INTERHEMISPHERIC CORRELATION OF LATE PLEISTOCENE GLACIAL EVENTS

LOWELL, TV; HEUSSER, CJ; ANDERSEN, BG; MORENO, PI; HAUSER, A; HEUSSER, LE; SCHLUCHTER, C; MARCHANT, DR; DENTON, GH

Abstract

A radiocarbon chronology shows that piedmont glacier lobes in the Chilean Andes achieved maxima during the last glaciation at 13,900 to 14,890, 21,000, 23,060, 26,940, 29,600, and greater than or equal to 33,500 carbon-14 years before present (C-14 yr B.P.) in a cold and wet Subantarctic 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 of 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 Ocean. 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 coupling implies a global atmospheric signal rather than regional climatic changes caused by North Atlantic thermohaline switches or Laurentide ice surges.

Más información

Título según WOS: ID WOS:A1995RU81300031 Not found in local WOS DB
Título de la Revista: SCIENCE
Volumen: 269
Número: 5230
Editorial: AMER ASSOC ADVANCEMENT SCIENCE
Fecha de publicación: 1995
Página de inicio: 1541
Página final: 1549
DOI:

10.1126/science.269.5230.1541

Notas: ISI