T176 Isotopic and Elemental Tracers of Late Quaternary Climate Change (Posters)
BA/CA IN NEOGLOBOQUADRINA PACHYDERMA AS AN INDICATOR OF MELTWATER DISCHARGE INTO THE WESTERN ARCTIC OCEAN
Paper number: T176-3
Program: Technical Sessions
Time: 1:30 PM – 5:30 PM
Authors
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Lui-Heung ChanLouisiana State Univ, Baton Rouge, LA
Abstract
Increases in Ba/Ca in N. pachyderma sin. directly correlate with the retreat of the Laurentide Ice Sheet and the evolution of the Mackenzie River drainage basin. Expansion of the Mackenzie River drainage basin due to retreating ice caused an increase in meltwater discharge to the western Arctic Ocean, corresponding to maximum barium concentrations in the Arctic surface water at 11.8 14C ka BP. Increased meltwater discharge may have triggered an increase in the export of freshwater from the Arctic to the North Atlantic surface waters, thus contributing to the onset of the Younger Dryas. The second meltwater event at 9.4 14C ka BP may be the result of glacial Lake Agassiz draining through the Clearwater spillway into the Mackenzie River.