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. 4
Presentation Time: 8:55 AM

ICE-SHEET-DERIVED SUBMARINE GROUNDWATER DISCHARGE ON GREENLAND'S CONTINENTAL SHELF


DEFOOR, Whitney, Earth and Environmental Science, New Mexico Tech, 801 Leroy Place, Socorro, NM 87801, PERSON, Mark, Dept of Earth & Environmental Science, New Mexico Tech, 801 Leroy Place, Socorro, NM 87801, DUGAN, Brandon, Earth Science, Rice University, 6100 Main Street, MS 126, Houston, TX 77005, LIZARRALDE, Dan, Department of Geology and Geophysics, Woods Hole Oceanographic Institution, 266 Woods Hole Rd., MS# 22, Woods Hole, MA 02543, LARSEN, Hans Christian, Integrated Ocean Drilling Program Management Inc, Tokyo University of Marine Science and Technology, 3rd Floor, 2-1-6, Etchujima, Koto-ku, 135-1855, Tokyo, Japan and COHEN, Denis, Geological and Atmospheric Sciences, Iowa State University, 253 Science 1, Ames, IA 50011, mperson@nmt.edu

Isotopically depleted, relatively fresh pore fluids were reported in continental shelf sediments 40 to 100 km off shore, southeastern Greenland during ODP drilling campaign Leg 152 in 1994. This suggests that significant quantities of glacial meltwater may be sequestered in volcanic and/or sedimentary formations on Greenland’s continental shelf. We present a paleohydrologic reconstruction of the late Pleistocene hydrogeology of southeastern Greenland using a finite element model that incorporates fluctuating sea level and ice sheet geometry. We varied permeabilities, δ18O and salinity boundary conditions as well as ice-sheet extent in order to constrain infiltration rates. Our model shows that the emplacement of isotopically depleted freshwater into offshore aquifers was greatest during the last glacial maximum when the ice sheet extended to near the shelf-slope break. Model results further suggest that significant temporal variations in submarine groundwater discharge occurred during the Pleistocene.
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