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...

Descripció completa

Dades bibliogràfiques
Autors principals: Carmichael, M, Inglis, G, Badger, M, Naafs, B, Behrooz, L, Remmelzwaal, S, Monteiro, F, Rohrssen, M, Farnsworth, A, Buss, H, Dickson, A, Valdes, P, Lunt, D, Pancost, R
Format: Journal article
Publicat: Elsevier 2017