2023
DOI: 10.1016/j.gloplacha.2023.104175
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Freshwater ecosystem collapse and mass mortalities at the Paleocene-Eocene thermal maximum

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Cited by 3 publications
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“…The PETM lasted less than 200 kyr, but it resulted in a global temperature increase of about 5-8 • C [9,10], accompanied by a negative carbon isotope excursion (CIE) of 2-7‰ [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15]. There is evidence that the PETM led to a significant increase in precipitation at the low and middle latitudes of East Asia [16][17][18]. The latest research results challenge the view that East Asia was in a hot and arid climate for a long time in the early Paleogene.…”
Section: Introductionmentioning
confidence: 99%
“…The PETM lasted less than 200 kyr, but it resulted in a global temperature increase of about 5-8 • C [9,10], accompanied by a negative carbon isotope excursion (CIE) of 2-7‰ [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15]. There is evidence that the PETM led to a significant increase in precipitation at the low and middle latitudes of East Asia [16][17][18]. The latest research results challenge the view that East Asia was in a hot and arid climate for a long time in the early Paleogene.…”
Section: Introductionmentioning
confidence: 99%