Strontium and Magnesium in Water and in Crassostrea Calcite
- 5 November 1965
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 150 (3697) , 745-751
- https://doi.org/10.1126/science.150.3697.745
Abstract
Distribution of magnesium and strontium was determined between waters and calcites secreted by the oyster species Crassostrea virginica and C. rhizophorae in natural habitats at eight localities, from Maine to Puerto Rico. The concentration of strontium in the calcite shells increases with increasing temperature in the range 13° to 25°C, and also with increasing Sr++/Ca++ molal ratio in the water. The concentration of magnesium in the shells increases irregularly with temperature, and it is apparently independent of the Mg++/Ca++ ratio in the water. The greater variation with temperature in the distribution factor for magnesium may be related to genetic differences between semi-isolated populations.This publication has 9 references indexed in Scilit:
- Paleoecological problems of Mg and Sr in biogenic calcites in light of recent thermodynamic dataGeochimica et Cosmochimica Acta, 1965
- The coprecipitation of cations with CaCO3—II. The coprecipitation of Sr+2 with calcite between 90° and 100°CGeochimica et Cosmochimica Acta, 1964
- On Some Aspects of the Chemical Evolution of Cave WatersThe Journal of Geology, 1964
- COMPARATIVE FIXATION OF CALCIUM AND STRONTIUM BY SNAIL SHELLAnnals of the New York Academy of Sciences, 1963
- TRACE ELEMENTS IN RECENT MOLLUSK SHELLSLimnology and Oceanography, 1963
- Salinity Response of Trace Element Concentration in Crassostrea virginicaNature, 1961
- The occurrence of magnesian calcites in natureGeochimica et Cosmochimica Acta, 1955
- Aspects of the Biogeochemistry of Magnesium 1. Calcareous Marine OrganismsThe Journal of Geology, 1954
- A Solid Solution between Calcite and DolomiteThe Journal of Geology, 1952