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Geophysical Monograph Series

Trace elements in marine ostracodes

Publication ,  Chapter
Dwyer, GS; Cronin, TM; Baker, PA
January 1, 2002

Extending the work of Cadot, Kaesler, De Deckker, Chivas, and Corrège, we have measured the elemental chemistry of shells of marine ostracodes to evaluate the usefulness of ostracode shell chemistry as a paleoenvironmental proxy. Our work has focused primarily on Mg/Ca, Sr/Ca, and Na/Ca ratios of two common genera: deep-sea genus Krithe and shallow marine/estuarine genus Loxoconcha. We evaluated in vivo effects including genus, species, gender, ontogeny, shell size, intra-shell heterogeneity (Mg), water temperature, and salinity, and postmortem diagenetic effects including partial dissolution, recrystallization, and shell surface contamination. Analysis of modern (core-top), fossil, and laboratory- raised specimens across a wide range of temperature and salinity conditions confirms earlier work indicating that Krithe and Loxoconcha Mg/Ca ratios are dominantly controlled by water temperature. Sr/Ca and Na/Ca ratios co-vary with temperature in core-top Krithe, but not in cultured Loxoconcha suggesting that the Krithe Sr/Ca and Na/Ca correlation with temperature may be related to another variable that broadly co-varies with temperature. Phylogenetic and ontogenetic effects are also indicated, including different Mg-thermodependence and intra-shell Mg distribution between Krithe and Loxoconcha. Inter-specific effects are suggested for two species of Krithe. Magnesium uptake in eldest juvenile shells seems to be identical to that of adult shells, thus greatly increasing the amount of shell material available for paleoenvironmental studies. No salinity effects were observed. Shell Na/Ca ratios showed a dramatic decrease with increasing dissolution (natural and artificial) in waters that are undersaturated with respect to calcite, whereas Mg/Ca ratios displayed a minor decrease and Sr/Ca ratios showed no change. Of the ratios studied, Mg/Ca offers the most promise for Quaternary marine studies as a paleothermometer. Further calibration studies are needed to better understand the marine ostracode Mg/Ca-paleothermometer.

Duke Scholars

DOI

Publication Date

January 1, 2002

Volume

131

Start / End Page

205 / 225
 

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Dwyer, G. S., Cronin, T. M., & Baker, P. A. (2002). Trace elements in marine ostracodes. In Geophysical Monograph Series (Vol. 131, pp. 205–225). https://doi.org/10.1029/131GM11
Dwyer, G. S., T. M. Cronin, and P. A. Baker. “Trace elements in marine ostracodes.” In Geophysical Monograph Series, 131:205–25, 2002. https://doi.org/10.1029/131GM11.
Dwyer GS, Cronin TM, Baker PA. Trace elements in marine ostracodes. In: Geophysical Monograph Series. 2002. p. 205–25.
Dwyer, G. S., et al. “Trace elements in marine ostracodes.” Geophysical Monograph Series, vol. 131, 2002, pp. 205–25. Scopus, doi:10.1029/131GM11.
Dwyer GS, Cronin TM, Baker PA. Trace elements in marine ostracodes. Geophysical Monograph Series. 2002. p. 205–225.

DOI

Publication Date

January 1, 2002

Volume

131

Start / End Page

205 / 225