(Table S1) Stable carbon and oxygen isotopes and Mg/Ca ratios of planktonic foraminifera from ODP Hole 198-1209B

The Paleocene-Eocene Thermal Maximum (PETM) has been attributed to a rapid rise in greenhouse gas levels. If so, warming should have occurred at all latitudes, although amplified toward the poles. Existing records reveal an increase in high-latitude sea surface temperatures (SSTs) (8° to 10°C) and i...

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Bibliographic Details
Main Authors: Zachos, James C, Wara, Michael W, Bohaty, Steven M, Delaney, Margaret Lois, Petrizzo, Maria Rose, Brill, Amanda, Bralower, Timothy J, Premoli Silva, Isabella
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.772090
https://doi.org/10.1594/PANGAEA.772090