CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 11
Presentation Time: 4:15 PM

AFTER THE SPILL: METAL CYCLING IN GULF COAST WETLANDS


KEIMOWITZ, Alison R.1, LEE, Ming-Kuo2, SAUNDERS, James A.3, LAMBORG, Carl H.4, OKEKE, Benedict5, NATTER, Michael6, KEEVAN, Jeffrey6, LEWIS, Deirdre1 and CHUNG, Hansol1, (1)Chemistry, Vassar College, 124 Raymond Ave, Poughkeepsie, NY 12604, (2)Department of Geology and Geography, Auburn University, Auburn, AL 36849, (3)Department of Geosciences, Auburn University, 210 Petrie Hall, Auburn, AL 36849, (4)Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, (5)Biology, Auburn University, Montgomery, 36124, (6)Department of Geology and Geography, Auburn University, AL 36849, alkeimowitz@vassar.edu

The Deepwater Horizon explosion (April 20, 2010) and subsequent oil spill contaminated hundreds of miles of Gulf Coast wetlands. It was expected that this influx of organic matter would serve as an electron donor to the system, thereby increasing biogeochemical activity and causing metals, as terminal electron acceptors, to be reduced and mobilized. Increased arsenic mobilization and mercury methylation are of special concern due to the toxicity of these elements. Arsenic may be mobilized by its reduction from As(V) to As(III), the more mobile form. Mercury may be methylated, and thereby bioaccumulate, due to the activity of sulfur reducing bacteria. Sediment cores and porewaters from ten Alabama, Mississippi, and Louisiana wetlands were collected and analyzed to examine this hypothesis. Initial data indicate that evidence of oil contamination is present over a large spatial extent and that strongly reducing conditions were attained, as indicated by high reduced sulfur concentrations. However, porewater metal concentrations remain low and evidence of altered metal cycling is limited. Explanations for this will be explored using both aqueous and solid phase analyses.
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