Biological forcing controls the chemistry of reef-building coral skeleton

• Published in: Geophysical Research Letters, vol. 34, p. -
• Publication date: 2007

[1] We present analyses of major elements C and Ca and trace elements N, S, Mg and Sr in a Porites sp. exoskeleton with a spatial resolution better than similar to 150 nm. Trace element variations are evaluated directly against the ultrastructure of the skeleton and are ascribed to dynamic biological forcing. Individual growth layers in the bulk fibrous aragonite skeleton form on sub-daily timescales. Magnesium concentration variations are dramatically correlated with the growth layers, but are uncorrelated with Sr concentration variations. Observed (sub) seasonal relationships between water temperature and skeletal trace-element chemistry are secondary, mediated by sensitive biological processes to which classical thermodynamic formalism does not apply.

Keywords: Scleractinian Coral ; Paleotemperature Proxy ; Stylophora-Pistillata ; Symbiotic Coral ; Trace-Elements ; Ion Microprobe ; Aragonite ; Strontium ; Biomineralization ; Ultrastructure

Reference

• EPFL-ARTICLE-177108
• doi:10.1029/2006GL028657
• View record in Web of Science

Record created on 2012-05-15, modified on 2016-08-09