Planktonic foraminifera, nannofossils and stable isotope record across tghe Paleocene-Eocene thermal maximum of ODP Hole 113-690B, supplement to: Kelly, Daniel Clay; Zachos, James C; Bralower, Timothy J; Schellenberg, Stephen A (2005): Enhanced terrestrial weathering/runoff and surface ocean carbonate production during the recovery stages of the Paleocene-Eocene thermal maximum. Paleoceanography, 20(4), PA4023
The carbonate saturation profile of the oceans shoaled markedly during a transient global warming event known as the Paleocene-Eocene thermal maximum (PETM) (circa 55 Ma). The rapid release of large quantities of carbon into the ocean-atmosphere system is believed to have triggered this intense epis...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA - Data Publisher for Earth & Environmental Science
2005
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.836317 https://doi.pangaea.de/10.1594/PANGAEA.836317 |