Paleoceanography


Sediment Waves and Sediment Drifts: Monitors of Global Changes in Deepwater Circulation

The purpose of this special section in Paleoceanography is to present interdisciplinary approaches for contributing to the reconstruction of ocean circulation and its response to climate changes. A high-priority objective for understanding the causes and mechanisms of climate change is the monitoring of past ocean circulation and oceanic heat and nutrient transport.


  1. Special Section Sediment Waves and Sediment Drifts: Monitors of Global Changes in Deepwater Circulation

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    2. Special Section Sediment Waves and Sediment Drifts: Monitors of Global Changes in Deepwater Circulation
    1. A 600,000-year record of Antarctic Bottom Water activity inferred from sediment textures and structures in a sediment core from the Southern Brazil Basin (pages 1017–1026)

      Laurent Massé, Jean-Claude Faugères, Michel Bernat, Annick Pujos, Marie-Laure Mézerais

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/94PA01442

    2. Abyssal sediment waves in the Gulf of Mexico: An enigma (pages 1087–1094)

      E. William Behrens

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/94PA01445

    3. Late Cenozoic sediment drift complex, northeast Rockall Trough, North Atlantic (pages 989–999)

      J. A. Howe, M. S. Stoker, D. A. V. Stow

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/94PA01440

    4. Modeling sediment drifts: A coupled oceanic circulation-sedimentation model of the northern North Atlantic (pages 897–916)

      Bernd J. Haupt, Christian Schäfer-Neth, Karl Stattegger

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/94PA01437

    5. Mudwaves on the Gardar sediment drift, NE Atlantic (pages 973–988)

      Patricia L. Manley, David W. Caress

      Version of Record online: 4 MAY 2010 | DOI: 10.1029/94PA01755

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