TY - JOUR
T1 - New in situ 14C data indicate the absence of nunataks in west Greenland during the Last Glacial Maximum
AU - Graham, Brandon L.
AU - Briner, Jason P.
AU - Schweinsberg, Avriel D.
AU - Lifton, Nathaniel A.
AU - Bennike, Ole
N1 - Funding Information:
We would like to thank CH2M Hill Polar Field services for logistical support and the United States 109th Air Lift Wing Air National Guard. We thank Casey Beel, Alia Lesnek, and Christopher Sbarra for assistance in the laboratory. This manuscript was improved by the efforts of two anonymous reviewers. This research was supported by National Science Foundation grant ARC-1204005.
Funding Information:
We would like to thank CH2M Hill Polar Field services for logistical support and the United States 109th Air Lift Wing Air National Guard. We thank Casey Beel, Alia Lesnek, and Christopher Sbarra for assistance in the laboratory. This manuscript was improved by the efforts of two anonymous reviewers. This research was supported by National Science Foundation grant ARC-1204005 .
Publisher Copyright:
© 2019 Elsevier Ltd
PY - 2019/12/1
Y1 - 2019/12/1
N2 - In situ cosmogenic nuclide exposure age distributions on Ice Age nunataks act as past ice thickness indicators and provide valuable targets for ice sheet model simulations of the Last Glacial Maximum. Several locations along West Greenland have been identified as being potential nunataks due to their weathered nature and their high cosmogenic nuclide inventories with little evidence for ice sheet burial. We present new in situ cosmogenic 14C measurements from four high elevation surfaces in the central Uummannaq Fjord system that were identified as potential nunataks in prior work. Building on previous work, we model cosmogenic radionuclide production and decay, and consider a range of ice sheet history scenarios. Since our results require more burial or shielding under ice than what independent methods suggest for Holocene ice cap cover, we propose that these locations were not nunataks during the Last Glacial Maximum, but rather were buried during the peak of the Last Glacial Maximum. However, we cannot confirm whether these sites were buried by the Greenland Ice Sheet or local glaciers.
AB - In situ cosmogenic nuclide exposure age distributions on Ice Age nunataks act as past ice thickness indicators and provide valuable targets for ice sheet model simulations of the Last Glacial Maximum. Several locations along West Greenland have been identified as being potential nunataks due to their weathered nature and their high cosmogenic nuclide inventories with little evidence for ice sheet burial. We present new in situ cosmogenic 14C measurements from four high elevation surfaces in the central Uummannaq Fjord system that were identified as potential nunataks in prior work. Building on previous work, we model cosmogenic radionuclide production and decay, and consider a range of ice sheet history scenarios. Since our results require more burial or shielding under ice than what independent methods suggest for Holocene ice cap cover, we propose that these locations were not nunataks during the Last Glacial Maximum, but rather were buried during the peak of the Last Glacial Maximum. However, we cannot confirm whether these sites were buried by the Greenland Ice Sheet or local glaciers.
KW - Cosmogenic in situ C
KW - Greenland
KW - Holocene
KW - Modelling
KW - Neoglaciation
KW - Pleistocene
UR - http://www.scopus.com/inward/record.url?scp=85073208668&partnerID=8YFLogxK
U2 - 10.1016/j.quascirev.2019.105981
DO - 10.1016/j.quascirev.2019.105981
M3 - Article
SN - 0277-3791
VL - 225
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
M1 - 105981
ER -