ABRUPT CLIMATE EVENTS 500,000 TO 340,000 YEARS AGO - EVIDENCE FROM SUBPOLAR NORTH-ATLANTIC SEDIMENTS

Subpolar North Atlantic proxy records document millennial-scale climat e variations 500,000 to 340,000 years ago. The cycles have an approxim ately constant pacing that is similar to that documented for the last glacial cycle. These findings suggest that such climate variations are inherent tp the late Pleistocene, regardless of glacial state. Sea su rface temperature during the warm peak of Marine Isotope Stage 11 (MIS 11) varied by 0.5 degrees to 1 degrees C, less than the 4 degrees to 4.5 degrees C estimated during times of ice growth and the 3 degrees C estimated for glacial maxima. Coherent deep ocean circulation changes were associated with glacial oscillations in sea surface temperature.