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Fe(II)-carbonate precipitation kinetics and the chemistry of anoxic ferruginous seawater

Abstract:

The chemical evolution of anoxic seawater through time is chronicled in part by the abundance of sedimentary Fe minerals. Our view of the chemical state of the oceans throughout much of Earth’s history, therefore, hinges on understanding the behaviour of Fe2+ in seawater and sedimentary pore water. However, the formation pathways and precipitation rates of a number of sedimentary Fe(II)-minerals are poorly understood. For example, because siderite is widely distributed Precambrian rocks, i...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.epsl.2018.11.010

Authors


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Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Oxford college:
Linacre College
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Oxford college:
St Peter's College
Role:
Author
ORCID:
0000-0003-4415-4231
More from this funder
Funding agency for:
Tosca, N
Grant:
PLP-2015-286
More from this funder
Funding agency for:
Tosca, N
Grant:
PLP-2015-286
Publisher:
Elsevier Publisher's website
Journal:
Earth and Planetary Science Letters Journal website
Volume:
506
Pages:
231-242
Publication date:
2018-11-16
Acceptance date:
2018-11-03
DOI:
ISSN:
0012-821X
Source identifiers:
936833
Keywords:
Pubs id:
pubs:936833
UUID:
uuid:4d25faa5-f4cb-4908-acb0-b18def9fea16
Local pid:
pubs:936833
Deposit date:
2018-11-03

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