Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology

Rich tetrapod ichnofaunas, known for more than a decade, from the Huangyangquan Reservoir (Wuerhe District, Karamay City, Xinjiang) have been an abundant source of some of the largest Lower Cretaceous track collections from China. They originate from inland lacustrine clastic exposures of the 581–87...

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Main Authors: Lida Xing, Martin G. Lockley, Chengkai Jia, Hendrik Klein, Kecheng Niu, Lijun Zhang, Liqi Qi, Chunyong Chou, Anthony Romilio, Donghao Wang, Yu Zhang, W Scott Persons, Miaoyan Wang
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Language:English
Published: PeerJ Inc. 2021-05-01
Series:PeerJ
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Online Access:https://peerj.com/articles/11476.pdf
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author Lida Xing
Martin G. Lockley
Chengkai Jia
Hendrik Klein
Kecheng Niu
Lijun Zhang
Liqi Qi
Chunyong Chou
Anthony Romilio
Donghao Wang
Yu Zhang
W Scott Persons
Miaoyan Wang
author_facet Lida Xing
Martin G. Lockley
Chengkai Jia
Hendrik Klein
Kecheng Niu
Lijun Zhang
Liqi Qi
Chunyong Chou
Anthony Romilio
Donghao Wang
Yu Zhang
W Scott Persons
Miaoyan Wang
author_sort Lida Xing
collection DOAJ
description Rich tetrapod ichnofaunas, known for more than a decade, from the Huangyangquan Reservoir (Wuerhe District, Karamay City, Xinjiang) have been an abundant source of some of the largest Lower Cretaceous track collections from China. They originate from inland lacustrine clastic exposures of the 581–877 m thick Tugulu Group, variously divided into four formations and subgroups in the northwestern margin of the Junggar Basin. The large Huangyangquan track assemblages occur in the Lower layer/Subgroup II. Similarly-composed track assemblages also occur at the smaller Asphaltite site in the Upper Layer/Subgroup III. The Huangyangquan assemblages have yielded more than 1,500 identified tracks including abundant tracks of avian and non-avian theropods, pterosaurs and turtles and less abundant tracks of stegosaurs. Previous avian track identifications have been reassessed to conclude that Moguiornipes robustus is a taphotaxon and Koreanaornis dodsoni might be better accommodated in the ichnogenus Aquatilavipes which appears to be the dominant avian ichnotaxon. The avian track Ignotornis is also recognized and represents the first occurrence of this ichnogenus in China. Although the Huangyangquan assemblages lack some of the larger components (e.g., sauropodan and ornithopodan tracks) known from other Lower Cretaceous localities, the association of abundant tracks of smaller tetrapods (avian and non-avian theropods, pterosaurs and turtles) appears to be representative of lacustrine basin faunas of this region, and are an excellent example of the shorebird ichnocoenosis/ichnofacies concept. This is the first comprehensive review and re-analysis of an important Lower Cretaceous ecosystem.
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spelling doaj.art-099227af756647209cee8e9c12bff0772023-12-02T21:54:57ZengPeerJ Inc.PeerJ2167-83592021-05-019e1147610.7717/peerj.11476Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecologyLida Xing0Martin G. Lockley1Chengkai Jia2Hendrik Klein3Kecheng Niu4Lijun Zhang5Liqi Qi6Chunyong Chou7Anthony Romilio8Donghao Wang9Yu Zhang10W Scott Persons11Miaoyan Wang12State Key Laboratory of Biogeology and Environmental Geology, China University of Geoscience (Beijing), Beijing, ChinaDinosaur Trackers Research Group, University of Colorado at Denver, Denver, United StatesResearch Institute of Experiment and Detection of Xinjiang Oil Company, PetroChina, Karamay, ChinaSaurierwelt Paläontologisches Museum, Neumarkt, GermanyYingliang Stone Natural History Museum, Nan’an, ChinaInstitute of Resources and Environment, Key Laboratory of Biogenic Traces & Sedimentary Minerals of Henan Province, Collaborative Innovation Center of Coalbed Methane and Shale Gas for Central Plains Economic Region, Henan Polytechnic University, Jiaozuo, ChinaFaculty of Petroleum, China University of Petroleum (Beijing) at Karamay, Karamay, ChinaSchool of the Earth Sciences and Resources, China University of Geoscience (Beijing), Beijing, ChinaSchool of Biological Sciences, The University of Queensland, Brisbane, AustraliaSchool of the Earth Sciences and Resources, China University of Geoscience (Beijing), Beijing, ChinaSchool of the Earth Sciences and Resources, China University of Geoscience (Beijing), Beijing, ChinaMace Brown Museum of Natural History, Department of Geology and Environmental Geosciences, College of Charleston, Charleston, United StatesSchool of the Earth Sciences and Resources, China University of Geoscience (Beijing), Beijing, ChinaRich tetrapod ichnofaunas, known for more than a decade, from the Huangyangquan Reservoir (Wuerhe District, Karamay City, Xinjiang) have been an abundant source of some of the largest Lower Cretaceous track collections from China. They originate from inland lacustrine clastic exposures of the 581–877 m thick Tugulu Group, variously divided into four formations and subgroups in the northwestern margin of the Junggar Basin. The large Huangyangquan track assemblages occur in the Lower layer/Subgroup II. Similarly-composed track assemblages also occur at the smaller Asphaltite site in the Upper Layer/Subgroup III. The Huangyangquan assemblages have yielded more than 1,500 identified tracks including abundant tracks of avian and non-avian theropods, pterosaurs and turtles and less abundant tracks of stegosaurs. Previous avian track identifications have been reassessed to conclude that Moguiornipes robustus is a taphotaxon and Koreanaornis dodsoni might be better accommodated in the ichnogenus Aquatilavipes which appears to be the dominant avian ichnotaxon. The avian track Ignotornis is also recognized and represents the first occurrence of this ichnogenus in China. Although the Huangyangquan assemblages lack some of the larger components (e.g., sauropodan and ornithopodan tracks) known from other Lower Cretaceous localities, the association of abundant tracks of smaller tetrapods (avian and non-avian theropods, pterosaurs and turtles) appears to be representative of lacustrine basin faunas of this region, and are an excellent example of the shorebird ichnocoenosis/ichnofacies concept. This is the first comprehensive review and re-analysis of an important Lower Cretaceous ecosystem.https://peerj.com/articles/11476.pdfTetrapod ichnofaunasShorebird tracksJunggar BasinTugulu GroupTheropodThyreophoran
spellingShingle Lida Xing
Martin G. Lockley
Chengkai Jia
Hendrik Klein
Kecheng Niu
Lijun Zhang
Liqi Qi
Chunyong Chou
Anthony Romilio
Donghao Wang
Yu Zhang
W Scott Persons
Miaoyan Wang
Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology
PeerJ
Tetrapod ichnofaunas
Shorebird tracks
Junggar Basin
Tugulu Group
Theropod
Thyreophoran
title Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology
title_full Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology
title_fullStr Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology
title_full_unstemmed Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology
title_short Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology
title_sort lower cretaceous avian dominated theropod thyreophoran pterosaur and turtle track assemblages from the tugulu group xinjiang china ichnotaxonomy and palaeoecology
topic Tetrapod ichnofaunas
Shorebird tracks
Junggar Basin
Tugulu Group
Theropod
Thyreophoran
url https://peerj.com/articles/11476.pdf
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