2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)

Paper No. 150-12
Presentation Time: 4:35 PM

INVESTIGATING HUMAN IMPACT ON THE JORDAN RIVER USING SEDIMENTARY AND STABLE ISOTOPIC RECORDS


ROBERTSON, Paul1, KERSWELL, Buchanan1, WALTHER, Suzanne2, WANG, Weihong3, CARLING, Gregory T.4, REY, Kevin A.5 and NELSON, Stephen T.6, (1)Department of Earth Science, Utah Valley University, 800 West University Parkway, Orem, UT 84058, (2)Department of Environmental and Ocean Sciences, University of San Diego, 5998 Alcala Park, San Diego, CA 92110, (3)Department of Earth Science, Utah Valley University, 800 W. University Parkway, Orem, UT 84058, (4)Geological Sciences, Brigham Young University, Provo, UT 84602, (5)Department of Geological Sciences, Brigham Young University, Provo, UT 84602, (6)Dept. of Geological Sciences, Brigham Young University, S-389 ESC, Provo, UT 84602

Changes in sediment size over time can represent past river dynamics and changes in stable isotope concentrations with depth can highlight environmental changes in aquatic ecosystems. Together, sedimentary and isotope data from sediment cores can reveal potential delivery processes and probable sources of organic matter inputs, particularly those from human activities. In this study, a total of nine one meter-long sediment cores along three transects were taken in June 2013. We subsampled the cores at 5cm intervals for δ13C, δ15N, C, N and grain size analyses. We used the depth profiles of the data to characterize important changes due to invasive species, farming practices and river dynamics. Our principle objectives were to answer the following questions: (1) How has the overall ecosystem changed with respect to vegetation and river dynamics? (2) How have the abundances of carbon and nitrogen isotopes changed prior to and after European settlement, and what are the carbon and nitrogen sources to Jordan River? Preliminary data has shown that the grain size percentages (clay, silt, sand) in several cores exhibit large shifts, particularly in JR2b, which coarsens dramatically in the top 20 cm of the core. These changes indicate variations in flow between the past and present. The depth profiles of δ13C showed large variations at different depths of the cores, ranging from -33‰ to -24‰ (vs. V-PDB). The large fluctuations of δ13C of sediment organic matter indicated rapid organic matter source change in the system post-European settlement in 1840, likely in part due to the introduction of the invasive species Phragmites australis. The depth profiles of δ15N have showed higher δ15N values in the upper sediment layers of the cores, which were likely due to historical nutrient discharges into the river associated with farming and untreated sewage. These data contribute to a growing interdisciplinary dataset that provide insight into the Utah Lake/Jordan River history.