The evolution of early diagenetic signals in Bering Sea subseafloor sediments in response to varying organic carbon deposition over the last 4.3 Ma

Transient pore-water and solid-phase signatures in deep subseafloor marine sediments, resulting from changes in both the amount and the quality of the organic matter input, are common but often difficult to interpret. We combined high-resolution pore-water and solid-phase data from Integrated Ocean...

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Bibliographic Details
Main Authors: Wehrmann, L., Arndt, S., Marz, C., Ferdelman, T., Brunner, B.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0001-C6CB-B
http://hdl.handle.net/21.11116/0000-0006-F446-8