The Paleocene-Eocene boundary in ODP Leg 208 sites

The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release of ~2000 * 10**9 metric tons of carbon in the form of methane. In theory, oxidation and ocean absorption of this carbon should have lowerd deep-sea pH, thereby triggering a rapid (<10,000-year) shoaling of the ca...

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Bibliographic Details
Main Authors: Zachos, James C, Röhl, Ursula, Schellenberg, Stephen A, Sluijs, Appy, Hodell, David A, Kelly, Daniel Clay, Thomas, Ellen, Nicolo, Micah J, Raffi, Isabella, Lourens, Lucas Joost, McCarren, H, Kroon, Dick
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.772051
https://doi.org/10.1594/PANGAEA.772051