DIATOM ASSEMBLAGES & GEOCHEMICAL ANALYSIS OF TERRE HAUTE, INDIANA’S HISTORIC INDUSTRAIL PARK
In June 2013, a 68-cm sediment core was collected from one of the IP holding ponds. The core has been analyzed using a combination of fossil diatom assemblage and geochemical analyses in order to isolate potential sources of pollution. Periodic flooding from the Wabash River may be responsible for abrupt changes in the diatom flora through time, recorded as more diverse taxa and those associated with the river are introduced into the sediment. Eutrophic indicator diatom taxa such as Stephanodiscus hantzschii and Cyclostephanos dubius are present in recent sediments and several diatom specimens have been observed with minor teratologic deformities, suggesting some possible influence of heavy metals. Slightly deeper into the sediment record the diatom productivity decreases dramatically.
Analysis of dried and crushed sediment samples via a Niton hand held XRF suggest that Zn and Cu concentrations exceed threshold effects levels (TEL) throughout the core. Pb and Cr concentrations are elevated above TEL only near the bottom of the core, while Cd concentrations exceed severe effects levels near the top of the core. These values represent significant heavy metal accumulation in the pond likely from multiple environmental sources. Further geochemical analyses will include detailed phosphorus geochemistry and acidification of samples and analysis via Inductively Coupled Plasma-Optical Emission Spectroscopy for an estimate of metal bioavailability.