FRESH-WATER BIVALVES (UNIONIDAE), DISEQUILIBRIUM ISOTOPIC FRACTIONATION, AND TEMPERATURES

Citation
De. Fastovsky et al., FRESH-WATER BIVALVES (UNIONIDAE), DISEQUILIBRIUM ISOTOPIC FRACTIONATION, AND TEMPERATURES, Palaios, 8(6), 1993, pp. 602-608
Citations number
35
Categorie Soggetti
Geology,Paleontology
Journal title
ISSN journal
08831351
Volume
8
Issue
6
Year of publication
1993
Pages
602 - 608
Database
ISI
SICI code
0883-1351(1993)8:6<602:FB(DIF>2.0.ZU;2-N
Abstract
A one-year study of two ponds and one river in Rhode Island was implem ented to determine whether Recent freshwater bivalves (Unionidae: Elli ptio complanata) secrete aragonite in oxygen isotopic equilibrium with the water in which they grow. Water samples and animals were retrieve d from each locality at two-week intervals for one year. The oxygen an d carbon stable isotopic composition of the youngest growth increment of the shells (shell edge) and the oxygen isotopic composition of wate r were measured and compared with the temperatures recorded during sam pling, via published equilibrium fractionation relationships. Elliptio does not secrete shell material in equilibrium with the ambient water . The disequilibrium is manifested as an offset of approximately -2 pa rts per thousand in the summer and -2.5 parts per thousand in the wint er. Incorporation of metabolic CO2 may contribute in large part to thi s offset.