Geology; April 2009; v. 37; no. 4;
p. 351-354; DOI: 10.1130/G25411A.1
© 2009 Geological Society of America
Salinity effects on the Mg/Ca and Sr/Ca in starfish skeletons and the echinoderm relevance for paleoenvironmental reconstructions
Catherine Borremans1,
Julie Hermans1,2,
Sandrine Baillon,
Luc André3 and
Philippe Dubois1,*
1 Laboratoire de Biologie Marine (CP 160/15), Université Libre de Bruxelles, 50 avenue F.D. Roosevelt, B-1050 Brussels, Belgium
2 Département des Invertébrés, Institut Royal des Sciences Naturelles de Belgique, 29 rue Vautier, B-1000 Brussels, Belgium
3 Section de Minéralogie, Pétrographie et Géochimie, Musée Royal d'Afrique Centrale, 13 Leuvensesteenweg, B-3080 Tervuren, Belgium
Correspondence: *E-mail: phdubois{at}ulb.ac.be.
Skeletal Mg/Ca ratios of well-preserved fossil echinoderms have been used to reconstruct past Mg/Ca ratio in seawater up to the Phanerozoic, taking into account the known temperature effect on this ratio. This study investigates the effects of salinity and growth rate on Mg/Ca and Sr/Ca ratios in starfish calcite skeletons grown in experimental conditions. Both ratios are not related to growth rate: on the contrary, both are positively related to salinity. This effect induces an error on the reconstructed Mg/Ca ratio in seawater that may reach 46%. An intriguing inverse relation between skeletal Sr/Ca ratio and temperature was recorded. The salinity effects are presumably due to physiological regulation processes.
Copyright © 2009 by Geological Society of America