Uptake of Mg and Sr in the euryhaline ostracod Cyprideis determined from in vitro experiments

This paper describes a series of in vitro experiments during which juvenile s of the euryhaline ostracod Cyprideis australiensis were grown to adulthoo d in waters of ranging salinities (from 10-70 parts per thousand) and Mg/Ca and Sr/Ca ratios, and under two different constant temperature regimes, 20 degrees and 25 degrees C. Results indicate the following thermodependence for Mg in the calcitic valves of adult Cyprideis australiensis: T(Mg) = 2.6 9 + 5230 x [Mg/Ca](ostracod)/[Mg/Ca](water). A minor thermodependence was a lso found for this ostracod species with respect to the uptake of Sr. There is a very strong relationship between the Mg/Ca of the ostracods and the M g/Ca of the waters in which they moulted. The same can be said between the Sr/Ca of the ostracods and the waters' Sr/Ca. There is no direct relationsh ip between water salinity and either the Mg/Ca ratio nor the Sr/Ca ratio of the ostracod valves. The 20 degrees and 25 degrees C experiments establish ed the following partition coefficients which we believe can be applied to any Cyprideis taxa grown in waters within the 5 to 20 Mg/Ca range: K-D[Mg] = -0.000514 + 0.00019 x Temperature degrees C, and K-D[Sr] = 0.223 + 0.0086 x Temperature degrees C. This relationship for Sr, which has been mentione d for the first time for Cyprideis is tentative. The Mg/Ca of ostracods is strongly dependant on temperature, but this effect can easily be masked by variations in the Mg/Ca of the host water commonly found in natural lakes. Ostracod physiology is adapted to constructing valves from low-Mg calcite, so when growing in waters with high (>30), or very low (<1) Mg/Ca, Cypridei s species will not take up Mg in accordance with the calculated K-D. (C) 19 99 Elsevier Science B.V. All rights reserved.