Stable isotope fractionation between mollusc shells and marine waters from Martinique Island

Forty-nine aragonitic and calcitic shells from 14 species of marine tropical molluscs (Bivalvia, Gastropoda, Polyplacophora) and ambient waters from Martinique have been analyzed for their carbon and oxygen isotope compositions. Mineralogy of shells was systematically determined by Raman spectroscopy that reveals composite shell structures and early processes of diagenetic alteration. In mangrove, brackish waters result from the mixing between 89 +/- 1% of seawater and 11 +/- 1% of freshwater, a hydrological budget quantified by both oxygen isotope and salinity mass balance calculations. Mollusc shells from the mangrove environment (S = 31parts per thousand; delta(18)O = 0.5parts per thousand) are characterized by mean delta(13)C values (- 1.2parts per thousand) lower than those (+ 2.6parts per thousand) living in the open sea (S = 35parts per thousand; delta(18)O = 1parts per thousand). These low carbon isotope compositions result from the oxidation of organic matter into bicarbonate ions used in the building of mollusc shells. The oxygen isotope compositions of the studied mollusc species are mainly controlled by the temperature and composition of seawater whereas the role of the so-called vital effects is negligible. Contrasting with carbon isotopes, variability in the delta(18)O values among and within species of mollusc shells is very low (1sigma=0.15) for a given littoral environment. Using ambient temperatures of seawater (28-30 degreesC), oxygen isotope fractionations between all studied living species and environmental waters match those extrapolated from the fractionation equation established for molluscs by Grossman and Ku [Chem. Geol., Isot. Geosci. Sect. 59, (1986) 59] in the range 3-20 degreesC. By analyzing calcite and aragonite layers from the same shell or by comparing shells from different species living in the same environment, there is no evidence that oxygen isotope fractionation between aragonite and water differs from that between calcite and water. On the basis of these results, we conclude that the oxygen isotope compositions of shells from most fossil mollusc species are suitable to estimate past seawater temperatures at any paleolatitude. (C) 2004 Elsevier B.V. All rights reserved.