Published June 2010 | Version public
Journal Article

A ^(40)K-^(40)Ca perspective on the oceanic calcium cyle

Abstract

This study uses the decay of ^(40)K to ^(40)Ca to investigate the contributions of weathering and hydrothermal fluxes in the oceanic Ca budget. Because of its high K/Ca ratio, the silicate upper crust delivers radiogenic Ca to the oceans, while hydrothermal reactions deliver unradiogenic Ca from the mantle.

Additional Information

© 2010 Published by Elsevier Ltd. Available online 15 May 2010.

Additional details

Identifiers

Eprint ID
47208
DOI
10.1016/j.gca.2010.04.028
Resolver ID
CaltechAUTHORS:20140715-090456536

Dates

Created
2014-07-15
Created from EPrint's datestamp field
Updated
2021-11-10
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