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Jonathan L Payne

Showing results (31-40 of 41) with videos related to

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Evolution; International Journal of Organic Evolution|September 6, 2012
Late paleozoic fusulinoidean gigantism driven by atmospheric hyperoxiaJonathan L Payne, John R Groves, Adam B Jost, et al.
Geobiology|November 4, 2022
Reduction in animal abundance and oxygen availability during and after the end-Triassic mass extinctionPulkit Singh, Wanyi Lu, Zunli Lu, et al.
Conservation Biology : the Journal of the Society for Conservation Biology|October 20, 2021
A global ecological signal of extinction risk in terrestrial vertebratesMaya J Munstermann, Noel A Heim, Douglas J McCauley, et al.
Current Biology : CB|June 26, 2025
Macroevolutionary coupling of marine biomass and biodiversity across the PhanerozoicPulkit Singh, Jordan Ferré, Bridget Thrasher, et al.
Communications Biology|October 26, 2025
Early gigantic lamniform marks the onset of mega-body size in modern shark evolutionMohamad Bazzi, Mikael Siversson, Sabine Wintner, et al.
Proceedings of the National Academy of Sciences of the United States of America|February 18, 2016
Marine anoxia and delayed Earth system recovery after the end-Permian extinctionKimberly V Lau, Kate Maher, Demir Altiner, et al.
Proceedings. Biological Sciences|June 23, 2017
Hierarchical complexity and the size limits of lifeNoel A Heim, Jonathan L Payne, Seth Finnegan, et al.
The Biological Bulletin|December 22, 2022
Breathless through Time: Oxygen and Animals across Earth's HistoryErik A Sperling, Thomas H Boag, Murray I Duncan, et al.
Proceedings of the National Academy of Sciences of the United States of America|July 6, 2026
Differences in physiological tolerance to global warming caused the Permian-Triassic transition between the Paleozoic and Modern faunasJ Andres Marquez, Justin L Penn, Richard G Stockey, et al.
Proceedings of the National Academy of Sciences of the United States of America|December 25, 2008
Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunityJonathan L Payne, Alison G Boyer, James H Brown, et al.
Pageof 5

Showing results (31-40 of 41) with videos related to

Sort By:
Pageof 5
Evolution; International Journal of Organic Evolution|September 6, 2012
Late paleozoic fusulinoidean gigantism driven by atmospheric hyperoxiaJonathan L Payne, John R Groves, Adam B Jost, et al.
Geobiology|November 4, 2022
Reduction in animal abundance and oxygen availability during and after the end-Triassic mass extinctionPulkit Singh, Wanyi Lu, Zunli Lu, et al.
Conservation Biology : the Journal of the Society for Conservation Biology|October 20, 2021
A global ecological signal of extinction risk in terrestrial vertebratesMaya J Munstermann, Noel A Heim, Douglas J McCauley, et al.
Current Biology : CB|June 26, 2025
Macroevolutionary coupling of marine biomass and biodiversity across the PhanerozoicPulkit Singh, Jordan Ferré, Bridget Thrasher, et al.
Communications Biology|October 26, 2025
Early gigantic lamniform marks the onset of mega-body size in modern shark evolutionMohamad Bazzi, Mikael Siversson, Sabine Wintner, et al.
Proceedings of the National Academy of Sciences of the United States of America|February 18, 2016
Marine anoxia and delayed Earth system recovery after the end-Permian extinctionKimberly V Lau, Kate Maher, Demir Altiner, et al.
Proceedings. Biological Sciences|June 23, 2017
Hierarchical complexity and the size limits of lifeNoel A Heim, Jonathan L Payne, Seth Finnegan, et al.
The Biological Bulletin|December 22, 2022
Breathless through Time: Oxygen and Animals across Earth's HistoryErik A Sperling, Thomas H Boag, Murray I Duncan, et al.
Proceedings of the National Academy of Sciences of the United States of America|July 6, 2026
Differences in physiological tolerance to global warming caused the Permian-Triassic transition between the Paleozoic and Modern faunasJ Andres Marquez, Justin L Penn, Richard G Stockey, et al.
Proceedings of the National Academy of Sciences of the United States of America|December 25, 2008
Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunityJonathan L Payne, Alison G Boyer, James H Brown, et al.
Pageof 5