Abstract Details

CAMP CENTURY SUBGLACIAL SEDIMENT PRESERVES EVIDENCE FOR DEGLACIATION OF NORTHWESTERN GREENLAND DURING MIS 11: IMPLICATIONS FOR PALEO-SEA LEVEL

CHRIST, Andrew1, RITTENOUR, Tammy M.2, BIERMAN, Paul R.3, SCHAEFER, Joerg M.4, KNUTZ, Paul C.5, THOMSEN, Tonny B.5, KEULEN, Nynke5, FOSDICK, Julie6, HEMMING, Sidney4 and KEISLING, Benjamin4, (1)Gund Institute for Environment, University of Vermont, Burlington, VT 05405; Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT 05405, (2)Department of Geosciences, Utah State University, 4505 Old Main Hill, Logan, UT 84322, (3)Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT 05405; Gund Institute for Environment, University of Vermont, Burlington, VT 05405, (4)Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, (5)Geological Survey of Denmark and Greenland, Ă˜ster Voldgade 10, Copenhagen, 1350, Denmark, (6)Department of Geosciences, Storrs, CT 06269-0001