Microbial hydrocarbon gases in the Witwatersrand Basin, South Africa: Implications for the deep biosphere
Authors:
- J.A WardJWJ.A Ward
- G.F SlaterGSG.F Slater
- D.P MoserDMD.P Moser
- L.-H LinL.-H Lin
- G Lacrampe-CouloumeGLG Lacrampe-Couloume
- A.S BoninABA.S Bonin
- M DavidsonMDM Davidson
- J.A HallJHJ.A Hall
- B MislowackBMB Mislowack
- R.E.S BellamyRBR.E.S Bellamy
- T.C OnstottT.C Onstott
- B Sherwood LollarBLB Sherwood Lollar
- 1 August 2004
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 68 (15) , 3239-3250
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- Related assemblages of sulphate‐reducing bacteria associated with ultradeep gold mines of South Africa and deep basalt aquifers of Washington StateEnvironmental Microbiology, 2003
- Oil preserved in fluid inclusions in Archaean sandstonesNature, 1998
- Reduction of CO2 during serpentinization of olivine at 300 °C and 500 barGeology, 1996
- Hydrothermal methane venting between 12°N and 26°N along the Mid‐Atlantic RidgeJournal of Geophysical Research, 1993
- Archaea in coastal marine environments.Proceedings of the National Academy of Sciences, 1992
- Geochemistry of reduced gas related to serpentinization of the Zambales ophiolite, PhilippinesApplied Geochemistry, 1990
- Methane-hydrogen gas seeps, Zambales Ophiolite, Philippines: Deep or shallow origin?Chemical Geology, 1988
- Reduction of water with zinc for hydrogen isotope analysisAnalytical Chemistry, 1982
- Molecular carbon isotopic evidence for the origin of geothermal hydrocarbonsNature, 1981
- Isotopic Variations in Meteoric WatersScience, 1961