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Laurence A. Coogan and Kathryn M. Gillis Evidence that low-temperature oceanic hydrothermal systems play an important role in the silicate-carbonate weathering cycle and long-term climate regulation Geochemistry, Geophysics, Geosystems 14

Article first published online: 10 JUN 2013 | DOI: 10.1002/ggge.20113

Key Points

  • Model to investigate secular changes in carbonate precipitation in oceanic crust
  • Changes in alkalinity production by alteration of crust required
  • Seafloor hydrothermal alteration plays important role in C-cycle and climate

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