Strontium/lithium ratio in aragonitic shells of Cerastoderma edule (Bivalvia) - A new potential temperature proxy for brackish environments
Strontium/lithium ratio in aragonitic shells of Cerastoderma edule (Bivalvia) - A new potential temperature proxy for brackish environments
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DOI:
10.1016/j.chemgeo.2015.10.030
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发表时间:
2015-12-06
期刊:
影响因子:
3.9
通讯作者:
Mertz-Kraus, Regina
中科院分区:
文献类型:
--
作者:
Fuellenbach, Christoph S.;Schoene, Bernd R.;Mertz-Kraus, Regina
Quantitative reconstruction of water temperature from shells of bivalve mollusks is still a very challenging task. For example, in highly variable environments such as intertidal zones, shell oxygen isotope values can only provide reliable temperature estimates if the delta O-18(water) signature during the time of growth is known. Furthermore, trace element-to-calcium ratios such as Sr/Ca or Mg/Ca often do not serve as reliable paleothermometers, because their incorporation into bivalve shells is known to be strongly biologically controlled. Here, we present a potential novel temperature proxy which is based on the Sr/Li-shell ratio of the intertidal bivalve Cerastoderma edule. Up to 81% of the variability in Sr/Li-shell is mathematically explained by water temperature. It is suggested that vital effects on the incorporation of Sr and Li into the aragonitic shells are largely eliminated by normalizing Sr/Ca to Li/Ca. Growth rate does not control the incorporation of Sr or Li into the shell of C. edule. By using this new proxy, it was possible to estimate water temperature from C. edule with an uncertainty of +/- 1.5 degrees C. Future studies are required to test if Sr/Li-shell also serves as a reliable temperature proxy in other bivalve species and in other environments. (C) 2015 Elsevier B.V. All rights reserved.