Zobrazeno 1 - 10
of 111
pro vyhledávání: '"Jeremy K. Caves"'
Autor:
Rugenstein, Jeremy K. Caves, Ibarra, Daniel E., Zhang, Shuang, Planavsky, Noah J., von Blanckenburg, Friedhelm
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America, 2021 Jul . 118(30), 1-2.
Externí odkaz:
https://www.jstor.org/stable/27052574
Autor:
Tyler Kukla, Daniel Enrique Ibarra, Jeremy K. Caves Rugenstein, Jared T. Gooley, Casey E. Mullins, Samuel Kramer, Danielle Y. Moragne, C. Page Chamberlain
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The John Day region of central Oregon, United States contains ∼50 million years of near-continuous, fossiliferous sedimentation, representing one of the world’s richest archives of Cenozoic terrestrial ecosystems and climate. Stable isotope proxy
Externí odkaz:
https://doaj.org/article/353538bd81e14af5839089f5e20f0594
Autor:
Jeremy K. Caves Rugenstein, Katharina Methner, Tyler Kukla, Andreas Mulch, Tina Lüdecke, Jens Fiebig, Anne Meltzer, Karl W. Wegmann, Peter Zeitler, C. Page Chamberlain
Publikováno v:
American Journal of Science. 322:28-54
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Zaijun Li, Jeremy K. Caves Rugenstein, Ilhomjon Oimuhammadzoda, Jay Quade, Peter G. DeCelles, Barbara Carrapa, Xu Zhang, Xin Wang, Fahu Chen, Mi Wang, Fei Wang, Mustafo Gadoev, Yuchen Sun, James B. Chapman, Gerrit Lohmann, David L. Dettman, Mark T. Clementz, Jie Chen
Publikováno v:
Geology. 48:728-732
Interactions between midlatitude westerlies and the Pamir–Tian Shan mountains significantly impact hydroclimate patterns in Central Asia today, and they played an important role in driving Asian aridification during the Cenozoic. We show that disti
Autor:
Jeremy K. Caves Rugenstein, Page Chamberlain, Caroline A.E. Strömberg, Tyler Kukla, Daniel E. Ibarra, Matthew J. Winnick
The shift from denser forests to open, grass-dominated vegetation in west-central North America between 26 and 15 million years ago is a major ecological transition with no clear driving force. Thi...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5c35697f89e476a367374ac79e5d4d0
https://doi.org/10.1002/essoar.10507866.1
https://doi.org/10.1002/essoar.10507866.1
Autor:
Noah J. Planavsky, Shuang Zhang, Friedhelm von Blanckenburg, Daniel E. Ibarra, Jeremy K. Caves Rugenstein
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America (PNAS)
Park et al. (1) use a global biogeochemical model (GEOCLIM) to suggest that weathering associated with emergence of mafic islands in Southeast Asia resulted in a ∼350-ppm decrease in atmospheric CO2 during the last 15 Ma. However, only matching p C
Autor:
Victor Brovkin, Philipp de Vrese, Tobias Stacke, Jason C. Goodman, Jeremy K. Caves Rugenstein
Publikováno v:
Communications Earth & Environment
Simple and complex climate models suggest a hard snowball – a completely ice-covered planet – is one of the steady-states of Earth’s climate. However, a seemingly insurmountable challenge to the hard-snowball hypothesis lies in the difficulty i
Autor:
H. J. Hassenruck-Gudipati, Albert Galy, Aaron Bufe, Jeremy K. Caves Rugenstein, Jui-Ming Chang, Robert Emberson, Niels Hovius
Publikováno v:
Nature Geoscience
Nature Geoscience, Nature Publishing Group, 2021, 14 (4), pp.211-216. ⟨10.1038/s41561-021-00714-3⟩
Nature Geoscience, Nature Publishing Group, 2021, 14 (4), pp.211-216. ⟨10.1038/s41561-021-00714-3⟩
Global climate is thought to be modulated by the supply of minerals to Earth’s surface. Whereas silicate weathering removes carbon dioxide (CO2) from the atmosphere, weathering of accessory carbonate and sulfide minerals is a geologically relevant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac8142f35c16c473d58d8707c185f2e8
https://hal.archives-ouvertes.fr/hal-03401635
https://hal.archives-ouvertes.fr/hal-03401635
Autor:
Jeremy K. Caves Rugenstein
Publikováno v:
Nature Geoscience. 13:5-7
Differential cycling of carbonate and organic carbon in the mantle may link the Great Oxidation Event and the subsequent increase in carbon isotope values, according to a model that links the Earth’s surface and interior.