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Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR)

2002; Elsevier BV; Volume: 191; Issue: 4 Linguagem: Inglês

10.1016/s0009-2541(02)00134-1

1872-6836

Jean‐Luc Charlou, Jean Pierre Donval, Yves Fouquet, Philippe Jean‐Baptiste, Nils G. Holm,

Geology and Paleoclimatology Research

The Flores diving cruise was part of the MAST III-AMORES (1995–1998) program funded by the European Union. One of the major achievements of the Flores cruise was the discovery of the Rainbow hydrothermal field hosted in ultramafic rocks south of the Amar segment on the Mid-Atlantic ridge (MAR). The Rainbow hydrothermal fluids exhibit temperatures of 365 °C, pH of 2.8, high chlorinity (750 mmol/kg), and low silica (6.9 mmol/kg). The uniformity in endmember major, minor, trace element concentrations and gas contents suggests that all Rainbow fluids originate from the same deep source. Although H2S content is relatively low (1.20 mmol/kg), all vent fluids show extraordinary high H2 (16 mmol/kg), CH4 (2.5 mmol/kg) and CO (5 μmol/kg) endmember concentrations compared to fluids collected from other vent sites along the MAR. Hydrogen represents more than 40% of the total gas volume extracted from the fluids. At Rainbow, H2 production is likely associated with alteration of olivine and orthopyroxene minerals during serpentinization. Given that exposures of ultramafic rock may be common, particularly along slow-spreading ridges, the production of H2 may have important implications for microbial activity at and beneath the seafloor.