xmlui.dri2xhtml.METS-1.0.item-citation:Geochimica et Cosmochimica Acta, 2004, 68, 22, 4665-4678
Date:2004
Abstract:
Calcium isotopic variations in carbonates, both marine organisms and inorganic systems, have recently been interpreted as a possible seawater temperature recorder [1,2]. In order to understand the behavior of calcium isotopes during precipitation of Ca-carbonate, synthetic calcite growth experiments were carried out at constant temperature and under various pH and alkalinity conditions.