Geochemical and palynological measurements from the ODP Leg 189 at Site 1172 on the East Tasman Plateau
A brief (~150 kyr) period of widespread global average surface warming marks the transition between the Paleocene and Eocene epochs, ~56 million years ago. This so-called "Paleocene-Eocene thermal maximum" (PETM) is associated with the massive injection of 13C-depleted carbon, reflected in...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2011
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.756399 https://doi.org/10.1594/PANGAEA.756399 |