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Laurence G. Miller

Researcher at United States Geological Survey

Publications -  61
Citations -  4048

Laurence G. Miller is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Water column & Anaerobic oxidation of methane. The author has an hindex of 32, co-authored 61 publications receiving 3816 citations. Previous affiliations of Laurence G. Miller include Duquesne University & University of California, Santa Cruz.

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Selenate Reduction to Elemental Selenium by Anaerobic Bacteria in Sediments and Culture: Biogeochemical Significance of a Novel, Sulfate-Independent Respiration

TL;DR: Results indicate that dissimilatory selenate reduction to elemental selenium is the major sink for selenia oxyanions in anoxic sediments and suggest application as a treatment process for removing selenio-oxyanions from wastewaters and also offer an explanation for the presence of selenite in oxic waters.
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Metabolism of reduced methylated sulfur compounds in anaerobic sediments and by a pure culture of an estuarine methanogen.

TL;DR: The results indicate the methanogens and sulfate reducers compete for DMS when it is present at low concentrations; however, at high concentrations, DMS is a "noncompetitive" substrate for methanogenesis.
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Isolation, Growth, and Metabolism of an Obligately Anaerobic, Selenate-Respiring Bacterium, Strain SES-3

TL;DR: Results suggest that reduction of selenite to Se may proceed, in part, by some of the components of a dissimilatory system for sulfur oxyanions.
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Arsenic(III) fuels anoxygenic photosynthesis in hot spring biofilms from Mono Lake, California.

TL;DR: Phylogenetic analysis indicates that microbial arsenic metabolism is ancient and probably extends back to the primordial Earth, and production of As(V) by anoxygenic photosynthesis probably opened niches forPrimordial Earth's first As( V)-respiring prokaryotes.
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Benthic fluxes in San Francisco Bay

TL;DR: In this paper, benthic fluxes have been measured at a channel station and a shoal station in South San Francisco Bay, using in situ flux chambers, and measurements of easily measured substances such as radon, oxygen, ammonia, and silica showed a variability (± 1σ) of 30% or more over distances of a few meters to tens of meters.