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SULFATE PROFILE MAP
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Sulfate is the most abundant
terminal electron acceptor in sediments deep beneath the seafloor.
Our global SO4-2 map displays the subsurface depths and SO4 -2
concentrations at which downward-diffusing SO 4 -2 stabilizes (circles)
or disappears (diamonds) at ODP sites throughout the world ocean (DHondt
et al., 2002 ). White circles indicate that the SO4-2 stabilizes
above five meters below the seafloor. Please check the details
of the data and methods that went into making this map.
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for more information about this page. Last revised June 2003.