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Stable isotope fractionation of strontium in coccolithophore calcite: Influence of temperature and carbonate chemistry
Author(s) -
Müller M. N.,
Krabbenhöft A.,
Vollstaedt H.,
Brandini F. P.,
Eisenhauer A.
Publication year - 2018
Publication title -
geobiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.859
H-Index - 72
eISSN - 1472-4669
pISSN - 1472-4677
DOI - 10.1111/gbi.12276
Subject(s) - coccolithophore , calcite , strontium , carbonate , coccolith , fractionation , biomineralization , geochemistry , isotopes of strontium , geology , chemistry , isotope fractionation , isotope , mineralogy , stable isotope ratio , environmental chemistry , paleontology , phytoplankton , physics , quantum mechanics , organic chemistry , nutrient
Marine calcifying eukaryotic phytoplankton (coccolithophores) is a major contributor to the pelagic production of Ca CO 3 and plays an important role in the biogeochemical cycles of C, Ca and other divalent cations present in the crystal structure of calcite. The geochemical signature of coccolithophore calcite is used as palaeoproxy to reconstruct past environmental conditions and to understand the underlying physiological mechanisms (vital effects) and precipitation kinetics. Here, we present the stable Sr isotope fractionation between seawater and calcite (Δ 88/86 Sr) of laboratory cultured coccolithophores in individual dependence of temperature and seawater carbonate chemistry. Coccolithophores were cultured within a temperature and a p CO 2 range from 10 to 25°C and from 175 to 1,240 μatm, respectively. Both environmental drivers induced a significant linear increase in coccolith stable Sr isotope fractionation. The temperature correlation at constant p CO 2 for Emiliania huxleyi and Coccolithus braarudii is expressed as Δ 88/86 Sr = −7.611 × 10 −3 T + 0.0061. The relation of Δ 88/86 Sr to p CO 2 was tested in Emiliania huxleyi at 10 and 20°C and resulted in Δ 88/86 Sr = −5.394 × 10 −5 p CO 2 – 0.0920 and Δ 88/86 Sr = −5.742 × 10 −5 p CO 2 – 0.1351, respectively. No consistent relationship was found between coccolith Δ 88/86 Sr and cellular physiology impeding a direct application of fossil coccolith Δ 88/86 Sr as coccolithophore productivity proxy. An overall significant correlation was detected between the elemental distribution coefficient ( D Sr ) and Δ 88/86 Sr similar to inorganic calcite with a physiologically induced offset. Our observations indicate (i) that temperature and p CO 2 induce specific effects on coccolith Δ 88/86 Sr values and (ii) that strontium elemental ratios and stable isotope fractionation are mainly controlled by precipitation kinetics when embedded into the crystal lattice and subject to vital effects during the transmembrane transport from seawater to the site of calcification. These results provide an important step to develop a coccolith Δ 88/86 Sr palaeoproxy complementing the existing toolbox of palaeoceanography.