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A 30,000 yr Continental Paleotemperature Record Derived from Noble Gases Dissolved in Groundwater from the San Juan Basin, New Mexico

Published online by Cambridge University Press:  20 January 2017

Martin Stute ,
Jordan F. Clark ,
Peter Schlosser ,
Wallace S. Broecker  and
Georges Bonani
Martin Stute
Affiliation:
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964
Jordan F. Clark
Affiliation:
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964; and Department of Geological Sciences, Columbia University, New York, New York 10027
Peter Schlosser
Affiliation:
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964; and Department of Geological Sciences, Columbia University, New York, New York 10027
Wallace S. Broecker
Affiliation:
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964; and Department of Geological Sciences, Columbia University, New York, New York 10027
Georges Bonani
Affiliation:
Eidgenössische Technische Hochschule (ETH), Zürich, Institut für Mittelenergiephysik, CH-8093 Zürich, Switzerland
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Abstract

Paleotemperatures for the last glacial maximum (LGM) have been derived from noble gases dissolved in 14C-dated groundwater of the Ojo Alamo and the Nacimiento formations in the San Juan Basin, northwestern New Mexico. The difference in mean annual (ground) temperature between the Holocene and the LGM was determined to be 5.5 ± 0.7°C. A practically identical result, 5.2 ± 0.7°C, has been obtained previously from the Carrizo aquifer in southern Texas. This suggests that the southwestern United States was uniformly cooler during the LGM and that the mean annual temperature gradient along a transect from the Gulf of Mexico to northwestern New Mexico has been unchanged since the LGM. The noble gas paleotemperatures are supported by paleoecological evidence in the region. The Holocene/LGM temperature difference of 5.4°C indicates that a simple lapse rate calculation may be applied to convert the 1000-m glacial depression of snowlines in the Colorado Front Range into a temperature decrease. A continental temperature change of 5.4 ± 0.7°C is inconsistent with a temperature change of about 2°C determined for the surface waters of the Gulf of Mexico.

Type
Research Article
Information
Quaternary Research , Volume 43 , Issue 2 , March 1995 , pp. 209 - 220
Copyright
University of Washington

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