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dc.contributor.author
Liu, Jun
dc.contributor.author
Abdala, Nestor Fernando
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dc.contributor.author
Angielczyk, Kenneth D.
dc.contributor.author
Sidor, Christian A.
dc.date.available
2022-07-16T02:33:56Z
dc.date.issued
2022-01
dc.identifier.citation
Liu, Jun; Abdala, Nestor Fernando; Angielczyk, Kenneth D.; Sidor, Christian A.; Tetrapod turnover during the Permo-Triassic transition explained by temperature change; Elsevier Science; Earth-science Reviews; 224; 103886; 1-2022; 1-10
dc.identifier.issn
0012-8252
dc.identifier.uri
http://hdl.handle.net/11336/162267
dc.description.abstract
Global temperatures significantly changed from the late Permian to the Early Triassic: the Earth transformed from a cool world to a hothouse climate. This transition undoubtedly had a strong impact on tetrapod physiology and distribution. During the global cooling, tetrapods generally increased their size; and the currently recognized late Permian tetrapod extinction, exemplified by the record preserved in the South African Karoo Basin, occurred in the late stage of cooling. Rapid warming in the Early Triassic is predicted to have resulted in extinctions and/or local extirpation of low latitude tetrapods, but the very limited fossil record from this region makes testing this hypothesis difficult. Warming is predicted to have had less negative impacts on the tetrapod diversity of mid-latitudes, and promoted the success of tetrapods in the high latitudes. Based on the known fossil record, a tetrapod gap could have existed in central Pangea between ~30°N and ~ 40°S, and lasting from the Induan to the early Spathian. However, the exact boundaries of this gap likely varied over time, and it could have encompassed a larger area during the hottest phases (Griesbachian and near the Smithian–Spathain boundary).
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier Science
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dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
CLIMATE CHANGE
dc.subject
DICYNODONTIA
dc.subject
LYSTROSAURUS
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P/TR
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PERMO-TRIASSIC EXTINCTION
dc.subject
TETRAPODA
dc.subject.classification
Paleontología
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dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente
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dc.subject.classification
CIENCIAS NATURALES Y EXACTAS
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dc.title
Tetrapod turnover during the Permo-Triassic transition explained by temperature change
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2022-07-04T19:58:42Z
dc.journal.volume
224
dc.journal.number
103886
dc.journal.pagination
1-10
dc.journal.pais
Países Bajos
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dc.journal.ciudad
Amsterdam
dc.description.fil
Fil: Liu, Jun. Chinese Academy of Sciences; República de China
dc.description.fil
Fil: Abdala, Nestor Fernando. University of the Witwatersrand; Sudáfrica. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - Tucumán. Unidad Ejecutora Lillo; Argentina
dc.description.fil
Fil: Angielczyk, Kenneth D.. University of the Witwatersrand; Sudáfrica. Field Museum of Natural History; Estados Unidos
dc.description.fil
Fil: Sidor, Christian A.. University of Washington; Estados Unidos
dc.journal.title
Earth-science Reviews
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dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.earscirev.2021.103886
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0012825221003871
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