Geochemistry and P and Fe fractionation in anoxic sediments

We investigated the phosphorus (P) and iron (Fe) fractionation in four cores with anoxic sediments, deposited during the mid-Cretaceous oceanic anoxic event 2 (~94 Ma) and the Paleocene-Eocene thermal maximum (?55 Ma), that were exposed to oxygen after core recovery. Surprisingly, P associated with...

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Bibliographic Details
Main Authors: Kraal, Peter, Slomp, Caroline P, Forster, Astrid, Kuypers, Marcel MM, Sluijs, Appy
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.783338
https://doi.org/10.1594/PANGAEA.783338