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Hesperornithiformes (Aves: Ornithurae) from the Upper Cretaceous Pierre Shale,Southern Manitoba,Canada
Institution:1. Palaeobiology Research Group, Biological Sciences Department, University of Cape Town, Private Bag X3, Rhodes Gift, 7701 South Africa;2. CNRS (UMR 8538), Laboratoire de Géologie de l’École Normale Supérieure, PSL Research University, 24, rue Lhomond, 75231 Paris cedex 05, France;3. Museo de Ciencias Naturales de Álava/Arabako Natur Zientzien Museoa, Siervas de Jesús 24, 01001 Vitoria-Gasteiz, Spain;4. Universidad del País Vasco/Euskal Herriko Unibertsitatea, Facultad de Ciencia y Tecnología, Departamento de Estratigrafía y Paleontología, Apartado 644, 48080 Bilbao, Spain;1. Division of Paleontology Institute of Geosciences, University of Bonn, Bonn, Germany;2. Red Paleontol?gica U.chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Universidad de Chile, Santiago, Chile;3. Department of Biological Sciences, University of Alberta, Edmonton, Alberta, T6G 2E9, Canada;4. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, T6G 2E9, Canada;1. PALEOLAB (Laboratório de Paleontologia), Departamento de Geologia, Centro de Tecnologia e Geociências, Universidade Federal de Pernambuco, UFPE, Av. Acadêmico Hélio Ramos s/n, CEP 50740-530, Recife, PE, Brazil;2. Laboratório de Paleontologia e Paleoecologia da Sociedade de História Natural, Travessa Florêncio Augusto Chagas nº 8B, 2560-230 Torres Vedras, Portugal;1. Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, 117737 Moscow, Russia;2. Zoological Institute of the Russian Academy of Sciences, Universitetskaya Emb. 1, 199034 Saint Petersburg, Russia;3. Department of Sedimentary Geology, Geological Faculty, Saint Petersburg State University, 16 liniya VO 29, 199178 Saint Petersburg, Russia;4. Department of Historical Geology and Paleontology, Geological Faculty, Saratov State University, 83 Astrakhanskaya Str., 410012 Saratov, Russia;5. Institute of Geology and Petroleum Technology, Kazan Federal University, Kremlevskaya Str. 4/5, 420008 Kazan, Russia;1. Centro de Investigaciones Geológicas (CONICET - UNLP), Diagonal 113 274, B1904DPK, La Plata, Buenos Aires, Argentina;2. Laboratorio de Anatomía Comparada y Evolución de los Vertebrados del Museo Argentino de Ciencias Naturales “Bernardino Rivadavia” (CONICET), Av. Ángel Gallardo 470, C1405DJR, Ciudad Autónoma de Buenos Aires, Argentina;3. Fundación de Historia Natural “Félix de Azara”, Departamento de Ciencias Naturales y Antropología, CEBBAD - Universidad Maimónides, Hidalgo C1405BDB, Buenos Aires, Argentina;4. División Paleobotánica. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia” (CONICET), Av. Ángel Gallardo 470, C1405DJR, Ciudad Autónoma de Buenos Aires, Argentina;5. Área de Paleontología, Departamento de Geología, Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria, C1428EGA, Buenos Aires, Argentina;6. Y-TEC (YPF S.A. - CONICET), Av. Del Petróleo s/n entre 129 y 143, Berisso, Buenos Aires, Argentina;7. Instituto de Geología y Paleontología (CONICET - CENPAT), Boulevard Brown 2915, U9120ACD Puerto Madryn, Argentina;8. Museo Paleontológico Egidio Feruglio (CONICET), Av. Fontana 140, 9100, Trelew, Argentina;9. Center for the Collections, Natural Museum of Nature & Science, Tsukuba 305-0005, Japan;10. Department of Geology & Paleontology, Natural Museum of Naure & Science, Tsukuba 305-0005, Japan
Abstract:A historical collection of hesperornithiform fossils from the Gammon Ferruginous, Pembina, and Millwood members of the Pierre Shale (Campanian, Upper Cretaceous) in southern Manitoba, Canada, was examined to revise their taxonomy. Only two species of Hesperornis have been recognized in previous studies on the Pierre Shale in Manitoba, but our study recognizes six species of two genera, including H. lumgairi sp. nov. H. regalis is the most common species but absent in the uppermost unit within the studied sequence. The result of this study supports the paleobiogeographic subdivision of the Campanian vertebrate fauna within the Western Interior Seaway, but not the faunal boundary that distinguishes the avian fauna of Manitoba from that of South Dakota and Kansas.
Keywords:Campanian  Paleobiogeography  Western Interior Seaway
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