VARIATION IN STABLE ISOTOPES OF FRESHWATER MUSSEL SHELLS IN THE LICKING RIVER OF KENTUCKY
Mussel shells representing 12 locations and seven species were collected from the two main branches of the Licking River. The organic δ13C and δ15N from the periostracum and δ13C, δ18O, and the δ15N of the prismatic layer were measured on the outermost growth band on all samples considered, along with multiple growth horizons on a subset of samples. To calibrate this data set, water and sediment samples were collected across a seasonal cycle, with sampling at February, May, and August 2018. Samples were analyzed for δ18O and δD of water, δ13C of DIC, and organic δ13C and δ15N of sediment.
Preliminary data of mussel shells from the Licking River in Kentucky show relationships linked to location, as well as differences between species. There is a general trend of isotope values for both inorganic carbon and oxygen that vary by stream location (upstream/downstream), as well as variability between the two main forks of the Licking River. Additionally, carbonate-bound δ15N was compared to the δ15N the outer periostracum at the same growth horizon. The results across 22 samples, including five species, were the same within analytical error.
These results will be placed in the context of the impact human activity has on freshwater systems, including multiple human constructed dams along the river as well as any changes in land use. Sampling sites are located on both sides of four dams, as well as spatially distributed to allow changes resulting from human activity to be visible. These results will also provide greater insight into the seasonal cycles of mussel growth and diet, and whether either has been affected by human activity within the length of the mussel’s seasonal records.