Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Maxime Tremblin"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-9 (2024)
Abstract The Indo-Pacific warm pool is the warmest and most dynamic ocean–atmosphere-climate system on Earth and was subject to significant climate changes during the Pleistocene glacial-interglacial transitions. This has been shown to significantl
Externí odkaz:
https://doaj.org/article/178e95111c9446ab94b2ef455b7b7f76
The Indo-Pacific Warm Pool (IPWP) is the warmest and most dynamic ocean-atmosphere-climate system on Earth and has undergone significant climatic changes during the Pleistocene glacial periods (De Deckker et al., 2012; Lea et al., 2000; Russell et al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76b89b90455a8b266b391d5d95011c06
https://doi.org/10.5194/egusphere-egu23-2105
https://doi.org/10.5194/egusphere-egu23-2105
Autor:
Sabí Peris Cabré, Luis Valero, Jorge E. Spangenberg, Andreu Vinyoles, Jean Verité, Thierry Adatte, Maxime Tremblin, Stephen Watkins, Nikhil Sharma, Miguel Garcés, Cai Puigdefàbregas, Sébastien Castelltort
Publikováno v:
Climate of the Past
Climate of the Past, 2023, 19 (3), pp.533-554. ⟨10.5194/cp-19-533-2023⟩
eISSN
Climate of the Past, 2023, 19 (3), pp.533-554. ⟨10.5194/cp-19-533-2023⟩
eISSN
The early Cenozoic marine sedimentary record is punctuated by several brief episodes ( kyr) of abrupt global warming, called hyperthermals, that have disturbed ocean life and water physicochemistry. Moreover, recent studies of fluvial–deltaic syste
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::153fb3f9f4fd7a44ddd6f24da98ffa33
https://doi.org/10.5194/egusphere-2022-891
https://doi.org/10.5194/egusphere-2022-891
Autor:
Sabí Peris Cabré, Luis Valero, Jorge E. Spangenberg, Andreu Vinyoles, Jean Verité, Thierry Adatte, Maxime Tremblin, Stephen Watkins, Nikhil Sharma, Miguel Garcés, Cai Puigdefàbregas, Sébastien Castelltort
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d65d583872eb163def396f4b5a7dad94
https://doi.org/10.5194/egusphere-2022-891-supplement
https://doi.org/10.5194/egusphere-2022-891-supplement
Autor:
Maxime Tremblin, Hassan Khozyem, Thierry Adatte, Jorge E. Spangenberg, Charlotte Fillon, Arnaud Grauls, Teodoro Hunger, Andres Nowak, Charlotte Läuchli, Eric Lasseur, Jean-Yves Roig, Olivier Serrano, Sylvain Calassou, François Guillocheau, Sébastien Castelltort
Publikováno v:
Global and Planetary Change
Global and Planetary Change, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, Elsevier, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, vol. 212, pp. 103794
Global and Planetary Change, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, Elsevier, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, vol. 212, pp. 103794
International audience; The Paleogene records the most prominent global climate change of the Cenozoic Era with a shift from a greenhouse to an icehouse world. Several transient hyperthermal events punctuated this long-term evolution. The most pronou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d85e05f012f9e54ec09bce99020b372
https://insu.hal.science/insu-03621183v2/file/1-s2.0-S0921818122000613-main.pdf
https://insu.hal.science/insu-03621183v2/file/1-s2.0-S0921818122000613-main.pdf
Autor:
Rocio Jaimes-Gutierrez, Thierry Adatte, Emmanuelle Puceat, Maxime Tremblin, Pierre Pellenard, Jean Braun, Sebastien Castelltort
We aim to determine the intensity of chemical weathering of detrital clays, as well as the lag time between the onset of the Paleocene-Eocene Thermal Maximum (PETM) and the chemical weathering response in a source-to-sink system. The PETM was a hyper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b17122f4fc6a1228acea2983974d6f77
https://doi.org/10.5194/egusphere-egu22-5824
https://doi.org/10.5194/egusphere-egu22-5824
Autor:
Sylvain Calassou, Thierry Adatte, Jorge E. Spangenberg, Jean-Yves Roig, Eric Lasseur, Arnaud Grauls, Olivier Serrano, Charlotte Fillon, Maxime Tremblin, Hassan Khozyem, François Guillocheau, Sébastien Castelltort
The Paleocene-Eocene thermal maximum (PETM; ~55.6 Ma) is one of the most pronounced and the best known of the transient hyperthermal events of the Paleogene. The PETM is characterized by global warming, a significant perturbation of the carbon cycle,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a375961facbd238c0fc615c9d71d983
https://doi.org/10.5194/egusphere-egu21-12788
https://doi.org/10.5194/egusphere-egu21-12788
Autor:
Stephen E. Watkins, Guy Simpson, Laure Guerit, Frédéric Arlaud, Valentin Marguin, Marine Prieur, Nikhil Sharma, Maxime Tremblin, Luis Valero, Abdallah S. Zaki, Sébastien Castelltort
Fluvial stratigraphy is the product of changes in Earth’s history and inverting this record has often resulted in interpretations associated with changes in base-level caused by sea-level and/or basement subsidence (downstream drivers). Similarly,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3bf38b078347da7fd9062a62fe36ba1
https://doi.org/10.5194/egusphere-egu21-12642
https://doi.org/10.5194/egusphere-egu21-12642
Autor:
Eric Lasseur, Maxime Tremblin, François Guillocheau, Sébastien Castelltort, Sylvain Calassou, Jean-Yves Roig, Hassan Khozyem, Thierry Adatte, Charlotte Fillon, Olivier Serrano, Jorge E. Spangenberg
The Palaeogene represents the last “greenhouse” period characterized by high atmospheric CO2 concentrations and warm surface temperatures. This long-term climatic state was punctuated by several transient hyperthermal events. These events are rec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fee65668eaba4d080ebed529d36137bd
https://doi.org/10.5194/egusphere-egu2020-9792
https://doi.org/10.5194/egusphere-egu2020-9792
Autor:
Maxime Tremblin, Frédéric Arlaud, Stephen E. Watkins, Guy Simpson, Luis Valero, Abdallah S. Zaki, N. Sharma, Sébastien Castelltort
Stratigraphic architecture of fluvial deposits is often interpreted as a record of changes in accommodation created by absolute sea-level change, subsidence, or a combination of both (downstream drivers). An increase or decrease in accommodation caus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8634a60916114baffaa2f52475f084f
https://doi.org/10.5194/egusphere-egu2020-15932
https://doi.org/10.5194/egusphere-egu2020-15932