Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient

Here we report high-latitude stable isotope compositions of Maastrichtian fossil fish and marine reptiles (mainly mosasaurs) from Antarctica (64°S paleolatitude) and compare them with mid-paleolatitude samples from Argentine Patagonia (45°S). Disparities between the δ13C values of bony fish and mari...

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Published in:Paleobiology
Main Authors: Leuzinger, Léa Sylvia, Kocsis, László, Luz, Zoneibe, Vennemann, Torsten Walter, Ulyanov, Alexey, Fernández, Marta Susana
Format: Article in Journal/Newspaper
Language:English
Published: Paleontological Society
Subjects:
Online Access:http://hdl.handle.net/11336/217816
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author Leuzinger, Léa Sylvia
Kocsis, László
Luz, Zoneibe
Vennemann, Torsten Walter
Ulyanov, Alexey
Fernández, Marta Susana
author_facet Leuzinger, Léa Sylvia
Kocsis, László
Luz, Zoneibe
Vennemann, Torsten Walter
Ulyanov, Alexey
Fernández, Marta Susana
author_sort Leuzinger, Léa Sylvia
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 2
container_start_page 353
container_title Paleobiology
container_volume 49
description Here we report high-latitude stable isotope compositions of Maastrichtian fossil fish and marine reptiles (mainly mosasaurs) from Antarctica (64°S paleolatitude) and compare them with mid-paleolatitude samples from Argentine Patagonia (45°S). Disparities between the δ13C values of bony fish and marine reptiles correspond to differences in the foraging ground (distance from the shore and depth), while dramatically higher δ13C values (by 18‰) in shark enameloid cannot be explained through ecology and are here imputed to biomineralization. Comparison with extant vertebrates suggests that the diet alone can explain the offset observed between bony fish and mosasaurs; however, breath holding due to a diving behavior in mosasaurs may have had some impact on their δ13C values, as previously suggested. The δ18OPO4 values of the remains confirm a relatively stable, elevated body temperature for marine reptiles, meaning that they were thermoregulators. We calculated a water temperature of ~8°C for Antarctica from the fish δ18OPO4 values, warmer than present-day temperatures and consistent with the absence of polar ice sheets during the latest Maastrichtian. Our fish data greatly extend the latitudinal range of Late Cretaceous fish δ18OPO4 values and result in a thermal gradient of 0.4°C/1° of latitude when combined with literature data. Fil: Leuzinger, Léa Sylvia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Kocsis, László. Universite de Lausanne; Suiza Fil: Luz, Zoneibe. Universite de Lausanne; Suiza Fil: Vennemann, Torsten Walter. Universite de Lausanne; Suiza Fil: Ulyanov, Alexey. Universite de Lausanne; Suiza Fil: Fernández, Marta Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ...
format Article in Journal/Newspaper
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Antarctica
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/217816 2025-01-16T19:24:15+00:00 Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient Leuzinger, Léa Sylvia Kocsis, László Luz, Zoneibe Vennemann, Torsten Walter Ulyanov, Alexey Fernández, Marta Susana application/pdf http://hdl.handle.net/11336/217816 eng eng Paleontological Society info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/paleobiology/article/latest-maastrichtian-middle-and-highlatitude-mosasaurs-and-fish-isotopic-composition-carbon-source-thermoregulation-strategy-and-thermal-latitudinal-gradient/71D43AE7F3DB83143643E41B63BB7637 info:eu-repo/semantics/altIdentifier/doi/10.1017/pab.2022.38 http://hdl.handle.net/11336/217816 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ Mosasaurs fish High latitude Maastrichtian Cretaceous 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/10.1017/pab.2022.38 2024-10-04T09:34:14Z Here we report high-latitude stable isotope compositions of Maastrichtian fossil fish and marine reptiles (mainly mosasaurs) from Antarctica (64°S paleolatitude) and compare them with mid-paleolatitude samples from Argentine Patagonia (45°S). Disparities between the δ13C values of bony fish and marine reptiles correspond to differences in the foraging ground (distance from the shore and depth), while dramatically higher δ13C values (by 18‰) in shark enameloid cannot be explained through ecology and are here imputed to biomineralization. Comparison with extant vertebrates suggests that the diet alone can explain the offset observed between bony fish and mosasaurs; however, breath holding due to a diving behavior in mosasaurs may have had some impact on their δ13C values, as previously suggested. The δ18OPO4 values of the remains confirm a relatively stable, elevated body temperature for marine reptiles, meaning that they were thermoregulators. We calculated a water temperature of ~8°C for Antarctica from the fish δ18OPO4 values, warmer than present-day temperatures and consistent with the absence of polar ice sheets during the latest Maastrichtian. Our fish data greatly extend the latitudinal range of Late Cretaceous fish δ18OPO4 values and result in a thermal gradient of 0.4°C/1° of latitude when combined with literature data. Fil: Leuzinger, Léa Sylvia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Kocsis, László. Universite de Lausanne; Suiza Fil: Luz, Zoneibe. Universite de Lausanne; Suiza Fil: Vennemann, Torsten Walter. Universite de Lausanne; Suiza Fil: Ulyanov, Alexey. Universite de Lausanne; Suiza Fil: Fernández, Marta Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ... Article in Journal/Newspaper Antarc* Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Argentine Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Patagonia Paleobiology 49 2 353 373
spellingShingle Mosasaurs fish
High latitude
Maastrichtian
Cretaceous
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Leuzinger, Léa Sylvia
Kocsis, László
Luz, Zoneibe
Vennemann, Torsten Walter
Ulyanov, Alexey
Fernández, Marta Susana
Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
title Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
title_full Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
title_fullStr Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
title_full_unstemmed Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
title_short Latest Maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
title_sort latest maastrichtian middle- and high-latitude mosasaurs and fish isotopic composition: carbon source, thermoregulation strategy, and thermal latitudinal gradient
topic Mosasaurs fish
High latitude
Maastrichtian
Cretaceous
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Mosasaurs fish
High latitude
Maastrichtian
Cretaceous
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/217816