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North Pacific deglacial hypoxic events linked to abrupt ocean warming

Author

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  • S. K. Praetorius

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
    †Present address: Department of Global Ecology, Carnegie Institution for Science, Stanford, California 94305, USA.)

  • A. C. Mix

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • M. H. Walczak

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • M. D. Wolhowe

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • J. A. Addison

    (US Geological Survey)

  • F. G. Prahl

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

Abstract

The processes responsible for driving the expansion of the ocean's oxygen minimum zones remain uncertain; here sediment core data from the Gulf of Alaska suggest that reduced oxygen solubility was a result of ocean warming initiating the expansion of the North Pacific oxygen minimum zone, leading to increased marine productivity and carbon export and, in turn, further reductions in dissolved oxygen levels.

Suggested Citation

  • S. K. Praetorius & A. C. Mix & M. H. Walczak & M. D. Wolhowe & J. A. Addison & F. G. Prahl, 2015. "North Pacific deglacial hypoxic events linked to abrupt ocean warming," Nature, Nature, vol. 527(7578), pages 362-366, November.
    • Handle: RePEc:nat:nature:v:527:y:2015:i:7578:d:10.1038_nature15753
    DOI: 10.1038/nature15753
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