首页> 中文期刊> 《极地科学进展:英文版》 >Late Cretaceous non-avian dinosaurs from the James Ross Basin,Antarctica:description of new material,updated synthesis,biostratigraphy,and paleobiogeography

Late Cretaceous non-avian dinosaurs from the James Ross Basin,Antarctica:description of new material,updated synthesis,biostratigraphy,and paleobiogeography

         

摘要

cqvip:Although the fossil record of non-avian dinosaurs from the Cretaceous of Antarctica is the poorest of any continent,fossils representing at least five major taxonomic groups(Ankylosauria,early-diverging Ornithopoda,Hadrosauridae,Titanosauria,and Theropoda)have been recovered.All come from Upper Cretaceous(Coniacian–Maastrichtian)marine and nearshore deposits belonging to the Gustav and Marambio groups of the James Ross Basin at the northern tip of the Antarctic Peninsula.The majority of these finds have come from the Campanian–Maastrichtian Snow Hill Island and López de Bertodano formations of James Ross and Vega islands.Given the rarity of Antarctic Cretaceous non-avian dinosaurs,discoveries of any fossils of these archosaurs,no matter how meager,are of significance.Here we describe fragmentary new ornithischian(ankylosaur and ornithopod)material from the upper Campanian–lower Maastrichtian Cape Lamb Member of the Snow Hill Island Formation and the Maastrichtian Sandwich Bluff Member of the López de Bertodano Formation.One of these specimens is considered to probably pertain to the holotypic individual of the early-diverging ornithopod Morrosaurus antarcticus.We also provide an up-to-date synthesis of the Late Cretaceous non-avian dinosaur record of the James Ross Basin and analyze the biostratigraphic occurrences of the various finds,demonstrating that most(including all named taxa and all reasonably complete skeletons discovered to date)occur within a relatively condensed temporal interval of the late Campanian to early Maastrichtian.Most or all James Ross Basin dinosaurs share close affinities with penecontemporaneous taxa from Patagonia,indicating that at least some continental vertebrates could disperse between southern South America and Antarctica during the final stages of the Mesozoic.

著录项

  • 来源
    《极地科学进展:英文版》 |2019年第3期|P.228-250|共23页
  • 作者单位

    Section of Vertebrate Paleontology Carnegie Museum of Natural History 4400 Forbes Avenue Pittsburgh Pennsylvania 15213 USA;

    Department of Biology Eastern Washington University Science Building 258 Cheney Washington 99004 USA;

    College of Science and Engineering James Cook University Townsville Queensland 4811 Australia;

    Royal British Columbia Museum 675 Belleville Street Victoria British Columbia V8W 9W2 Canada;

    Department of Earth and Atmospheric Sciences Indiana University Geological Sciences Building 1001 East 10th Street Bloomington Indiana 47401 USA;

    School of Biological Sciences The University of Queensland Brisbane Queensland 4072 Australia;

    Department of Geological Sciences The University of Texas at Austin 2275 Speedway Stop C9000 Austin Texas 78712 USA;

    School of Natural Sciences Black Hills State University 1200 University Street Spearfish South Dakota 57799 USA;

    Department of Biological Sciences University of Pittsburgh 4249 Fifth Avenue Pittsburgh Pennsylvania 15260 USA;

    Department of Biomedical Sciences Ohio University Heritage College of Osteopathic Medicine 119 Life Sciences Building Athens Ohio 45701 USA;

    Ohio Center for Ecology and Evolutionary Studies Ohio University Irvine Hall Athens Ohio 45701 USA;

  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 历史地质学、地层学;
  • 关键词

    Dinosauria; Antarctica; Cretaceous; James Ross Basin; biostratigraphy; paleobiogeography;

    机译:恐龙南极洲;白垩纪;詹姆斯·罗斯盆地;生物地层学古生物学;
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