Cool glacial temperatures and changes in moisture source recorded in oman groundwaters
Concentrations of atmospheric noble gases (neon, argon, krypton, and xenon) dissolved in groundwaters from northern Oman indicate that the average ground temperature during the Late Pleistocene (15,000 to 24,000 years before present) was 6.5 degrees +/- 0.6 degrees C lower than that of today. Stable oxygen and hydrogen isotopic groundwater data show that the origin of atmospheric water vapor changed from a primarily southern, Indian Ocean source during the Late Pleistocene to a dominantly northern, Mediterranean source today. The reduced northern water vapor source is consistent with a drier Last Glacial Maximum through much of northern Africa and Arabia.
Weyhenmeyer
CE
Institute of Geology, University of Bern, CH-3012 Bern, Switzerland. Environmental Physics, EAWAG/ETH, CH-8600 Duebendorf, Switzerland. Institute of Physics, University of Bern, CH-3012 Bern, Switzerland.
Burns
SJ
Waber
HN
Aeschbach-Hertig
W
Kipfer
R
Loosli
HH
Matter
A