Zobrazeno 1 - 10
of 152
pro vyhledávání: '"Yannick Donnadieu"'
Autor:
Sebastian Steinig, Ayako Abe-Ouchi, Agatha M. de Boer, Wing-Le Chan, Yannick Donnadieu, David K. Hutchinson, Gregor Knorr, Jean-Baptiste Ladant, Polina Morozova, Igor Niezgodzki, Christopher J. Poulsen, Evgeny M. Volodin, Zhongshi Zhang, Jiang Zhu, David Evans, Gordon N. Inglis, A. Nele Meckler, Daniel J. Lunt
Publikováno v:
Scientific Data, Vol 11, Iss 1, Pp 1-13 (2024)
Abstract Paleoclimate model simulations provide reference data to help interpret the geological record and offer a unique opportunity to evaluate the performance of current models under diverse boundary conditions. Here, we present a dataset of 35 cl
Externí odkaz:
https://doaj.org/article/526a866f6b4f4a469dfd69c47630652c
Autor:
Khushboo Gurung, Katie J. Field, Sarah A. Batterman, Yves Goddéris, Yannick Donnadieu, Philipp Porada, Lyla L. Taylor, Benjamin J. W. Mills
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-9 (2022)
Climatic variables have played a significant role in plant evolution across the Phanerozoic. Here, the authors link climate with a new dynamic vegetation model to identify two windows of opportunity for plant biomass expansion, corresponding with the
Externí odkaz:
https://doaj.org/article/4557a08921fc45a085e05877ab540f93
Autor:
Thomas W. Wong Hearing, Alexandre Pohl, Mark Williams, Yannick Donnadieu, Thomas H. P. Harvey, Christopher R. Scotese, Pierre Sepulchre, Alain Franc, Thijs R. A. Vandenbroucke
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
There is a lot of uncertainty about what Earth’s climate and geography were like in the early Cambrian, when animal life diversified throughout the oceans. Here we show that numeric comparisons of model simulations and climatically influenced rocks
Externí odkaz:
https://doaj.org/article/5236c32b78534f95b003fca752813457
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-9 (2016)
Indirect evidence indicates the surprising occurrence of glacial events during the peak warmth of the Cretaceous world. Here, based on coupled climate-ice sheet model simulations, the authors show that such events were likely thwarted by palaeogeogra
Externí odkaz:
https://doaj.org/article/1455b6db7b2942cebf1cfd9000db9a15
Autor:
Yannick Donnadieu, Emmanuelle Pucéat, Mathieu Moiroud, François Guillocheau, Jean- François Deconinck
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-12 (2016)
In the Earth's history, the timing of oceanic large-scale events of oxygen depletion remains poorly understood. Here, the authors show that palaeogeography was a major preconditioning factor during the Cretaceous, implying that thresholds to shift to
Externí odkaz:
https://doaj.org/article/6c39ec6dd14e4c15bc296fc392d7da38
Publikováno v:
Geological Society, London, Special Publications. 532:157-169
Surface currents constitute an efficient transport agent for (larvae of) marine faunas, while the circulation of water masses in the ocean interior drives nutrient redistribution, ventilates the ocean and contributes to shaping surface biological pro
Publikováno v:
EGU General Assembly 2009
EGU General Assembly 2009, 0000, à renseigner, Unknown Region. pp.7279
ResearcherID
EGU General Assembly 2009, 0000, à renseigner, Unknown Region. pp.7279
ResearcherID
International audience; The Mesozoic, perhaps representing the longest period of warmth during the Phanerozoic Earth history has been repeatedly affected by short-lived cold interludes lasting less than a million of years in length. The evidence for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::82ec57fb73407d61bd88702cdbfe8d33
https://hal.science/hal-04113691
https://hal.science/hal-04113691
Autor:
Igor Niezgodzki, Gregor Knorr, Gerrit Lohmann, Daniel Lunt, Christopher Poulsen, Sebastian Steinig, Jiang Zhu, Agatha de Boer, Wing-Le Chan, Yannick Donnadieu, David Hutchinson, Jean-Baptiste Ladant, Polina Morozova
The early Eocene greenhouse climate driven by high atmospheric CO2 concentrations serves as a testbed for future climate changes dominated by increasing CO2 forcing. Especially, the early Eocene Arctic region is important in light of future CO2-drive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90042be2f149dd7da59801310c4e58b1
https://doi.org/10.5194/egusphere-egu23-8420
https://doi.org/10.5194/egusphere-egu23-8420
Autor:
Jean-Baptiste Ladant, Jeanne Millot-Weil, Yannick Donnadieu, Casimir de Lavergne, Mattias Green
Mixing in the ocean interior is largely fueled by internal tides that bring energy available for the irreversible mixing of the deep ocean. However, the inclusion of mixing schemes to represent the breaking of internal waves is not always included in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7292b66c79bafaa3cf720bde781b50b1
https://doi.org/10.5194/egusphere-egu23-15934
https://doi.org/10.5194/egusphere-egu23-15934
Autor:
Zhen Xu, Jianxin Yu, Hongfu Yin, Andrew Merdith, Jason Hilton, Bethany Allen, Khushboo Gurung, Paul Wignall, Alexander Dunhill, Jun Shen, David Schwartzman, Yves Goddéris, Yannick Donnadieu, Yuxuan Wang, Yinggang Zhang, Simon Poulton, Benjamin Mills
The Permian–Triassic Mass Extinction (PTME), life’s most severe crisis1, has been attributed to intense global warming triggered by CO2 emissions from Large Igneous Province volcanism2–8. It remains unclear, however, why super-greenhouse condit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43ccaa97fe61bbaabbb337569e8f35ac
https://doi.org/10.5194/egusphere-egu23-6194
https://doi.org/10.5194/egusphere-egu23-6194