Iron Biogeochemical Cycle Throughout Earth History

Iron (Fe) is present over a very wide range of redox conditions and is one of most the important nutrients for phytoplankton growth in the ocean. In a marine environment, Fe composition in the sediments is intimately linked to the chemistry of the waters from which they precipitate. Particularly, th...

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Bibliographic Details
Main Author: Kenlee, Bridget
Other Authors: Lyons, Timothy W
Format: Other/Unknown Material
Language:English
Published: eScholarship, University of California 2021
Subjects:
Biogeochemistry
Geochemistry
Paleoclimate science
Pirie
Scotia Sea
Southern Ocean
North Atlantic
Online Access:https://escholarship.org/uc/item/72s3c24r

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