Effect of different seawater Mg2 + concentrations on calcification in two benthic foraminifers


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Antje.Mewes [ at ] awi.de

Abstract

Magnesium, incorporated in foraminiferal calcite (Mg/CaCC), is used intensively to reconstruct past seawater temperatures but, in addition to temperature, the Mg/CaCC of foraminiferal tests also depends on the ratio of Mg and Ca in seawater (Mg/CaSW). The physiological mechanisms responsible for these proxy relationships are still unknown. This culture study investigates the impact of different seawater [Mg2 +] on calcification in two benthic foraminiferal species precipitating contrasting Mg/CaCC: Ammonia aomoriensis, producing low-Mg calcite and Amphistegina lessonii, 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/CaSW 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/CaSW. The relationship between Mg/CaSW and Mg/CaCC shows a distinct positive y-axis intercept, possibly reflecting at least two processes involved in foraminiferal biomineralization. The associated Mg partition (DMg) changes non-linearly with increasing Mg/CaSW, hence suggesting that the DMg is best described by an exponential function approaching an asymptote.



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ISI/Scopus peer-reviewed
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Published
Eprint ID
36878
DOI 10.1016/j.marmicro.2014.09.003

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Mewes, A. , Langer, G. , De Noojer, L. J. , Bijma, J. and Reichart, G. J. (2014): Effect of different seawater Mg2 + concentrations on calcification in two benthic foraminifers , Marine Micropaleontology, 113 , pp. 56-64 . doi: 10.1016/j.marmicro.2014.09.003


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