Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 9, 1897-1914, 2012
https://doi.org/10.5194/bg-9-1897-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
29 May 2012
Marine bivalve shell geochemistry and ultrastructure from modern low pH environments: environmental effect versus experimental bias
S. Hahn1, R. Rodolfo-Metalpa2, E. Griesshaber3, W. W. Schmahl3, D. Buhl1, J. M. Hall-Spencer2, C. Baggini2, K. T. Fehr3, and A. Immenhauser1 1Inst. of Geology, Mineralogy and Geophysics, Ruhr-University Bochum, Universitätsstraße 150, 44801 Bochum, Germany
2Marine Institute, Marine Biology and Ecology Research Centre, University of Plymouth, A428, Portland Square, Drake Circus, Plymouth, Devon, PL4 8AA, UK
3Dept. of Earth and Environmental Science, Ludwig Maximilian University, Theresienstraße 41, 80333 Munich, Germany
Abstract. Bivalve shells can provide excellent archives of past environmental change but have not been used to interpret ocean acidification events. We investigated carbon, oxygen and trace element records from different shell layers in the mussels Mytilus galloprovincialis combined with detailed investigations of the shell ultrastructure. Mussels from the harbour of Ischia (Mediterranean, Italy) were transplanted and grown in water with mean pHT 7.3 and mean pHT 8.1 near CO2 vents on the east coast of the island. Most prominently, the shells recorded the shock of transplantation, both in their shell ultrastructure, textural and geochemical record. Shell calcite, precipitated subsequently under acidified seawater responded to the pH gradient by an in part disturbed ultrastructure. Geochemical data from all test sites show a strong metabolic effect that exceeds the influence of the low-pH environment. These field experiments showed that care is needed when interpreting potential ocean acidification signals because various parameters affect shell chemistry and ultrastructure. Besides metabolic processes, seawater pH, factors such as salinity, water temperature, food availability and population density all affect the biogenic carbonate shell archive.

Citation: Hahn, S., Rodolfo-Metalpa, R., Griesshaber, E., Schmahl, W. W., Buhl, D., Hall-Spencer, J. M., Baggini, C., Fehr, K. T., and Immenhauser, A.: Marine bivalve shell geochemistry and ultrastructure from modern low pH environments: environmental effect versus experimental bias, Biogeosciences, 9, 1897-1914, https://doi.org/10.5194/bg-9-1897-2012, 2012.
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