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      Geomicrobiology of Manganese

      edited_book
      CRC Press

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          Chemistry of submarine hydrothermal solutions at 21 °N, East Pacific Rise

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            Chemistry of Pacific pelagic sediments

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              Geomicrobiology of deep-sea hydrothermal vents.

              During the cycling of seawater through the earth's crust along the mid-ocean ridge system, geothermal energy is transferred into chemical energy in the form of reduced inorganic compounds. These compounds are derived from the reaction of seawater with crustal rocks at high temperatures and are emitted from warm (
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                Book Chapter
                April 12 2002
                December 03 2009
                : 429-528
                10.1201/9780824744458.ch16
                caf4e460-50bf-4293-abf7-8cd556f6b9b3
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