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Autor:
G. R. Sharman, E. Szymanski, R. A. Hackworth, A. C. M. Kahn, L. A. Febo, J. Oefinger, G. M. Gregory
Publikováno v:
Climate of the Past, Vol 19, Pp 1743-1775 (2023)
The Paleocene–Eocene Thermal Maximum (PETM) represents the most pronounced hyperthermal of the Cenozoic era and is hypothesized to have resulted in an intensification of the paleohydrologic cycle, including enhanced seasonality and increased sedime
Externí odkaz:
https://doaj.org/article/57305c2ee4e644c2ac3f0cdc8cbe9c94