Late Pleistocene South Atlantic

  • Mulitza S
  • Paul A
  • Wefer G
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The South Atlantic and the Southern Ocean play an important role in the global thermohaline circulation. Paleoceanographic records from South Atlantic sediments indicate that many of the present-day factors, which are critical for the circulation in the South Atlantic, have been affected by late Pleistocene climatic changes. These include the distribution of sea-surface temperature, upper ocean stratification, freshwater input, sea ice, coastal upwelling, and productivity as well as the intermediate and deep-water circulation. The temporal evolution of late Pleistocene paleoceanographic proxy records suggest that the South Atlantic is an active component of climate change at orbital and millennial timescales.

Author-supplied keywords

  • Agulhas leakage
  • Bipolar Seesaw
  • Central water
  • Coastal upwelling
  • Dansgaard-Oeschger Cycles
  • Deep water
  • Heinrich Event
  • Ice-rafted detritus
  • Intermediate water
  • Intertropical Convergence
  • Last Glacial Maximum
  • Late Pleistocene
  • Meltwater
  • Monsoon
  • Nutrients
  • Precession
  • Precipitation
  • Productivity
  • River runoff
  • SE trade winds
  • Sea ice
  • Sea-surface temperature
  • South Atlantic
  • Southern Ocean
  • Stratification
  • Thermocline
  • Upwelling
  • Ventilation
  • Younger Dryas

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  • S. Mulitza

  • A. Paul

  • G. Wefer

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