(Table S) Planktonic foraminifera I/Ca during the PETM

As yet no evidence has been presented for pervasive deoxygenation in the upper water column through expansion of Oxygen Minimum Zones (OMZs) during the PETM. We apply a novel proxy for paleo-redox conditions, the iodine to calcium ratio (I/Ca) in bulk coarse fraction sediment and planktonic foramini...

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Bibliographic Details
Main Authors: Zhou, Xiaoli, Thomas, Ellen, Rickaby, Rosalind E M, Winguth, Arne M E, Lu, Zunli
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Age
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.869448
https://doi.org/10.1594/PANGAEA.869448