 1.5 (<xref ref-type="bibr" rid="B10">Goloboff et al. 2008</xref>; <xref ref-type="bibr" rid="B9">Goloboff and Catalano 2016</xref>). The maximum number of trees held in memory was set to 50,000. The traditional search strategy used 1,000 replicates of Wagner trees, TBR branch swapping, and 10 trees held per replicate.</p>
            <p>The analysis under equal weighting produced 50 most parsimonious trees (MPTs), with a length of 3,509 steps, CI = 0.309, and RI = 0.780. In the strict consensus tree, <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic>, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic>, and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> are recovered as a clade forming the earliest-diverging branch within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>, and <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is recovered as the sister group of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> (Fig. <xref ref-type="fig" rid="F15">15A</xref>). <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic>, <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/44, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic>, and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinusonasus">Sinusonasus</tp:taxon-name-part></tp:taxon-name></italic> are recovered as a paraphyletic assemblage. All Late Cretaceous troodontids are recovered as a monophyletic group, and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Almas">Almas</tp:taxon-name-part></tp:taxon-name></italic> is recovered as the earliest-diverging taxon of this clade, as in previous studies (<xref ref-type="bibr" rid="B33">Pei et al. 2017b</xref>, <xref ref-type="bibr" rid="B35">2021</xref>).</p>
            <fig id="F15">
              <object-id content-type="doi">10.3897/sjp.145.196379.figure15</object-id>
              <object-id content-type="arpha">FBAA40D1-3A9C-5F20-893E-21524C233EF8</object-id>
              <label>Figure 15.</label>
              <caption>
                <p>Phylogenetic reconstruction. Reduced topologies based on <bold>A</bold>. the strict consensus tree and <bold>B</bold>. the agreement subtree under equal weighting.</p>
              </caption>
              <graphic xlink:href="sjp-145-901_article-196379__-g015.jpg" id="oo_1763448.jpg">
                <uri content-type="original_file">https://binary.pensoft.net/fig/1763448</uri>
              </graphic>
            </fig>
            <p>To improve the topological resolution of the strict consensus tree obtained under equal weighting, the agreement subtree was also calculated (<xref ref-type="bibr" rid="B41">Tschopp and Upchurch 2018</xref>) (Fig. <xref ref-type="fig" rid="F15">15B</xref>). The agreement subtree routine implemented in TNT automatically pruned 27 phylogenetically unstable terminal taxa. Within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>, <abbrev content-type="institution" xlink:title="Mongolian Institute of Geology (Ulaan Baatar, Mongolia)">IGM</abbrev> 100/44 and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Byronosaurus">Byronosaurus</tp:taxon-name-part></tp:taxon-name></italic> were among the pruned unstable terminals. In the agreement subtree, <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is also recovered as the sister group of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> (Fig. <xref ref-type="fig" rid="F15">15B</xref>). <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic>, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic>, and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinusonasus">Sinusonasus</tp:taxon-name-part></tp:taxon-name></italic> exhibit well-resolved topological relationships. The topological relationships among the Late Cretaceous troodontids remain unchanged.</p>
            <p>The analysis under implied weighting (<italic>k</italic> = 15; <xref ref-type="bibr" rid="B5">Ezcurra 2024</xref>) produced 790 MPTs, with a length of 3,514 steps, CI = 0.308, and RI = 0.780. The topological relationships within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name> in the strict consensus tree derived from implied weighting are identical to those recovered under equal weighting. <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is again recovered as the sister group of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic>. Although the strict consensus trees from implied weighting and equal weighting show topological discrepancies for other clades, these differences lie beyond the primary focus of this study. Consistent with the strict consensus tree, the agreement subtree calculated under implied weighting recovers troodontid topological relationships identical to those from the equal-weighting analyses. Full topologies of the strict consensus trees and agreement subtrees recovered under equal weighting and implied weighting are provided in Suppl. material <xref ref-type="supplementary-material" rid="S2">2</xref>.</p>
          </sec>
          <sec sec-type="Osteohistological study" id="sec6">
            <title>Osteohistological study</title>
            <p>An osteohistological analysis was conducted to further determine the ontogenetic stage of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062. Osteohistological samples were taken from the right ulna at a fracture approximately 40.0 mm distal to its proximal end (Fig. <xref ref-type="fig" rid="F2">2</xref>).</p>
            <p>The thin section of the ulna has an elliptical shape, with the major axis measuring approximately 4.3 mm and the minor axis measuring approximately 3.6 mm (Fig. <xref ref-type="fig" rid="F16">16</xref>). The medullary cavity is large (2.8 mm × 2.1 mm). A distinct, thin internal circumferential layer of bone (endosteal lamellar bone, approximately 0.1 mm thick) is present, indicating that the expansion of the medullary cavity was nearly complete (<xref ref-type="bibr" rid="B40">Shen et al. 2017c</xref>; <xref ref-type="bibr" rid="B35">Pei et al. 2021</xref>). The cortex of the bone is primarily formed by fibrolamellar bone, with predominantly longitudinal vascular canals (Fig. <xref ref-type="fig" rid="F16">16A, B</xref>). The density of vascular canals and osteocytes decreases from the inner to the outer cortex (Fig. <xref ref-type="fig" rid="F16">16A, B</xref>). Secondary osteons (Haversian systems) are present in the inner cortex (Fig. <xref ref-type="fig" rid="F16">16C, D</xref>). Four lines of arrested growth (<abbrev xlink:title="lines of arrested growth">LAGs</abbrev>) are observed (Fig. <xref ref-type="fig" rid="F16">16C</xref>). The spacing among the outer three <abbrev xlink:title="lines of arrested growth">LAGs</abbrev> is extremely narrow, and this area is nearly avascular. This avascular area is interpreted here as the external fundamental system (<abbrev xlink:title="external fundamental system">EFS</abbrev>) (Fig. <xref ref-type="fig" rid="F16">16A, C</xref>). All osteohistological evidence indicates that <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 had almost attained its maximum somatic size when the individual died.</p>
            <fig id="F16">
              <object-id content-type="doi">10.3897/sjp.145.196379.figure16</object-id>
              <object-id content-type="arpha">FAFD42D5-1346-5360-BB25-9D8B46EF60C6</object-id>
              <label>Figure 16.</label>
              <caption>
                <p>Histological thin section of the right ulna of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (30 µm thick). Whole cross-section <bold>A, B</bold>. and enlarged image <bold>C, D</bold>. under plain and cross-polarized light. Green arrows point to <abbrev xlink:title="lines of arrested growth">LAGs</abbrev>. Abbreviations: <abbrev xlink:title="external fundamental system">EFS</abbrev>, external fundamental system; <abbrev xlink:title="endosteal lamella">el</abbrev>, endosteal lamella; <abbrev xlink:title="metacarpal">mc</abbrev>, medullary cavity; <abbrev xlink:title="secondary osteon">so</abbrev>, secondary osteon; <abbrev xlink:title="vascular canal">vc</abbrev>, vascular canal.</p>
              </caption>
              <graphic xlink:href="sjp-145-901_article-196379__-g016.jpg" id="oo_1763449.jpg">
                <uri content-type="original_file">https://binary.pensoft.net/fig/1763449</uri>
              </graphic>
            </fig>
          </sec>
        </tp:treatment-sec>
      </tp:taxon-treatment>
    </sec>
    <sec sec-type="Discussion" id="sec7">
      <title>Discussion</title>
      <sec sec-type="Taxonomic identification of SDUST-V1062 and comparisons with other Jehol troodontids" id="sec8">
        <title>Taxonomic identification of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 and comparisons with other Jehol troodontids</title>
        <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 can be referred to <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name> based on the combination of the following characters: the neural spines of the distal caudal vertebrae are absent, and the remaining midline sulci are centered on the neural arches; the presence of an asymmetrical foot with a slender metatarsal II and robust metatarsal IV; the distal end of metatarsal II is not ginglymoid; and manual phalanges III-1 and III-2 are subequal in length. These features are regarded as synapomorphies of <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name> in different studies (<xref ref-type="bibr" rid="B20">Makovicky and Norell 2004</xref>; <xref ref-type="bibr" rid="B45">Turner et al. 2012</xref>). Within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>, <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 shows affinity with early-diverging troodontids and differs from late-diverging troodontids based on the presence of a subarctometatarsalian pes and a slightly asymmetrical metatarsus, with metatarsal IV being slightly wider mediolaterally than metatarsal II.</p>
        <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is assigned to <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> in this study based on the presence of two pneumatic foramina on the lateral surface of the anterior cervical vertebrae (Fig. <xref ref-type="fig" rid="F4">4A, B, G, H</xref>), a diagnostic feature of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>). The phylogenetic analyses recovered <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 as the sister group of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic>, which further supports this view. In the holotype of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> (<abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615), a possible anterior cervical vertebra has been identified, and two similar pneumatic foramina are also developed (<xref ref-type="bibr" rid="B51">Xu 2002</xref>: fig. 39A). In contrast, another postcranial diagnostic feature of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> reported in <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583—a prominent lateral cnemial crest continuous with the fibular crest at the proximal end of the tibia—is absent in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 (<xref ref-type="bibr" rid="B55">Xu et al. 2002</xref>; <xref ref-type="bibr" rid="B61">Yin et al. 2018</xref>) (Fig. <xref ref-type="fig" rid="F11">11C</xref>). Notably, the proximal tibial morphology of the referred specimen of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> (<abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583) is possibly unusual: the proximal tibia is transversely expanded, in contrast to the anteroposteriorly elongated condition present in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 and other troodontids. Moreover, <abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12583 is relatively poorly preserved, which suggests that its proximal tibial morphology may have been affected by taphonomic processes. In summary, the presence of a prominent lateral cnemial crest continuous with the fibular crest at the proximal end of the tibia in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> remains uncertain, and the validity of this character requires further investigation.</p>
        <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 displays clear differences from other troodontids of the Jehol Biota. It differs from <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> in having a mediolaterally flat proximal pubic shaft, whereas the proximal end of the pubic shaft is significantly compressed anteroposteriorly in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>; <xref ref-type="bibr" rid="B7">Gao et al. 2012</xref>). In <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, the shafts of metatarsals II and IV are nearly parallel in posterior view and do not contact each other. In <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic>, however, metatarsals II and IV contact each other (<xref ref-type="bibr" rid="B52">Xu and Norell 2004</xref>). <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 differs from <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> by possessing a relatively short radius, approximately 65% of the humeral length, compared with 86% in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B14">Ji et al. 2005</xref>).</p>
        <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 can be distinguished from <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Daliansaurus">Daliansaurus</tp:taxon-name-part></tp:taxon-name></italic> by the presence of a small pedal ungual IV, with pedal ungual II being significantly larger than ungual IV, whereas pedal ungual IV is approximately the same size as pedal ungual II in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Daliansaurus">Daliansaurus</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B39">Shen et al. 2017b</xref>). <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 differs from <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> in possessing a short pedal digit I, with the distal end of ungual I reaching only the proximal end of the distal condyles of metatarsal III. In contrast, pedal digit I is proportionally long, and the distal end of ungual I extends beyond the distal end of metatarsal III in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic>. In addition, the length ratio of pedal phalanx I-1 to metatarsal I is 0.7 in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, whereas the ratio is 1.9 in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B60">Xu et al. 2017</xref>). Unlike in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic>, manual phalanx I-1 and metacarpal II of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 are subequal in length, whereas manual phalanx I-1 is longer than metacarpal II, and the length ratio of phalanx I-1 to metacarpal II is approximately 1.49 in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B38">Shen et al. 2017a</xref>). <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 differs from <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinusonasus">Sinusonasus</tp:taxon-name-part></tp:taxon-name></italic> in having a subarctometatarsalian pes rather than the fully arctometatarsalian condition (<xref ref-type="bibr" rid="B53">Xu and Wang 2004</xref>).</p>
        <p>As previously mentioned, <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 is attributed to <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> rather than being used to erect a new taxon until more fossil material becomes available or more comprehensive studies are conducted.</p>
      </sec>
      <sec sec-type="Notable new morphologies observed in SDUST-V1062" id="sec9">
        <title>Notable new morphologies observed in <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062</title>
        <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 shows anatomical characteristics that distinguish it from other troodontids. In Late Cretaceous troodontids such as <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B26">Norell et al. 2009</xref>), <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B42">Tsuihiji et al. 2014</xref>), and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Latenivenatrix">Latenivenatrix</tp:taxon-name-part></tp:taxon-name></italic> (<xref ref-type="bibr" rid="B46">Van der Reest and Currie 2017</xref>), the ambiens process at the proximal end of the pubis is clearly elongated anteroposteriorly and is longer than the ischial peduncle of the pubis (Fig. <xref ref-type="fig" rid="F17">17</xref>). However, because of the incomplete preservation of the pelvis, this feature is ambiguous in Early Cretaceous Jehol troodontids (<xref ref-type="bibr" rid="B46">Van der Reest and Currie 2017</xref>). Notably, the ambiens process appears to be absent in the holotype of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic> (Fig. <xref ref-type="fig" rid="F17">17A</xref>), although this could result from preservation. In <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, the ambiens process is moderately developed, and its anteroposterior length is less than that of the ischial peduncle of the pubis (Fig. <xref ref-type="fig" rid="F17">17B</xref>), unlike the condition in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic>, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Latenivenatrix">Latenivenatrix</tp:taxon-name-part></tp:taxon-name></italic>, and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic>. The moderately developed ambiens process of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 possibly represents the incipient stage of elongation of the ambiens process in troodontids, revealing an evolutionary trend toward anteroposterior lengthening of the ambiens process within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>.</p>
        <fig id="F17">
          <object-id content-type="doi">10.3897/sjp.145.196379.figure17</object-id>
          <object-id content-type="arpha">6F6EB868-9E83-5C60-BF5B-8341872F351C</object-id>
          <label>Figure 17.</label>
          <caption>
            <p>Proximal pubes of selected troodontids in lateral view. <bold>A</bold>. <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> (<abbrev content-type="institution" xlink:title="Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences (Beijing, China)">IVPP</abbrev> V12615); <bold>B</bold>. <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062; <bold>C</bold>. <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Gobivenator">Gobivenator</tp:taxon-name-part></tp:taxon-name></italic>; <bold>D</bold>. <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Latenivenatrix">Latenivenatrix</tp:taxon-name-part></tp:taxon-name></italic>; <bold>E</bold>. <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Saurornithoides">Saurornithoides</tp:taxon-name-part></tp:taxon-name></italic>. Abbreviations: <abbrev xlink:title="ambiens process">amp</abbrev>, ambiens process; <abbrev xlink:title="ischial peduncle of the pubis">ipp</abbrev>, ischial peduncle of the pubis.</p>
          </caption>
          <graphic xlink:href="sjp-145-901_article-196379__-g017.jpg" id="oo_1763450.jpg">
            <uri content-type="original_file">https://binary.pensoft.net/fig/1763450</uri>
          </graphic>
        </fig>
        <p>The ambiens process serves as the primary attachment site for M. ambiens and also bears attachment areas for M. obliquus abdominis and the pelvic ligaments (<xref ref-type="bibr" rid="B12">Hutchinson 2001</xref>; <xref ref-type="bibr" rid="B36">Rhodes et al. 2021</xref>). In dinosaurs, M. ambiens is one of the primary knee extensors (<xref ref-type="bibr" rid="B1">Allen et al. 2021</xref>), and the degree of development of its bony attachment directly governs the moment output of the hindlimb extensor complex and overall locomotor performance. Late Cretaceous troodontids possess anteroposteriorly elongated ambiens processes that lengthen the moment arm of M. ambiens, potentially improving their capacity for sustained running and weight-bearing. In contrast, the moderately developed ambiens process of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 provides a shorter moment arm, which may imply relatively limited sprinting and locomotor performance compared with Late Cretaceous troodontids.</p>
      </sec>
      <sec sec-type="Paleogeographic significance of SDUST-V1062" id="sec10">
        <title>Paleogeographic significance of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062</title>
        <p>In China, at least eight Early Cretaceous troodontid species have been reported, and most were reported from the Jehol Biota, except <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinornithoides">Sinornithoides</tp:taxon-name-part></tp:taxon-name></italic>, which was reported from the Ordos Basin (<xref ref-type="bibr" rid="B37">Russell and Dong 1993</xref>). <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic>, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinusonasus">Sinusonasus</tp:taxon-name-part></tp:taxon-name></italic>, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic>, <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Daliansaurus">Daliansaurus</tp:taxon-name-part></tp:taxon-name></italic>, and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Liaoningvenator">Liaoningvenator</tp:taxon-name-part></tp:taxon-name></italic> were discovered in the Lower Cretaceous Yixian Formation at Lujiatun, western Liaoning; <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jianianhualong">Jianianhualong</tp:taxon-name-part></tp:taxon-name></italic> was discovered in the Yixian Formation at Baicaigou, western Liaoning; and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> was discovered in the Lower Cretaceous Qiaotou Formation at Fengning, Hebei Province. <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 was collected from Ningcheng, Inner Mongolia, and the faunal composition and lithological features of the fossil beds are the same as those of the Lujiatun Unit of the Yixian Formation at Beipiao, western Liaoning (<xref ref-type="bibr" rid="B65">Zhang et al. 2022</xref>). The new specimen of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic> described here is the first record of a troodontid from the Jehol Biota in Inner Mongolia, which expands the geographical range of the troodontids of the Jehol Biota.</p>
      </sec>
      <sec sec-type="Body size variation within deinonychosaurians" id="sec11">
        <title>Body size variation within deinonychosaurians</title>
        <p>Body size influences many aspects of animal biology, including physiology, ecology, life history, and energetics, and extreme variation in body size reflects substantial divergence in the underlying biological processes (<xref ref-type="bibr" rid="B3">Benson et al. 2017</xref>). Body size change has previously been investigated in theropod dinosaurs, including deinonychosaurians (<xref ref-type="bibr" rid="B43">Turner et al. 2007</xref>; <xref ref-type="bibr" rid="B17">Lee et al. 2014</xref>; <xref ref-type="bibr" rid="B47">Wang et al. 2021</xref>). An updated body size dataset (Suppl. material <xref ref-type="supplementary-material" rid="S3">3</xref>), expanded from <xref ref-type="bibr" rid="B43">Turner et al. (2007)</xref>, was examined. Body size estimates were calculated using an empirical regression equation derived from femoral length. Among all measured specimens, only <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Wulong">Wulong</tp:taxon-name-part></tp:taxon-name></italic> likely represents a juvenile individual, whereas all remaining specimens were identified as subadults or adults in their original published studies. The results of the body size analyses indicate that troodontids range from 0.54 to 2.82 m in body length and from 0.36 to 61.64 kg in body mass. Early Cretaceous troodontids display limited body size variation, with estimated body lengths ranging from 0.54 to 1.24 m. In contrast, Late Cretaceous troodontids exhibit far greater variation, with body length estimates spanning 0.57–2.82 m. Among Jehol troodontids, most species have a body length of approximately 1 m, except for <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic> and <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Jinfengopteryx">Jinfengopteryx</tp:taxon-name-part></tp:taxon-name></italic> (Fig. <xref ref-type="fig" rid="F18">18</xref>), and <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 represents the largest known Jehol troodontid specimen (1.24 m and 4.53 kg). Body size estimates for dromaeosaurids range from 0.49 to 4.94 m in body length and from 0.26 to 368.70 kg in body mass. The body length of the largest dromaeosaurid is approximately 10.08 times that of the smallest, whereas this ratio is only approximately 5.22 in troodontids. This demonstrates that dromaeosaurids exhibit significantly greater size disparity than troodontids (Fig. <xref ref-type="fig" rid="F18">18</xref>). This pattern may reflect greater diversity in locomotion, ecological niches, or growth strategies in dromaeosaurids than in troodontids. A similar pattern is already evident in the Early Cretaceous Jehol Biota: the smallest known dromaeosaurid specimen (<italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Zhongjianosaurus">Zhongjianosaurus</tp:taxon-name-part></tp:taxon-name></italic>, 0.49 m) and troodontid specimen (<italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Mei">Mei</tp:taxon-name-part></tp:taxon-name></italic>, 0.54 m) exhibit comparable body lengths, whereas the largest known dromaeosaurid specimen (<abbrev content-type="institution" xlink:title="Shandong Tianyu Museum of Natural History (Linyi, China)">STM</abbrev> 1-3, a subadult of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Tianyuraptor">Tianyuraptor</tp:taxon-name-part></tp:taxon-name></italic>, 1.82 m) attains a substantially greater body length than the largest troodontid specimen (<abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062, 1.24 m).</p>
        <fig id="F18">
          <object-id content-type="doi">10.3897/sjp.145.196379.figure18</object-id>
          <object-id content-type="arpha">DD7ABCDE-4EFB-5738-9310-24AE4CCF484B</object-id>
          <label>Figure 18.</label>
          <caption>
            <p>Boxplot of body length in deinonychosaurians.</p>
          </caption>
          <graphic xlink:href="sjp-145-901_article-196379__-g018.jpg" id="oo_1763451.jpg">
            <uri content-type="original_file">https://binary.pensoft.net/fig/1763451</uri>
          </graphic>
        </fig>
      </sec>
    </sec>
    <sec sec-type="Conclusion" id="sec12">
      <title>Conclusion</title>
      <p><abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 from the Yixian Formation of the Ningcheng Basin, Inner Mongolia, China, is the first record of a troodontid from the Jehol Biota in this area. Based on the presence of two pneumatic foramina on the lateral surface of the anterior cervical vertebrae, this specimen is referred to <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic>. The results of the phylogenetic analyses further corroborate this evolutionary inference. This finding expands the paleogeographic distribution of this species. Moreover, <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062 shows a moderately developed pubic ambiens process, representing the first record of this feature in <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part> <tp:taxon-name-part taxon-name-part-type="species" reg="changii">changii</tp:taxon-name-part></tp:taxon-name></italic>. This trait differs from the anteroposteriorly elongated pubic ambiens processes seen in Late Cretaceous troodontids, indicating a gradual evolutionary trend toward lengthening of the ambiens process within <tp:taxon-name><tp:taxon-name-part taxon-name-part-type="family" reg="Troodontidae">Troodontidae</tp:taxon-name-part></tp:taxon-name>. Furthermore, body size comparisons within deinonychosaurians demonstrate substantially greater body size disparity among dromaeosaurids than among troodontids.</p>
    </sec>
  </body>
  <back>
    <ack>
      <title>Acknowledgments</title>
      <p>The authors thank Dr. Ya-Lei Yin (Shenyang Normal University, Shenyang, China) for his helpful discussions on the morphology of <italic><tp:taxon-name><tp:taxon-name-part taxon-name-part-type="genus" reg="Sinovenator">Sinovenator</tp:taxon-name-part></tp:taxon-name></italic>. The authors also thank Dr. Yu Peng (Zhejiang University, Hangzhou, China) for his assistance with the <abbrev xlink:title="computed tomography">CT</abbrev> scanning of this fossil and Qiang Yang, Shurui Yang, Shuai Shao, Peng Yu, and Yuguo Yang (all from the Paleontological Museum of Liaoning, Shenyang, China) for their assistance with field excavations and fossil preparation. The authors also thank Dr. Emanuel Tschopp and Dr. James Logan King for reviewing the paper and providing insightful comments.</p>
    </ack>
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    <sec sec-type="Additional information" id="sec13">
      <title>Additional information</title>
      <sec sec-type="Conflict of interest" id="sec14">
        <title>Conflict of interest</title>
        <p>The authors have declared that no competing interests exist.</p>
      </sec>
      <sec sec-type="Ethical statement" id="sec15">
        <title>Ethical statement</title>
        <p>No ethical statement was reported.</p>
      </sec>
      <sec sec-type="Artificial Intelligence (AI) use" id="sec16">
        <title>Artificial Intelligence (AI) use</title>
        <p>The authors accept full responsibility for the content of the manuscript, including the disclosure of any use of AI.</p>
        <p>No AI tools were used in the preparation of this manuscript.</p>
      </sec>
      <sec sec-type="Funding" id="sec17">
        <title>Funding</title>
        <p>This work was supported by the International Partnership Program of Chinese Academy of Sciences (Grant no. 052GJHZ2024029GC), the Taishan Scholar Program of Shandong Province (Grant no. tstp20240514), and the National Natural Science Foundation of China (Grant nos. 42372031 and 42288201).</p>
      </sec>
      <sec sec-type="Author contributions" id="sec18">
        <title>Author contributions</title>
        <p>Conceptualization: RP, CFZ. Data curation: CFZ, RP. Funding acquisition: CFZ, RP. Investigation: DY, CFZ, RP. Supervision: RP, CFZ. Validation: CFZ, RP, DY. Visualization: DY, RP, CFZ. Writing - original draft: CFZ, RP, DY. Writing - review and editing: DY, HZ, RP, CFZ.</p>
      </sec>
      <sec sec-type="Author ORCIDs" id="sec19">
        <title>Author ORCIDs</title>
        <p>D. Yu <ext-link xlink:href="https://orcid.org/0009-0002-9704-057X" ext-link-type="uri">https://orcid.org/0009-0002-9704-057X</ext-link></p>
        <p>H. Zhang <ext-link xlink:href="https://orcid.org/0009-0008-2587-0770" ext-link-type="uri">https://orcid.org/0009-0008-2587-0770</ext-link></p>
        <p>C.-F. Zhou <ext-link xlink:href="https://orcid.org/0000-0002-3744-7573" ext-link-type="uri">https://orcid.org/0000-0002-3744-7573</ext-link></p>
        <p>R. Pei <ext-link xlink:href="https://orcid.org/0000-0002-5954-0728" ext-link-type="uri">https://orcid.org/0000-0002-5954-0728</ext-link></p>
      </sec>
      <sec sec-type="Data availability" id="sec20">
        <title>Data availability</title>
        <p>A total of 2,501 TIFF slices forming a single image stack, along with the 3D models of the cervical vertebrae, have been deposited in ADMorph (<ext-link xlink:href="10.12112/R.44.Fossil" ext-link-type="doi">https://doi.org/10.12112/R.44.Fossil</ext-link>). Original X-ray projection data were not archived during <abbrev xlink:title="computed tomography">CT</abbrev> data acquisition and therefore have not been deposited. The morphological matrix and tree files for the phylogenetic analyses can be accessed via MorphoBank (<ext-link xlink:href="https://www.morphobank.org/permalink/?P6437" ext-link-type="uri">https://www.morphobank.org/permalink/?P6437</ext-link>). <abbrev xlink:title="computed tomography">CT</abbrev>-rendered images of the proatlas, atlas, and axis; full topologies derived from the phylogenetic analyses; and the body size dataset for deinonychosaurians are provided in Suppl. materials of this article.</p>
      </sec>
    </sec>
    <sec sec-type="supplementary-material">
      <title>Supplementary materials</title>
      <supplementary-material id="S1" position="float" orientation="portrait" xlink:type="simple">
        <object-id content-type="doi">10.3897/sjp.145.196379.suppl1</object-id>
        <object-id content-type="arpha">4A2559AE-333A-5627-AAE8-55D998A70836</object-id>
        <label>Supplementary material 1</label>
        <caption>
          <p><abbrev xlink:title="computed tomography">CT</abbrev>-rendered images of proatlas, atlas, and axis of <abbrev content-type="institution" xlink:title="Vertebrate Palaeontological Collection of College of Earth Science and Engineering, Shandong University of Science and Technology (Qingdao, China)">SDUST</abbrev>-V1062</p>
        </caption>
        <statement content-type="dataType">
          <label>Data type</label>
          <p>jpg</p>
        </statement>
        <statement content-type="notes">
          <label>Explanation note</label>
          <p>(A, B) lateral view, (C) anterior view, (D) posterior view, (E) dorsal view, (F) ventral view. Abbreviations: <abbrev xlink:title="atlantal intercentrum">ainc</abbrev>, atlantal intercentrum; <abbrev xlink:title="atlantal neural arch">anar</abbrev>, atlantal neural arch; <abbrev xlink:title="axis">ax</abbrev>, axis; <abbrev xlink:title="epipophysis">ep</abbrev>, epipophysis; <abbrev xlink:title="odontoid">od</abbrev>, odontoid; <abbrev xlink:title="posterior articular facet of the centrum">paf</abbrev>, posterior articular facet of the centrum; <abbrev xlink:title="proatlas">proa</abbrev>, proatlas; <abbrev xlink:title="spinopostzygapophyseal fossa">spof</abbrev>, spinopostzygapophyseal fossa; <abbrev xlink:title="spinopostzygapophyseal laminae">spol</abbrev>, spinopostzygapophyseal laminae.</p>
        </statement>
        <media xlink:href="sjp-145-901_article-196379__-s001.jpg" mimetype="image" mime-subtype="jpeg" position="float" orientation="portrait" id="oo_1763452.jpg">
          <uri content-type="original_file">https://binary.pensoft.net/file/1763452</uri>
        </media>
        <permissions>
          <license>
            <license-p>This dataset is made available under the Open Database License (<ext-link ext-link-type="uri" xlink:href="http://opendatacommons.org/licenses/odbl/1.0">http://opendatacommons.org/licenses/odbl/1.0</ext-link>). The Open Database License (ODbL) is a license agreement intended to allow users to freely share, modify, and use this Dataset while maintaining this same freedom for others, provided that the original source and author(s) are credited.</license-p>
          </license>
        </permissions>
        <attrib specific-use="authors"> Dongxiang Yu, Honggang Zhang, Chang‑Fu Zhou, Rui Pei</attrib>
      </supplementary-material>
      <supplementary-material id="S2" position="float" orientation="portrait" xlink:type="simple">
        <object-id content-type="doi">10.3897/sjp.145.196379.suppl2</object-id>
        <object-id content-type="arpha">93B7EF6F-517B-5C24-9924-A1CD4B81C82E</object-id>
        <label>Supplementary material 2</label>
        <caption>
          <p>Full topologies of strict consensus trees and agreement subtrees recovered under equal weighting and implied weighting</p>
        </caption>
        <statement content-type="dataType">
          <label>Data type</label>
          <p>zip</p>
        </statement>
        <media xlink:href="sjp-145-901_article-196379__-s002.zip" mimetype="application" mime-subtype="zip" position="float" orientation="portrait" id="oo_1763453.zip">
          <uri content-type="original_file">https://binary.pensoft.net/file/1763453</uri>
        </media>
        <permissions>
          <license>
            <license-p>This dataset is made available under the Open Database License (<ext-link ext-link-type="uri" xlink:href="http://opendatacommons.org/licenses/odbl/1.0">http://opendatacommons.org/licenses/odbl/1.0</ext-link>). The Open Database License (ODbL) is a license agreement intended to allow users to freely share, modify, and use this Dataset while maintaining this same freedom for others, provided that the original source and author(s) are credited.</license-p>
          </license>
        </permissions>
        <attrib specific-use="authors"> Dongxiang Yu, Honggang Zhang, Chang‑Fu Zhou, Rui Pei</attrib>
      </supplementary-material>
      <supplementary-material id="S3" position="float" orientation="portrait" xlink:type="simple">
        <object-id content-type="doi">10.3897/sjp.145.196379.suppl3</object-id>
        <object-id content-type="arpha">58786CEA-1B2C-58BA-8FDF-15B003CD2AD8</object-id>
        <label>Supplementary material 3</label>
        <caption>
          <p>The body size dataset in deinonychosaurians</p>
        </caption>
        <statement content-type="dataType">
          <label>Data type</label>
          <p>xlsx</p>
        </statement>
        <media xlink:href="sjp-145-901_article-196379__-s003.xlsx" mimetype="application" mime-subtype="vnd.openxmlformats-officedocument.spreadsheetml.sheet" position="float" orientation="portrait" id="oo_1763454.xlsx">
          <uri content-type="original_file">https://binary.pensoft.net/file/1763454</uri>
        </media>
        <permissions>
          <license>
            <license-p>This dataset is made available under the Open Database License (<ext-link ext-link-type="uri" xlink:href="http://opendatacommons.org/licenses/odbl/1.0">http://opendatacommons.org/licenses/odbl/1.0</ext-link>). The Open Database License (ODbL) is a license agreement intended to allow users to freely share, modify, and use this Dataset while maintaining this same freedom for others, provided that the original source and author(s) are credited.</license-p>
          </license>
        </permissions>
        <attrib specific-use="authors"> Dongxiang Yu, Honggang Zhang, Chang‑Fu Zhou, Rui Pei</attrib>
      </supplementary-material>
    </sec>
  </back>
</article>
