Paleoceanography


The Younger Dryas Event

Interest in the Younger Dryas cooling has increased mainly because it began and ended with large climatic shifts that took place very abruptly, indeed, within a few human life spans [F lohn, 1986]. Understanding global change of this sort is essential because of current concern about rapid, anthropogenically caused climate change.

  1. Special Section: The Younger Dryas Event

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    2. Special Section: The Younger Dryas Event
    1. Deglacial climatic oscillations in the Gulf of California (pages 1009–1023)

      L. D. Keigwin, G. A. Jones

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/PA005i006p01009

    2. Cryosphere/ocean interactions at the margin of the Laurentide Ice Sheet during the Younger Dryas Chron: SE Baffin Shelf, northwest Territories (pages 921–935)

      J. T. Andrews, L. W. Evans, K. M. Williams, W. M. Briggs, A. J. T. Jull, H. Erlenkeuser, I. Hardy

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/PA005i006p00921

    3. The Younger Dryas Cooling Event: An introduction (pages 891–895)

      J. P. Kennett

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/PA005i006p00891

    4. Nutricline variation in the equatorial Atlantic coincident with the Younger Dryas (pages 997–1008)

      Barbara Molfino, Andrew McIntyre

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/PA005i006p00997

    5. The Younger Dryas Cool Episode in the Gulf of Mexico (pages 949–961)

      B. P. Flower, J. P. Kennett

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/PA005i006p00949

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