Sedimentary and carbonate preservation of ODP Sites 1262, 1263 and 1266

Rapid carbon input into the ocean-atmosphere system caused a dramatic shoaling of the lysocline during the Paleocene-Eocene thermal maximum (PETM), a transient (~170 kyr) global warming event that occurred roughly 55 Ma. Carbon cycle models invoking an accelerated carbonate-silicate feedback mechani...

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Bibliographic Details
Main Authors: Kelly, Daniel Clay, Nielsen, Tina M J, McCarren, Heather K, Zachos, James C, Röhl, Ursula
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2010
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738505
https://doi.org/10.1594/PANGAEA.738505