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Comment on “What do we know about the evolution of Mg to Ca ratios in seawater?” by Wally Broecker and Jimin Yu

Coggon, Rosalind M., Teagle, Damon A.H. and Dunkley Jones, Tom (2011) Comment on “What do we know about the evolution of Mg to Ca ratios in seawater?” by Wally Broecker and Jimin Yu Paleoceanography, 26, (3), PA3224. (doi:10.1029/2011PA002186).

Record type: Article

Abstract

A record of the Mg/Ca ratio of ancient seawater is essential to understand variations in the major geological processes that control ocean chemistry and for estimating past ocean temperatures. A recent contribution by Broecker and Yu (2011) regarding past seawater Mg/Ca provides an unbalanced assessment of the uncertainties and key assumptions of the methodologies considered. It misrepresents aspects of a new method to estimate past ocean Mg/Ca proposed by Coggon et al. (2010); here we provide clarification of that approach. We estimate the accuracy and precision of seawater Mg/Ca estimates derived from planktonic foraminifera test calcite, the preferred approach of Broecker and Yu. These are shown to be consistent with other records that suggest major changes in seawater cation chemistry. An explanation of how major changes in the Mg/Ca of seawater might occur is beyond the scope of this comment.

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Published date: 2011
Organisations: Ocean and Earth Science, Geochemistry

Identifiers

Local EPrints ID: 201075
URI: http://eprints.soton.ac.uk/id/eprint/201075
ISSN: 0883-8305
PURE UUID: 364b3623-43a8-4f28-84d1-0765e4efa84b
ORCID for Damon A.H. Teagle: ORCID iD orcid.org/0000-0002-4416-8409

Catalogue record

Date deposited: 25 Oct 2011 09:40
Last modified: 18 Jul 2017 11:13

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Contributors

Author: Tom Dunkley Jones

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