INTERHEMISPHERIC CORRELATION OF LATE PLEISTOCENE GLACIAL EVENTS

A radiocarbon chronology shows that piedmont glacier lobes in the Chil ean Andes achieved maxima during the last glaciation at 13,900 to 14,8 90, 21,000, 23,060, 26,940, 29,600, and greater than or equal to 33,50 0 carbon-14 years before present (C-14 yr B.P.) in a cold and wet Suba ntarctic Parkland environment. The last glaciation ended with massive collapse of ice lobes close to 14,000 C-14 yr B.P., accompanied by an influx of North Patagonian Rain Forest species. In the Southern Alps o f New Zealand, additional glacial maxima are registered at 17,720 C-14 yr B.P., and at the beginning of the Younger Dryas at 11,050 C-14 yr B.P. These glacial maxima in mid-latitude mountains rimming the South Pacific were coeval with ice-rafting pulses in the North Atlantic Ocea n. Furthermore, the last termination began suddenly and simultaneously in both polar hemispheres before the resumption of the modern mode of deep-water production in the Nordic Seas. Such interhemispheric coupl ing implies a global atmospheric signal rather than regional climatic changes caused by North Atlantic thermohaline switches or Laurentide i ce surges.