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      Interhemispheric Climate Linkages 

      Full and Late Glacial Lake Records Along the PEP 1 Transect

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          Interhemispheric correlation of late pleistocene glacial events.

          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 >/=33,500 carbon-14 years before present ((14)C 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(14)C 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(14)C yr B.P., and at the beginning of the Younger Dryas at 11,050 (14)C 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.
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            Chronology of expansion and contraction of four great Basin lake systems during the past 35,000 years

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              Upper quaternary vegetational and climatic sequence of the fuquene area (Eastern Cordillera, Colombia)

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                Author and book information

                Book Chapter
                2001
                : 265-291
                10.1016/B978-012472670-3/50019-7
                076a9f02-fea3-448d-9a82-0ffdc790eb9e
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