Effect of different seawater Mg concentrations on calcification in two benthic foraminifers.

Mar Micropaleontol

Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, D-27570 Bremerhaven, Germany ; Royal Netherlands Institute for Sea Research, Landsdiep 4, 't Horntje, Texel 1797 SZ, The Netherlands ; Department of Earth Sciences, University of Utrecht, Budapestlaan 4, 3584 CD Utrecht, The Netherlands.

Published: December 2014

Magnesium, incorporated in foraminiferal calcite (Mg/Ca), is used intensively to reconstruct past seawater temperatures but, in addition to temperature, the Mg/Ca of foraminiferal tests also depends on the ratio of Mg and Ca in seawater (Mg/Ca). The physiological mechanisms responsible for these proxy relationships are still unknown. This culture study investigates the impact of different seawater [Mg] on calcification in two benthic foraminiferal species precipitating contrasting Mg/Ca: , producing low-Mg calcite and , producing intermediate-Mg calcite. Foraminiferal growth and test thickness were determined and, Mg/Ca was analyzed using Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry (LA-ICP-MS). Results show that at present-day seawater Mg/Ca of ~ 5, both species have highest growth rates, reflecting their adaptation to modern seawater element concentrations. Test thickness is not significantly affected by different Mg/Ca. The relationship between Mg/Ca and Mg/Ca shows a distinct positive y-axis intercept, possibly reflecting at least two processes involved in foraminiferal biomineralization. The associated Mg partition (D) changes non-linearly with increasing Mg/Ca, hence suggesting that the D is best described by an exponential function approaching an asymptote.

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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4459688PMC
http://dx.doi.org/10.1016/j.marmicro.2014.09.003DOI Listing

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