Zobrazeno 1 - 10
of 95
pro vyhledávání: '"Seth Finnegan"'
Autor:
Sara S. Kahanamoku-Meyer, Maya Samuels-Fair, Sarah M. Kamel, Da’shaun Stewart, Bryan Wu, Leah X. Kahn, Max Titcomb, Yingyan Alyssa Mei, R. Cheyenne Bridge, Yuerong Sophie Li, Carolina Sinco, Julissa Moreno, Josef T. Epino, Gerson Gonzalez-Marin, Chloe Latt, Heather Fergus, Ivo A. P. Duijnstee, Seth Finnegan
Publikováno v:
Scientific Data, Vol 11, Iss 1, Pp 1-14 (2024)
Abstract The Santa Barbara Basin is an extraordinary archive of environmental and ecological change, where varved sediments preserve microfossils that provide an annual to decadal record of the dynamics of surrounding ecosystems. Of the microfossils
Externí odkaz:
https://doaj.org/article/05f83f2738f3483f808dd8d87e82527d
Autor:
Joshua B. Zimmt, Steven M. Holland, Mariko Cappello, David S. Jones, Jisuo Jin, Jon M. Husson, Blair Schoene, Charles Mitchell, Michael Melchin, Seth Finnegan, André Desrochers
Publikováno v:
Estonian Journal of Earth Sciences, Vol 72, Iss 1, Pp 170-0 (2023)
Anticosti Island, Canada, has long been recognized as an exceptional OrdovicianâSilurian boundary succession with the potential to serve as one of the best records of climatic, oceanographic, and biological events associated with the Late Ordovician
Externí odkaz:
https://doaj.org/article/524444e7b8984ca9a740cbf48401e358
Autor:
Ming-Xing Ling, Ren-Bin Zhan, Guang-Xu Wang, Yi Wang, Yuri Amelin, Peng Tang, Jian-Bo Liu, Jisuo Jin, Bing Huang, Rong-Chang Wu, Shuo Xue, Bin Fu, Vickie C. Bennett, Xin Wei, Xiao-Cong Luan, Seth Finnegan, David A.T. Harper, Jia-Yu Rong
Publikováno v:
Solid Earth Sciences, Vol 4, Iss 4, Pp 190-198 (2019)
The end Ordovician mass extinction (EOME) was the second most severe biotic crisis in Phanerozoic, and has been widely linked to a major glaciation. However, robust geochronology of this interval is still lacking. Here we present four successive high
Externí odkaz:
https://doaj.org/article/edd418835a2d41ff92dfabd2b3687d05
Autor:
Craig R. McClain, Thomas J. Webb, Clifton C. Nunnally, S. River Dixon, Seth Finnegan, James A. Nelson
Publikováno v:
Frontiers in Marine Science, Vol 7 (2020)
The great anthropogenic alterations occurring to carbon availability in the oceans necessitate an understanding of the energy requirements of species and how changes in energy availability may impact biodiversity. The deep-sea floor is characterized
Externí odkaz:
https://doaj.org/article/5b59a5c31d014d43833abd045557ebdf
Autor:
Ming-Xing Ling, Ren-Bin Zhan, Guang-Xu Wang, Yi Wang, Yuri Amelin, Peng Tang, Jian-Bo Liu, Jisuo Jin, Bing Huang, Rong-Chang Wu, Shuo Xue, Bin Fu, Vickie C. Bennett, Xin Wei, Xiao-Cong Luan, Seth Finnegan, David A.T. Harper, Jia-Yu Rong
Publikováno v:
Solid Earth Sciences, Vol 5, Iss 1, Pp 82- (2020)
Externí odkaz:
https://doaj.org/article/c57b216c5a3e425b98ff38c59034965b
Publikováno v:
Trends in Ecology & Evolution.
Autor:
Emily A. Orzechowski, Seth Finnegan
Publikováno v:
Paleobiology. 47:418-431
As the most recent time in Earth history when global temperatures were warmer than at present, the peak of the last interglacial (Marine Isotope Substage [MIS] 5e; ~120,000 years ago) can serve as a pre-anthropogenic baseline for a warmer near-future
Publikováno v:
Palaeontology. 64:1-20
Autor:
Alexander Farnsworth, Daniel J. Lunt, Erin E. Saupe, Alan T. Kennedy-Asser, Paul J. Valdes, Yannick Donnadieu, Jean-Baptiste Ladant, Alexandre Pohl, Seth Finnegan, Huijie Qiao
Publikováno v:
Nature Geoscience
Nature Geoscience, Nature Publishing Group, 2020, 13 (1), pp.65-70. ⟨10.1038/s41561-019-0504-6⟩
Nature Geoscience, 2020, 13 (1), pp.65-70. ⟨10.1038/s41561-019-0504-6⟩
Saupe, E, Qiao, H, Donnadieu, Y, Farnsworth, A J, Kennedy-Asser, A T, Ladant, J-B, Lunt, D J, Pohl, A, Valdes, P J & Finnegan, S 2020, ' Extinction intensity during Ordovician and Cenozoic glaciations explained by cooling and palaeogeography ', Nature Geoscience . https://doi.org/10.1038/s41561-019-0504-6
Nature Geoscience, Nature Publishing Group, 2020, 13 (1), pp.65-70. ⟨10.1038/s41561-019-0504-6⟩
Nature Geoscience, 2020, 13 (1), pp.65-70. ⟨10.1038/s41561-019-0504-6⟩
Saupe, E, Qiao, H, Donnadieu, Y, Farnsworth, A J, Kennedy-Asser, A T, Ladant, J-B, Lunt, D J, Pohl, A, Valdes, P J & Finnegan, S 2020, ' Extinction intensity during Ordovician and Cenozoic glaciations explained by cooling and palaeogeography ', Nature Geoscience . https://doi.org/10.1038/s41561-019-0504-6
A striking feature of the marine fossil record is the variable intensity of extinction during superficially similar climate transitions. Here we combine climate models and species trait simulations to explore the degree to which differing palaeogeogr
Autor:
Alexandre Pohl, Maya Elrick, Menghan Li, Ruliang He, Richard G. Stockey, André Desrochers, Yanan Shen, Zunli Lu, Andy Ridgwell, Seth Finnegan, Wanyi Lu
Publikováno v:
Nature Geoscience
Nature Geoscience, Nature Publishing Group, 2021, ⟨10.1038/s41561-021-00843-9⟩
Nature Geoscience, Nature Publishing Group, 2021, ⟨10.1038/s41561-021-00843-9⟩
Geochemical redox proxies indicate that seafloor anoxia occurred during the latest Ordovician glacial maximum, coincident with the second pulse of the Late Ordovician mass extinction. However, expanded anoxia in a glacial climate strikingly contrasts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0710f3ce6cf2577a07231267a0ae63fe
https://hal.archives-ouvertes.fr/hal-03412068
https://hal.archives-ouvertes.fr/hal-03412068