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...
Main Authors: | , , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2010
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.738505 https://doi.org/10.1594/PANGAEA.738505 |