Ostracod Geochemistry as a Proxy for Paleoenvironmental Change

Recent studies in the field of paleoceanography suggest that the geochemistry of ostracods, through their uptake of elements from their environment, has the potential to act as proxies for paleoenvironmental change. For example, pH-sensitive elements such as Boron and Uranium potentially record changes in the environment’s pH, while temperature sensitive elements Magnesium and Strontium record temperature changes. If this is the case, a random sample of ostracods taken from the same environment should have very little variation in their elemental concentration. This hypothesis was tested using a group of ostracods of the genus Cyprideis taken from a horizon in a hypersaline lake in the southwest of Big Darby Island, Bahamas.

Laser-ablation inductively coupled plasma mass spectrometer (LA-ICP-MS) was used in order to measure the elemental concentrations from each ostracod carapace. Despite differences in size and species, the ostracods showed very little variations in Boron and Uranium concentrations. However, Magnesium and Strontium showed more elemental variation in each ostracod. This data suggests that ostracod carapaces do have the potential to act as proxies for environmental pH change; however, their potential to record temperature changes is inconclusive based on these results.