Modification of Ca isotope and trace metal composition of the major matrices involved in shell formation of Mytilus edulis
Modification of Ca isotope and trace metal composition of the major matrices involved in shell formation of Mytilus edulis
复制标题
贻贝壳形成主要基质的钙同位素和痕量金属组成的修饰
DOI:
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发表时间:
2008
期刊:
影响因子:
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通讯作者:
K. Zumholz
中科院分区:
文献类型:
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作者:
A. Heinemann;J. Fietzke;A. Eisenhauer;K. Zumholz
In this study we present the first combined investigation into the composition of the major matrices involved in calcification processes (surrounding water, extrapallial fluid, aragonite, and calcite) of Mytilus edulis with respect to their calcium isotope (δ44/40Ca) and elemental compositions (Sr/Ca and Mg/Ca). Our aim was to examine the suitability of Mytilus edulis as a proxy archive and to contribute to the understanding of the process of biomineralization. Mytilus edulis specimens were live collected from the Schwentine Estuary, Kiel Fjord, and North Sea (Sylt). δ44/40Ca was determined by thermal ionization mass spectrometry (TIMS) accompanied by measurements of Mg/Ca and Sr/Ca using inductively coupled plasma–optical emission spectroscopy (ICP‐OES). The elemental and isotopic compositions of the investigated matrices showed systematic offsets. The carbonates are strongly depleted in their magnesium and strontium concentrations and fractionated toward lighter calcium isotope compositions relative to the surrounding Schwentine Estuary water. The opposite is observed for the extrapallial fluid (EPF). Our findings extend the results of previous studies reporting a strong biological control and the interaction of different environmental conditions influencing biomineralization. Future studies should focus on the temporal development of the interrelation between the different matrices.