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U/Ca in benthic foraminifers: A proxy for the deep-sea carbonate saturation

U/Ca in benthic foraminifers: A proxy for the deep-sea carbonate saturation

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1642299374

U/Ca in benthic foraminifers: A proxy for the deep-sea carbonate saturation

About this item

Full title

U/Ca in benthic foraminifers: A proxy for the deep-sea carbonate saturation

Publisher

Washington: Blackwell Publishing Ltd

Journal title

Geochemistry, geophysics, geosystems : G3, 2011-06, Vol.12 (6), p.np-n/a

Language

English

Formats

Publication information

Publisher

Washington: Blackwell Publishing Ltd

More information

Scope and Contents

Contents

The ocean plays a major role in the global carbon cycle, and attempts to reconstruct past changes in the marine carbonate system are increasing. The speciation of dissolved uranium is sensitive to variations in carbonate system parameters, and previous studies have shown that this is recorded in the uranium‐to‐calcium ratio (U/Ca) of the calcite sh...

Alternative Titles

Full title

U/Ca in benthic foraminifers: A proxy for the deep-sea carbonate saturation

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_1642299374

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1642299374

Other Identifiers

ISSN

1525-2027

E-ISSN

1525-2027

DOI

10.1029/2010GC003344

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