Neutrophilic Fe-Oxidizing Bacteria Are Abundant at the Loihi Seamount Hydrothermal Vents and Play a Major Role in Fe Oxide Deposition
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Open Access
- 1 June 2002
- journal article
- Published by American Society for Microbiology in Applied and Environmental Microbiology
- Vol. 68 (6) , 3085-3093
- https://doi.org/10.1128/aem.68.6.3085-3093.2002
Abstract
A number of hydrothermal vent sites exist on the summit of the Loihi Seamount, a shield volcano that is part of the Hawaiian archipelago. The vents are 1,100 to 1,325 m below the surface and range in temperature from slightly above ambient (10°C) to high temperature (167°C). The vent fluid is characterized by high concentrations of CO 2 (up to 17 mM) and Fe(II) (up to 268 μM), but there is a general paucity of H 2 S. Most of the vents are surrounded by microbial mats that have a gelatinous texture and are heavily encrusted with rust-colored Fe oxides. Visually, the Fe oxides appeared homogeneous. However, light microscopy revealed that the oxides had different morphologies, which fell into three classes: (i) sheaths, (ii) twisted or irregular filaments, and (iii) amorphous oxides. A morphological analysis of eight different samples indicated that the amorphous oxides were overall the most abundant; however, five sites had >50% sheaths and filamentous oxides. These latter morphologies are most likely the direct result of microbial deposition. Direct cell counts revealed that all of the oxides had abundant microbial populations associated with them, from 6.9 × 10 7 to 5.3 × 10 8 cells per ml of mat material. At most sites, end point dilution series for lithotrophic Fe oxidizers were successful out to dilutions of 10 −6 and 10 −7 . A pure culture was obtained from a 10 −7 dilution tube; this strain, JV-1, was an obligate, microaerophilic Fe oxidizer that grew at 25 to 30°C. A non-cultivation-based molecular approach with terminal-restriction fragment length polymorphism also indicated the common presence of Fe-oxidizing bacteria at Loihi. Together, these results indicate that Fe-oxidizing bacteria are common at the Loihi Seamount and probably play a major role in Fe oxidation. A review of the literature suggests that microbially mediated Fe oxidation at hydrothermal vents may be important globally.Keywords
This publication has 53 references indexed in Scilit:
- Suboxic Deposition of Ferric Iron by Bacteria in Opposing Gradients of Fe(II) and Oxygen at Circumneutral pHApplied and Environmental Microbiology, 2001
- Iron bacterial and fungal mats, Bajocian stratotype (Mid-Jurassic, northern Normandy, France)Sedimentary Geology, 2000
- Continuous sampling of hydrothermal fluids from Loihi Seamount after the 1996 eventJournal of Geophysical Research, 2000
- Early Jurassic hydrothermal vent community from the Franciscan Complex, San Rafael Mountains, CaliforniaGeology, 1999
- Carbonate precipitation into alkaline silica-rich environmentsGeology, 1998
- Low-temperature hydrothermal deposits of Franklin Seamount, Woodlark Basin, Papua New GuineaMarine Geology, 1997
- Researchers rapidly respond to submarine activity at Loihi Volcano, HawaiiEos, 1997
- Comparative mineralogy and geochemistry of hydrothermal iron‐rich crusts from the Pitcairn, Teahitia‐mehetia, and Macdonald hot spot areas of the S. W. pacificMarine Georesources & Geotechnology, 1993
- Microbial involvement in the formation of Cambrian sea-floor silica-iron oxide deposits, AustraliaGeology, 1992
- Autotrophic and mixotrophic growth of Gallionella ferrugineaJournal of General Microbiology, 1991