Using Foraminifera Shell Geochemistry to Test Proxies for Paleoclimate Reconstruction

Previous research conducted on Foraminifera tests determined that the elemental concentrations of the shell reflect pH and salinity of the environment these organisms lived in. Changes in concentrations of Boron and Uranium were analyzed because they are both pH and salinity indicators. For this project, sand samples were gathered from two different stations along Terrebonne Bay in the Gulf of Mexico. Each station had a different depth and salinity. Alabaminella sp. were then separated from the sand sample.

Foraminifera were analyzed using an LA-ICP-MS to determine if there were geochemical differences in the shells from different stations. If differences were determined to exist, then it would be possible to use these differences to reconstruct changes in past coastal environments.

Because the depth and salinity at each Terrebonne station was different, it was expected that the geochemisty of the shells would also be different. It has been concluded that the Foraminifera shells from each station show no significant variation in their Boron and Uranium concentrations. Therefore, paleoclimate pH and salinity cannot be accurately reconstructed using these Foraminifera collected from Terrebonne Bay. The similarity of the geochemistries is likely due to the short distance between stations, allowing the Foraminifera to easily move from one location to another. Further tests can evaluate whether Foraminifera collected from stations farther apart do show the expected geochemical changes that result from different environments.