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Eubrontes and Anomoepus Track
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 345 EUBRONTES AND ANOMOEPUS TRACK ASSEMBLAGES FROM THE MIDDLE JURASSIC XIASHAXIMIAO FORMATION OF ZIZHONG COUNTY, SICHUAN, CHINA: REVIEW, ICHNOTAXONOMY AND NOTES ON PRESERVED TAIL TRACES LIDA XING1, MARTIN G. LOCKLEY2, GUANGZHAO PENG3, YONG YE3, JIANPING ZHANG1, MASAKI MATSUKAWA4, HENDRIK KLEIN5, RICHARD T. MCCREA6 and W. SCOTT PERSONS IV7 1School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; -email: [email protected]; 2Dinosaur Trackers Research Group, University of Colorado Denver, P.O. Box 173364, Denver, CO 80217; 3 Zigong Dinosaur Museum, Zigong 643013, Sichuan, China; 4 Department of Environmental Sciences, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan; 5 Saurierwelt Paläontologisches Museum Alte Richt 7, D-92318 Neumarkt, Germany; 6 Peace Region Palaeontology Research Centre, Box 1540, Tumbler Ridge, British Columbia V0C 2W0, Canada; 7 Department of Biological Sciences, University of Alberta 11455 Saskatchewan Drive, Edmonton, Alberta T6G 2E9, Canada Abstract—The Nianpanshan dinosaur tracksite, first studied in the 1980s, was designated as the type locality of the monospecific ichnogenus Jinlijingpus, and the source of another tridactyl track, Chuanchengpus, both presumably of theropod affinity. After the site was mapped in 2001, these two ichnotaxa were considered synonyms of Eubrontes and Anomoepus, respectively, the latter designation being the first identification of this ichnogenus in China. The assemblage indicates a typical Jurassic ichnofauna. The present study reinvestigates the site in the light of the purported new ichnospecies Chuanchengpus shenglingensis that was introduced in 2012. After re- evaluation of the morphological and extramorphological features, C. -
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A couple of partially-feathered creatures about the The Outside Story size of a turkey pop out of a stand of ferns. By the water you spot a flock of bigger animals, lean and predatory, catching fish. And then an even bigger pair of animals, each longer than a car, with ostentatious crests on their heads, stalk out of the heat haze. The fish-catchers dart aside, but the new pair have just come to drink. We can only speculate what a walk through Jurassic New England would be like, but the fossil record leaves many hints. According to Matthew Inabinett, one of the Beneski Museum of Natural History’s senior docents and a student of vertebrate paleontology, dinosaur footprints found in the sedimentary rock of the Connecticut Valley reveal much about these animals and their environment. At the time, the land that we know as New England was further south, close to where Cuba is now. A system of rift basins that cradled lakes ran right through our region, from North Carolina to Nova Scotia. As reliable sources of water, with plants for the herbivores and fish for the carnivores, the lakes would have been havens of life. While most of the fossil footprints found in New England so far are in the lower Connecticut Valley, Dinosaur Tracks they provide a window into a world that extended throughout the region. According to Inabinett, the By: Rachel Marie Sargent tracks generally fall into four groupings. He explained that these names are for the tracks, not Imagine taking a walk through a part of New the dinosaurs that made them, since, “it’s very England you’ve never seen—how it was 190 million difficult, if not impossible, to match a footprint to a years ago. -
Mini Revision 20160403.Compressed
Xing, L., Lockley, M. G., Yang, G., Cao, J., Benton, M. J., Xu, X., Zhang, J., Klein, H., Persons IV, W. S., Kim, J. Y., Peng, G., Ye, Y., & Ran, H. (2016). A new Minisauripus site from the Lower Cretaceous of China: Tracks of small adults or juveniles? Palaeogeography, Palaeoclimatology, Palaeoecology, 452, 28-39. https://doi.org/10.1016/j.palaeo.2016.04.006 Peer reviewed version License (if available): CC BY-NC-ND Link to published version (if available): 10.1016/j.palaeo.2016.04.006 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via Elsevier at http://www.sciencedirect.com/science/article/pii/S0031018216300608. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ 1 1 A new Minisauripus site from the Lower Cretaceous of China: tracks of small adults or juveniles? 2 3 Lida Xing a, Martin G. Lockley b, Geng Yang c, Jun Cao c, Michael Benton d, Xing Xu e, Jianping Zhang a, 4 Hendrik Klein f, W. Scott Persons IV g, Jeong Yul Kim h, Guangzhao Peng i, Yong Ye i, Hao Ran j 5 6 a School of the Earth Sciences and Resources, China University of Geosciences, Beijing, China, 7 b Dinosaur Trackers Research -
Tetrapod Track Assemblages from Lower Cretaceous Desert Facies In
Palaeogeography, Palaeoclimatology, Palaeoecology 507 (2018) 1–14 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Tetrapod track assemblages from Lower Cretaceous desert facies in the Ordos Basin, Shaanxi Province, China, and their implications for Mesozoic T paleoecology ⁎ Lida Xinga,b,c, Martin G. Lockleyd, , Yongzhong Tange, Anthony Romiliof, Tao Xue, Xingwen Lie, Yu Tange, Yizhao Lie a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China b School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China c State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China d Dinosaur Trackers Research Group, CB 172, University of Colorado at Denver, PO Box 173364, Denver, CO 80217-3364, USA e Shaanxi Geological Survey, Xi'an 710054, Shaanxi, China f School of Biological Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia ARTICLE INFO ABSTRACT Keywords: Tetrapod ichnofaunas are reported from desert, playa lake facies in the Lower Cretaceous Luohe Formation at Ichnofacies Baodaoshili, Shaanxi Province, China, which represent the first Asian example of an ichnnofauna typical of the Brasilichnium Chelichnus Ichnofacies (Brasilichnium sub-ichnofacies) characteristic of desert habitats. The mammaliomorph Sarmientichnus tracks, assigned to Brasilichnium, -
The First Record of Anomoepus Tracks from the Middle Jurassic of Henan Province, Central China
Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: http://www.tandfonline.com/loi/ghbi20 The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China Lida Xing, Nasrollah Abbassi, Martin G. Lockley, Hendrik Klein, Songhai Jia, Richard T. McCrea & W. Scott Persons IV To cite this article: Lida Xing, Nasrollah Abbassi, Martin G. Lockley, Hendrik Klein, Songhai Jia, Richard T. McCrea & W. Scott Persons IV (2016): The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China, Historical Biology, DOI: 10.1080/08912963.2016.1149480 To link to this article: http://dx.doi.org/10.1080/08912963.2016.1149480 Published online: 22 Feb 2016. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Download by: [Lida Xing] Date: 22 February 2016, At: 05:53 HISTORICAL BIOLOGY, 2016 http://dx.doi.org/10.1080/08912963.2016.1149480 The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China Lida Xinga, Nasrollah Abbassib, Martin G. Lockleyc, Hendrik Kleind, Songhai Jiae, Richard T. McCreaf and W. Scott PersonsIVg aSchool of the Earth Sciences and Resources, China University of Geosciences, Beijing, China; bFaculty of Sciences, Department of Geology, University of Zanjan, Zanjan, Iran; cDinosaur Tracks Museum, University of Colorado Denver, Denver, CO, USA; dSaurierwelt Paläontologisches Museum, Neumarkt, Germany; eHenan Geological Museum, Henan Province, China; fPeace Region Palaeontology Research Centre, British Columbia, Canada; gDepartment of Biological Sciences, University of Alberta, Edmonton, Canada ABSTRACT ARTICLE HISTORY Small, gracile mostly tridactyl tracks from the Middle Jurassic of Henan Province represent the first example Received 30 December 2015 of the ichnogenus Anomoepus from this region. -
Lower Cretaceous Avian-Dominated, Theropod
Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology Lida Xing1,2, Martin G. Lockley3, Chengkai Jia4, Hendrik Klein5, Kecheng Niu6, Lijun Zhang7, Liqi Qi8, Chunyong Chou2, Anthony Romilio9, Donghao Wang2, Yu Zhang2, W Scott Persons10 and Miaoyan Wang2 1 State Key Laboratory of Biogeology and Environmental Geology, China University of Geoscience (Beijing), Beijing, China 2 School of the Earth Sciences and Resources, China University of Geoscience (Beijing), Beijing, China 3 Dinosaur Trackers Research Group, University of Colorado at Denver, Denver, United States 4 Research Institute of Experiment and Detection of Xinjiang Oil Company, PetroChina, Karamay, China 5 Saurierwelt Paläontologisches Museum, Neumarkt, Germany 6 Yingliang Stone Natural History Museum, Nan’an, China 7 Institute 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, China 8 Faculty of Petroleum, China University of Petroleum (Beijing) at Karamay, Karamay, China 9 School of Biological Sciences, The University of Queensland, Brisbane, Australia 10 Mace Brown Museum of Natural History, Department of Geology and Environmental Geosciences, College of Charleston, Charleston, United States ABSTRACT Rich tetrapod ichnofaunas, known for more than a decade, from the Huangyangquan Reservoir (Wuerhe District, Karamay City, Xinjiang) have been an abundant source Submitted 10 January 2021 of some of the largest Lower Cretaceous track collections from China. They originate Accepted 26 April 2021 from inland lacustrine clastic exposures of the 581–877 m thick Tugulu Group, 28 May 2021 Published variously divided into four formations and subgroups in the northwestern margin of Corresponding author the Junggar Basin. -
The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus
19 The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus Paul E. Olsen and Emma C. Rainforth nomoepus is an Early Jurassic footprint genus and 19.2). Because skeletons of dinosaur feet were not produced by a relatively small, gracile orni- known at the time, he naturally attributed the foot- A thischian dinosaur. It has a pentadactyl ma- prints to birds. By 1848, however, he recognized that nus and a tetradactyl pes, but only three pedal digits some of the birdlike tracks were associated with im- normally impressed while the animal was walking. The pressions of five-fingered manus, and he gave the name ichnogenus is diagnosed by having the metatarsal- Anomoepus, meaning “unlike foot,” to these birdlike phalangeal pad of digit IV of the pes lying nearly in line with the axis of pedal digit III in walking traces, in combination with a pentadactyl manus. It has a pro- portionally shorter digit III than grallatorid (theropod) tracks, but based on osteometric analysis, Anomoepus, like grallatorids, shows a relatively shorter digit III in larger specimens. Anomoepus is characteristically bi- pedal, but there are quadrupedal trackways and less common sitting traces. The ichnogenus is known from eastern and western North America, Europe, and southern Africa. On the basis of a detailed review of classic and new material, we recognize only the type ichnospecies Anomoepus scambus within eastern North America. Anomoepus is known from many hundreds of specimens, some with remarkable preservation, showing many hitherto unrecognized details of squa- mation and behavior. . Pangea at approximately 200 Ma, showing the In 1836, Edward Hitchcock described the first of what areas producing Anomoepus discussed in this chapter: 1, Newark we now recognize as dinosaur tracks from Early Juras- Supergroup, eastern North America; 2, Karoo basin; 3, Poland; sic Newark Supergroup rift strata of the Connecticut 4, Colorado Plateau. -
Ichnotaxonomy of the Eocene Green River Formation
Ichnotaxonomy of the Eocene Green River Formation, Soldier Summit and Spanish Fork Canyon, Uinta Basin, Utah: Interpreting behaviors, lifestyles, and erecting the Cochlichnus Ichnofacies By © 2018 Joshua D. Hogue B.S. Old Dominion University, 2013 Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Science. Chair: Dr. Stephen T. Hasiotis Dr. Paul Selden Dr. Georgios Tsoflias Date Defended: May 1, 2018 ii The thesis committee for Joshua D. Hogue certifies that this is the approved version of the following thesis: Ichnotaxonomy of the Eocene Green River Formation, Soldier Summit and Spanish Fork Canyon, Uinta Basin, Utah: Interpreting behaviors, lifestyles, and erecting the Cochlichnus Ichnofacies Chair: Dr. Stephen T. Hasiotis Date Approved: May 1, 2018 iii ABSTRACT The Eocene Green River Formation in the Uinta Basin, Utah, has a diverse ichnofauna. Nineteen ichnogenera and 26 ichnospecies were identified: Acanthichnus cursorius, Alaripeda lofgreni, c.f. Aquatilavipes isp., Aulichnites (A. parkerensis and A. tsouloufeidos isp. nov.), Aviadactyla (c.f. Av. isp. and Av. vialovi), Avipeda phoenix, Cochlichnus (C. anguineus and C. plegmaeidos isp. nov.), Conichnus conichnus, Fuscinapeda texana, Glaciichnium liebegastensis, Glaroseidosichnus ign. nov. gierlowskii isp. nov., Gruipeda (G. fuenzalidae and G. gryponyx), Midorikawapeda ign. nov. semipalmatus isp. nov., Planolites montanus, Presbyorniformipes feduccii, Protovirgularia dichotoma, Sagittichnus linki, Treptichnus (T. bifurcus, T. pedum, and T. vagans), and Tsalavoutichnus ign. nov. (Ts. ericksonii isp. nov. and Ts. leptomonopati isp. nov.). Four ichnocoenoses are represented by the ichnofossils—Cochlichnus, Conichnus, Presbyorniformipes, and Treptichnus—representing dwelling, feeding, grazing, locomotion, predation, pupation, and resting behaviors of organisms in environments at and around the sediment-water-air interface. -
New Excavations at the Mill Canyon Dinosaur Track Site (Cedar Mountain Formation, Lower Cretaceous) of Eastern Utah
287 Lockley, M.G. & Lucas, S.G., eds., 2014, Fossil footprints of western North America: NMMNHS Bulletin 62 NEW EXCAVATIONS AT THE MILL CANYON DINOSAUR TRACK SITE (CEDAR MOUNTAIN FORMATION, LOWER CRETACEOUS) OF EASTERN UTAH MARTIN G. LOCKLEY1, GERARD D. GIERLINSKI2,3, KAREN HOUCK1, JONG-DEOCK LIM4, KYUNG SOO KIM5, DAL-YONG KIM4, TAE HYEONG KIM4, SEUNG-HYEOP KANG5, REBECCA HUNT FOSTER6, RIHUI LI7, CHRISTOPHER CHESSSER6, ROB GAY6, ZOFIA DUBICKA2, 8, KEN CART9 AND CHRISTY WRIGHT 9 1Dinosaur Tracks Museum, University of Colorado at Denver, PO Box 173364, Denver, Colorado, 80217. [email protected]; 2 JuraPark, ul. Sandomierska 4, 27-400 Ostrowiec Swiztokrzyski, Poland; 3Moab Giants, PO Box 573, Moab, Utah 84532; 4Natural Heritage Center, National Research Institute of Cultural Heritage, 927 Yudeng-ro, Seo-gu, Daejon, 302-834, Korea; 5 Department of Science Education, Chinju National University of Education, Jinju, Kyungnam, 660-756, Korea; 6Moab District Field Office, Bureau of Land Management, Moab, Utah; 7Qingdao Institute of Marine Geology, Qingdao, China; 8Faculty of Geology, University of Warsaw, Al. Zwirki i Wigury 93, PL-02-089 Warsaw, Poland; 93072 Bison Avenue, Grand Junction, Colorado 81504 Abstract—The discovery of the Mill Canyon Dinosaur Tracksite (MCDT) in the Cedar Mountain Formation (Ruby Ranch Member), near Moab in eastern Utah, has generated considerable interest. Following the completion of a preliminary study of natural exposures, reported elsewhere in this volume, an international team was assembled to excavate the site in 2013. Complementary to the preliminary report published elsewhere in this volume, we here outline the initial cartographic results of the 2013 excavation in order to show the extent of the exposed track-bearing surface, the diversity of track types and the excellent potential for further development of the site. -
Bifurculapes Hitchcock 1858: a Revision of the Ichnogenus
Document généré le 28 sept. 2021 10:48 Atlantic Geology Bifurculapes Hitchcock 1858 a revision of the ichnogenus Patrick R. Getty Volume 52, 2016 Résumé de l'article Les caractéristiques qui différencient la piste d’arthropode Bifurculapes des URI : https://id.erudit.org/iderudit/ageo52art10 ichnogenres Lithographus et Copeza similaires sont la position, la disposition et l’orientation des traces à l’intérieur de la série. Parmi les cinq espèces de Aller au sommaire du numéro Bifurculapes originalement décrites, seules Bifurculapes laqueatus et Bifurculapes scolopendroideus sont ici reconnues. Les trois autres ichnoespèces sont considérées comme nomina dubia ou comme synonymes subjectifs plus Éditeur(s) récents de Bifurculapes laqueatus. Les deux nouveaux spécimens trouvés dans la formation du Jurassique précoce d’East Berlin dans le bassin de Hartford, à Atlantic Geoscience Society Holyoke, au Massachusetts, représentent seulement la seconde présence sans équivoque de l’ichnogenre à l’extérieur du bassin de Deerfield. À l’heure ISSN actuelle, Bifurculapes n’est associé qu’au Jurassique précoce. 0843-5561 (imprimé) [Traduit par la redaction] 1718-7885 (numérique) Découvrir la revue Citer cet article Getty, P. R. (2016). Bifurculapes Hitchcock 1858: a revision of the ichnogenus. Atlantic Geology, 52, 247–255. All rights reserved © Atlantic Geology, 2016 Ce document est protégé par la loi sur le droit d’auteur. L’utilisation des services d’Érudit (y compris la reproduction) est assujettie à sa politique d’utilisation que vous pouvez consulter en ligne. https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Cet article est diffusé et préservé par Érudit. Érudit est un consortium interuniversitaire sans but lucratif composé de l’Université de Montréal, l’Université Laval et l’Université du Québec à Montréal. -
Cretaceous Research 74 (2017) 155E164
Cretaceous Research 74 (2017) 155e164 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Mid-Cretaceous dinosaur track assemblage from the Tongfosi Formation of China: Comparison with the track assemblage of South Korea * Lida Xing a, b, , Martin G. Lockley c, Kyung Soo Kim d, Hendrik Klein e, Masaki Matsukawa f, Jong Deock Lim g, W. Scott Persons IV h, Xing Xu i a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China b School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China c Dinosaur Trackers Research Group, University of Colorado Denver, PO Box 173364, Denver, CO 80217, USA d Department of Science Education, Chinju National University of Education, Shinan-dong, Jinju, Kyungnam 660-756, South Korea e Saurierwelt Palaontologisches€ Museum, Alte Richt 7, D-92318 Neumarkt, Germany f Department of Environmental Sciences, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan g Natural Heritage Center, National Research Institute of Cultural Heritage, 927 Yudeng-ro, Seo-gu, Daejon 302-834, South Korea h Department of Biological Sciences, University of Alberta, 11455 Saskatchewan Drive, Edmonton, Alberta T6G 2E9, Canada i Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China article info abstract Article history: A Yanji Basin tracksite in the Cretaceous Tongfosi Formation in the Yanbian Korean Autonomous Pre- Received 14 October 2016 fecture, Jilin Province was reinvestigated twenty years after the original study. Received in revised form The re-examination confirms the presence of tracks tentatively referred to ornithopods and theropod 15 February 2017 tracks including several not previously reported. -
Durlachia Striata Gen. Nov., Spec. Nov., a New Beetle (Coleoptera) from the Upper Buntsand- Stein (German Lower Triassic) from Karlsruhe
©Staatl. Mus. f. Naturkde Karlsruhe & Naturwiss. Ver. Karlsruhe e.V.; download unter www.zobodat.at carolinea, 67 (2009): 5-12, 3 Abb.; Karlsruhe, 15.12.2009 5 Durlachia striata gen. nov., spec. nov., a new beetle (Coleoptera) from the Upper Buntsand- stein (German Lower Triassic) from Karlsruhe EBERHARD FREY, SAMUEL GIERSCH & WOLFGANG MUNK Abstract Autoren A fossil beetle from the Upper Buntsandstein (Röt- EBERHARD FREY, SAMUEL GIERSCH & WOLFGANG MUNK, Folge, Lower Triassic) in Karlsruhe Durlach-Eisen- Staatliches Museum für Naturkunde, Geowissen- hafengrund is described. The specimen is one of the schaftliche Abteilung, Erbprinzenstraße 13, 76133 oldest known beetle findings in Germany. According to Karlsruhe, Germany. E-mail of corresponding author: its stratigrafic context, the finding layer can be corre- [email protected]. lated with the Voltzia-Sandstone (E-France), which also yielded fossil beetles. The silty matrix, in which the bee- tle occurs, is interpreted as seasonal playa sediment. 1 Introduction The beetle was fragmented during extraction. The lack of diagnostic features of elytra, scutellum and prono- tum does not allow to assign the specimen to a family. The earliest fossil Coleoptera are reported from However, the elytral humeral callus, the set off prono- the Early Permian of southern Siberia and the tum with caudolaterally concave margins combined Ural Mountains (PONOMARENKO 2003). They are with the size of almost 15 mm allows a diagnostic referred to Tschekardocoleidae (Protocoleo- distinction from other coeval Coleoptera at least in Eu- ptera, ROHDENDORF 1944). Throughout the later rope. Therefore, it is justified to refer the specimen from Permian, beetle fossils are frequently found. Durlach-Eisenhafengrund to a new genus and species: These early beetles are referred to Archostema- Durlachia striata.