Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica
The Eocene La Meseta Formation on Seymour Island, Antarctic Peninsula, is known for its remarkable wealth of fossil remains of chondrichthyans and teleosts. Chondrichthyans seemingly were dominant elements in the Antarctic Paleogene fish fauna, but decreased in abundance from middle to late Eocene,...
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ftconicet:oai:ri.conicet.gov.ar:11336/54351 2023-10-09T21:46:28+02:00 Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica Kriwet, Jürgen Engelbrecht, Andrea Mörs, Thomas Reguero, Marcelo Alfredo Pfaff, Cathrin application/pdf http://hdl.handle.net/11336/54351 eng eng Society of Vertebrate Paleontology info:eu-repo/semantics/altIdentifier/doi/10.1080/02724634.2016.1160911 info:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/abs/10.1080/02724634.2016.1160911 info:eu-repo/semantics/altIdentifier/url/https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5346486/ http://hdl.handle.net/11336/54351 Kriwet, Jürgen; Engelbrecht, Andrea; Mörs, Thomas; Reguero, Marcelo Alfredo; Pfaff, Cathrin; Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica; Society of Vertebrate Paleontology; Journal of Vertebrate Paleontology; 36; 4; 7-2016; 1-19; e1160911 0272-4634 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Chondrichthyans Paleogene Submeseta Fm Antarctica https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1080/02724634.2016.1160911 2023-09-24T19:54:31Z The Eocene La Meseta Formation on Seymour Island, Antarctic Peninsula, is known for its remarkable wealth of fossil remains of chondrichthyans and teleosts. Chondrichthyans seemingly were dominant elements in the Antarctic Paleogene fish fauna, but decreased in abundance from middle to late Eocene, during which time remains of bony fishes increase. This decline of chondrichthyans at the end of the Eocene generally is related to sudden cooling of seawater, reduction in shelf area, and increasing shelf depth due to the onset of the Antarctic thermal isolation. The last chondrichthyan records known so far include a chimeroid tooth plate from TELM 6 (Lutetian) and a single pristiophorid rostral spine from TELM 7 (Priabonian). Here, we present new chondrichthyan records of Squalus, Squatina, Pristiophorus, Striatolamia, Palaeohypotodus, Carcharocles, and Ischyodus from the upper parts of TELM 7 (Priabonian), including the first record of Carcharocles sokolovi from Antarctica. This assemblage suggests that chondrichthyans persisted much longer in Antarctic waters despite rather cool sea surface temperatures of approximately 5°C. The final disappearance of chondrichthyans at the Eocene–Oligocene boundary concurs with abrupt ice sheet formation in Antarctica. Diversity patterns of chondrichthyans throughout the La Meseta Formation appear to be related to climatic conditions rather than plate tectonics. Fil: Kriwet, Jürgen. Universidad de Viena; Austria Fil: Engelbrecht, Andrea. Universidad de Viena; Austria Fil: Mörs, Thomas. Swedish Museum of Natural History; Suecia Fil: Reguero, Marcelo Alfredo. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Pfaff, Cathrin. Universidad de Viena; Austria Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Dirección Nacional del Antártico Ice Sheet Instituto Antártico Argentino Seymour Island CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic The Antarctic Antarctic Peninsula Argentino Argentina Seymour ENVELOPE(-56.767,-56.767,-64.283,-64.283) Seymour Island ENVELOPE(-56.750,-56.750,-64.283,-64.283) Suecia ENVELOPE(-62.617,-62.617,-66.733,-66.733) Pfaff ENVELOPE(-67.733,-67.733,-66.883,-66.883) Journal of Vertebrate Paleontology 36 4 e1160911 |
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CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
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language |
English |
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Chondrichthyans Paleogene Submeseta Fm Antarctica https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
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Chondrichthyans Paleogene Submeseta Fm Antarctica https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Kriwet, Jürgen Engelbrecht, Andrea Mörs, Thomas Reguero, Marcelo Alfredo Pfaff, Cathrin Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica |
topic_facet |
Chondrichthyans Paleogene Submeseta Fm Antarctica https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
The Eocene La Meseta Formation on Seymour Island, Antarctic Peninsula, is known for its remarkable wealth of fossil remains of chondrichthyans and teleosts. Chondrichthyans seemingly were dominant elements in the Antarctic Paleogene fish fauna, but decreased in abundance from middle to late Eocene, during which time remains of bony fishes increase. This decline of chondrichthyans at the end of the Eocene generally is related to sudden cooling of seawater, reduction in shelf area, and increasing shelf depth due to the onset of the Antarctic thermal isolation. The last chondrichthyan records known so far include a chimeroid tooth plate from TELM 6 (Lutetian) and a single pristiophorid rostral spine from TELM 7 (Priabonian). Here, we present new chondrichthyan records of Squalus, Squatina, Pristiophorus, Striatolamia, Palaeohypotodus, Carcharocles, and Ischyodus from the upper parts of TELM 7 (Priabonian), including the first record of Carcharocles sokolovi from Antarctica. This assemblage suggests that chondrichthyans persisted much longer in Antarctic waters despite rather cool sea surface temperatures of approximately 5°C. The final disappearance of chondrichthyans at the Eocene–Oligocene boundary concurs with abrupt ice sheet formation in Antarctica. Diversity patterns of chondrichthyans throughout the La Meseta Formation appear to be related to climatic conditions rather than plate tectonics. Fil: Kriwet, Jürgen. Universidad de Viena; Austria Fil: Engelbrecht, Andrea. Universidad de Viena; Austria Fil: Mörs, Thomas. Swedish Museum of Natural History; Suecia Fil: Reguero, Marcelo Alfredo. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Pfaff, Cathrin. Universidad de Viena; Austria |
format |
Article in Journal/Newspaper |
author |
Kriwet, Jürgen Engelbrecht, Andrea Mörs, Thomas Reguero, Marcelo Alfredo Pfaff, Cathrin |
author_facet |
Kriwet, Jürgen Engelbrecht, Andrea Mörs, Thomas Reguero, Marcelo Alfredo Pfaff, Cathrin |
author_sort |
Kriwet, Jürgen |
title |
Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica |
title_short |
Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica |
title_full |
Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica |
title_fullStr |
Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica |
title_full_unstemmed |
Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica |
title_sort |
ultimate eocene (priabonian) chondrichthyans (holocephali, elasmobranchii) of antarctica |
publisher |
Society of Vertebrate Paleontology |
url |
http://hdl.handle.net/11336/54351 |
long_lat |
ENVELOPE(-56.767,-56.767,-64.283,-64.283) ENVELOPE(-56.750,-56.750,-64.283,-64.283) ENVELOPE(-62.617,-62.617,-66.733,-66.733) ENVELOPE(-67.733,-67.733,-66.883,-66.883) |
geographic |
Antarctic The Antarctic Antarctic Peninsula Argentino Argentina Seymour Seymour Island Suecia Pfaff |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Argentino Argentina Seymour Seymour Island Suecia Pfaff |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Dirección Nacional del Antártico Ice Sheet Instituto Antártico Argentino Seymour Island |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Dirección Nacional del Antártico Ice Sheet Instituto Antártico Argentino Seymour Island |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1080/02724634.2016.1160911 info:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/abs/10.1080/02724634.2016.1160911 info:eu-repo/semantics/altIdentifier/url/https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5346486/ http://hdl.handle.net/11336/54351 Kriwet, Jürgen; Engelbrecht, Andrea; Mörs, Thomas; Reguero, Marcelo Alfredo; Pfaff, Cathrin; Ultimate Eocene (Priabonian) chondrichthyans (Holocephali, Elasmobranchii) of Antarctica; Society of Vertebrate Paleontology; Journal of Vertebrate Paleontology; 36; 4; 7-2016; 1-19; e1160911 0272-4634 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1080/02724634.2016.1160911 |
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Journal of Vertebrate Paleontology |
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36 |
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e1160911 |
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