Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal, ~56 million years ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. Characterised by surface temperature increases of between 5 – 9 °C and a rapid onset of less than 20 kyr, the PETM has been widely studied as a natura...
Autors principals: | , , , , , , , , , , , , , |
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Format: | Journal article |
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Elsevier
2017
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