Reduction of humic substances and Fe(III) by hyperthermophilic microorganisms

By Derek R. Lovley, K. Kashefi, M. Vargas, Jason M. Tor, E. L. Blunt-Harris. 2000

122 citations recorded by the source corpus.

Subfields: Ecology, Environmental Engineering, Geochemistry and Petrology

View Paper: https://www.semanticscholar.org/paper/f919a0f76040a085dcd3821bf19de7a557d9f840

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. A. Kappler
2. N. Posth
3. K. Konhauser

In Environmental Engineering

1. A. Kappler
2. N. Posth
3. K. Konhauser
4. J. Ramsay
5. Y. Luu

In Geochemistry and Petrology

1. K. Konhauser
2. A. Kappler

Citations in the corpus

• Dissimilatory Fe(III) and Mn(IV)-reducing Prokaryotes (2000, unknown): “…FMR that have been evaluated to date, including the hyperthermophiles, have the ability to transfer electrons to humic substances (humics) or other extracellular quinones such as the humics analog, anthraquinone-2,6-disulfonate (AQDS) Lovley et al., 1996; Lovley et al., 1998; Lovley et al. 2000).”
• Review: microbial mechanisms of accessing insoluble Fe(III) as an energy source (2003, background): “Humicreducing bacteria have been recovered from diverse environments (Coates et al. 1998) and include hyperthermophilic (Lovley et al. 2000) and fermenting bacteria (Benz et al. 1998).”
• Microbiological processes in banded iron formation deposition (2013, background): “surface (Lovley et al., 2000).”