Iron and sulfide oxidation within the basaltic ocean crust: implications for chemolithoautotrophic microbial biomass production
- 1 October 2003
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 67 (20) , 3871-3887
- https://doi.org/10.1016/s0016-7037(03)00304-1
Abstract
No abstract availableKeywords
This publication has 109 references indexed in Scilit:
- Geochemistry of hydrothermally altered oceanic crust: DSDP/ODP Hole 504B – Implications for seawater‐crust exchange budgets and Sr‐ and Pb‐isotopic evolution of the mantleGeochemistry, Geophysics, Geosystems, 2003
- Discovery of ancient and active hydrothermal systems along the ultra‐slow spreading Southwest Indian Ridge 10°–16°EGeochemistry, Geophysics, Geosystems, 2002
- Bacterial and thermochemical sulfate reduction in diagenetic settings — old and new insightsSedimentary Geology, 2001
- Regional heat flow variations across the sedimented Juan de Fuca Ridge eastern flank: Constraints on lithospheric cooling and lateral hydrothermal heat transportJournal of Geophysical Research, 1999
- Sulfur in serpentinized oceanic peridotites: Serpentinization processes and microbial sulfate reductionJournal of Geophysical Research, 1998
- The development of direct and indirect methods for the study of the thermodynamics of microbial growthThermochimica Acta, 1998
- Deep subsurface microbial processesReviews of Geophysics, 1995
- Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and CenozoicJournal of Geophysical Research, 1995
- Hydrogen concentrations as an indicator of the predominant terminal electron-accepting reactions in aquatic sedimentsGeochimica et Cosmochimica Acta, 1988
- The heat flow through oceanic and continental crust and the heat loss of the EarthReviews of Geophysics, 1980