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Gradual global warming might trigger the release of large amounts of carbon from natural reservoirs such as submarine methane hydrates and permafrost, exacerbating the effects of human-caused carbon emissions. These "tipping points" in the carbon cyc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bc2b4459877a74f7a991244fc474ed7
https://doi.org/10.5194/egusphere-egu23-14530
https://doi.org/10.5194/egusphere-egu23-14530
Autor:
Shruti Setty, Margot J. Cramwinckel, Egbert H. van Nes, Ingrid A. van de Leemput, Henk A. Dijkstra, Lucas J Lourens, Marten Scheffer, Appy Sluijs
Publikováno v:
Science Advances, 9(14), eade5466-eade5466
Science Advances 9 (2023) 14
Science Advances 9 (2023) 14
Superimposed on long-term late Paleocene–early Eocene warming (~59 to 52 million years ago), Earth’s climate experienced a series of abrupt perturbations, characterized by massive carbon input into the ocean-atmosphere system and global warming.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::478a7e7fa9dbe8dd5fca1e70fad11b10
https://doi.org/10.1126/sciadv.ade5466
https://doi.org/10.1126/sciadv.ade5466
Autor:
Shruti Setty, Margot Cramwinckel, Ingrid van de Leemput, Egbert H. van Nes, Lucas J. Lourens, Appy Sluijs, Marten Scheffer
The Paleocene-Eocene Thermal Maximum (PETM; 56 Ma) and Eocene Thermal Maximum 2 and 3 (ETM2; 54.06 Ma and ETM3; 52.87 Ma) were three of a series of abrupt climate and carbon cycle perturbations, characterized by massive carbon input into the ocean-at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd2a8e6b6ba70b1496bf6f0fb87758bd
https://doi.org/10.5194/egusphere-egu22-10628
https://doi.org/10.5194/egusphere-egu22-10628