Ronald Oremland (Former Employee)
Science and Products
Filter Total Items: 120
Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation
Methyl fluoride (MF) and dimethyl ether (DME) were effective inhibitors of aerobic methanotrophy in a variety of soils. MF and DME blocked consumption of CH4 as well as the oxidation of 14CH4 to 14CO2, but neither MF nor DME affected the oxidation of [14C]methanol or [14C]formate to 14CO2. Cooxidation of ethane and propane by methane-oxidizing soils was also inhibited by MF...
Authors
Ronald Oremland, Charles Culbertson
Measurement of in situ rates of selenate removal by dissimilatory bacterial reduction in sediments Measurement of in situ rates of selenate removal by dissimilatory bacterial reduction in sediments
A radioisotope method for measurement of bacteria respiratory reduction of selenate to elemental selenium in aquatic sediments was devised. Sediments were labeled with [75Se]selenate, incubated, and washed, and 75Se0(s) was determined as counts remaining in the sediments. Core profiles of selenate reduction, sulfate reduction, and denitrification were made simultaneously in the sediments...
Authors
Ronald Oremland, Nisan Steinberg, Ann Maest, Laurence G. Miller, James T. Hollibaugh
Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration
Interstitial water profiles of SeO42−, SeO32−, SO42−, and Cl− in anoxic sediments indicated removal of the seleno-oxyanions by a near-surface process unrelated to sulfate reduction. In sediment slurry experiments, a complete reductive removal of SeO42− occurred under anaerobic conditions, was more rapid with H2 or acetate, and was inhibited by O2, NO3−, MnO2, or autoclaving but not by...
Authors
Ronald Oremland, James T. Hollibaugh, Ann Maest, Theresa Presser, Laurence G. Miller, Charles Culbertson
Methanogenesis in hypersaline environments Methanogenesis in hypersaline environments
No abstract available.
Authors
Ronald Oremland, G.M. King
Description of an estuarine methylotrophic methanogen, which grows on dimethyl sulfite Description of an estuarine methylotrophic methanogen, which grows on dimethyl sulfite
Characteristics of an obligately methylotrophic coccoid methanogen (strain GS-16) previously isolated from estuarine sediment are described. Growth was demonstrated on dimethyl sulfide (DMS) or trimethylamine (TMA), but not on methane thiol, methane thiol plus hydrogen, dimethyl disulfide, or methionine. DMS-grown cells were able to metabolize DMS and TMA simultaneously when inoculated...
Authors
Ronald Oremland, Ronald Kiene, Indra Mathrani, Michael Whiticar, David Boone
The biogeochemistry of methanogenic bacteria The biogeochemistry of methanogenic bacteria
No abstract available.
Authors
Ronald Oremland
Use of "specific" inhibitors in biogeochemistry and microbial ecology Use of "specific" inhibitors in biogeochemistry and microbial ecology
The above statement, although meant to be tongue in cheek, contains an essential truism: all work with inhibitors is inherently suspect. This fact has been known by biochemists for some time. However, use of chemical inhibitors of enzymic systems and membranes continues to be a common approach taken toward unraveling the biochemistry and biophysics of plants, animals, and microorganisms...
Authors
Ronald Oremland, D.G. Capone
Big Soda Lake (Nevada). 2. Pelagic sulfate reduction Big Soda Lake (Nevada). 2. Pelagic sulfate reduction
The epilimnion of hypersaline, alkaline, meromictic Big Soda Lake contains an average 58 mmol sulfate liter−1 and 0.4 µmol dissolved iron liter−1. The monimolimnion, which is permanently anoxic, has a sulfide concentration ranging seasonally from 4 to 7 mmol liter−1. Depth profiles of sulfate reduction in the monimolimnion, assayed with a 35S tracer technique and in situ incubations...
Authors
Richard Smith, Ronald Oremland
Big Soda Lake (Nevada). 3. Pelagic methanogenesis and anaerobic methane oxidation Big Soda Lake (Nevada). 3. Pelagic methanogenesis and anaerobic methane oxidation
In situ rates of methanogenesis and methane oxidation were measured in meromictic Big Soda Lake. Methane production was measured by the accumulation of methane in the headspaces of anaerobically sealed water samples; radiotracer was used to follow methane oxidation. Nearly all the methane oxidation occurred in the anoxic zones of the lake. Rates of anaerobic oxidation exceeded production...
Authors
Niels Iversen, Ronald Oremland, Michael Klug
Reduction of selenate to selenide by sulfate-respiring bacteria: Experiments with cell suspensions and estuarine sediments Reduction of selenate to selenide by sulfate-respiring bacteria: Experiments with cell suspensions and estuarine sediments
Washed cell suspensions of Desulfovibrio desulfuricans subsp. aestuarii were capable of reducing nanomolar levels of selenate to selenide as well as sulfate to sulfide. Reduction of these species was inhibited by 1 mM selenate or tungstate. The addition of 1 mM sulfate decreased the reduction of selenate and enhanced the reduction of sulfate. Increasing concentrations of sulfate...
Authors
J.P. Zehr, Ronald Oremland
Sources and flux of natural gases from Mono Lake, California Sources and flux of natural gases from Mono Lake, California
The ability to identify a formation mechanism for natural gas in a particular environment requires consideration of several geochemical factors when there are multiple sources present. Four primary sources of methane have been identified in Mono Lake. Two of these sources were associated with numerous natural gas seeps which occur at various locations in the lake and extend beyond its...
Authors
Ronald Oremland, L.G. Miller, Michael Whiticar
Science and Products
Filter Total Items: 120
Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation Evaluation of methyl fluoride and dimethyl ether as inhibitors of aerobic methane oxidation
Methyl fluoride (MF) and dimethyl ether (DME) were effective inhibitors of aerobic methanotrophy in a variety of soils. MF and DME blocked consumption of CH4 as well as the oxidation of 14CH4 to 14CO2, but neither MF nor DME affected the oxidation of [14C]methanol or [14C]formate to 14CO2. Cooxidation of ethane and propane by methane-oxidizing soils was also inhibited by MF...
Authors
Ronald Oremland, Charles Culbertson
Measurement of in situ rates of selenate removal by dissimilatory bacterial reduction in sediments Measurement of in situ rates of selenate removal by dissimilatory bacterial reduction in sediments
A radioisotope method for measurement of bacteria respiratory reduction of selenate to elemental selenium in aquatic sediments was devised. Sediments were labeled with [75Se]selenate, incubated, and washed, and 75Se0(s) was determined as counts remaining in the sediments. Core profiles of selenate reduction, sulfate reduction, and denitrification were made simultaneously in the sediments...
Authors
Ronald Oremland, Nisan Steinberg, Ann Maest, Laurence G. Miller, James T. Hollibaugh
Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration
Interstitial water profiles of SeO42−, SeO32−, SO42−, and Cl− in anoxic sediments indicated removal of the seleno-oxyanions by a near-surface process unrelated to sulfate reduction. In sediment slurry experiments, a complete reductive removal of SeO42− occurred under anaerobic conditions, was more rapid with H2 or acetate, and was inhibited by O2, NO3−, MnO2, or autoclaving but not by...
Authors
Ronald Oremland, James T. Hollibaugh, Ann Maest, Theresa Presser, Laurence G. Miller, Charles Culbertson
Methanogenesis in hypersaline environments Methanogenesis in hypersaline environments
No abstract available.
Authors
Ronald Oremland, G.M. King
Description of an estuarine methylotrophic methanogen, which grows on dimethyl sulfite Description of an estuarine methylotrophic methanogen, which grows on dimethyl sulfite
Characteristics of an obligately methylotrophic coccoid methanogen (strain GS-16) previously isolated from estuarine sediment are described. Growth was demonstrated on dimethyl sulfide (DMS) or trimethylamine (TMA), but not on methane thiol, methane thiol plus hydrogen, dimethyl disulfide, or methionine. DMS-grown cells were able to metabolize DMS and TMA simultaneously when inoculated...
Authors
Ronald Oremland, Ronald Kiene, Indra Mathrani, Michael Whiticar, David Boone
The biogeochemistry of methanogenic bacteria The biogeochemistry of methanogenic bacteria
No abstract available.
Authors
Ronald Oremland
Use of "specific" inhibitors in biogeochemistry and microbial ecology Use of "specific" inhibitors in biogeochemistry and microbial ecology
The above statement, although meant to be tongue in cheek, contains an essential truism: all work with inhibitors is inherently suspect. This fact has been known by biochemists for some time. However, use of chemical inhibitors of enzymic systems and membranes continues to be a common approach taken toward unraveling the biochemistry and biophysics of plants, animals, and microorganisms...
Authors
Ronald Oremland, D.G. Capone
Big Soda Lake (Nevada). 2. Pelagic sulfate reduction Big Soda Lake (Nevada). 2. Pelagic sulfate reduction
The epilimnion of hypersaline, alkaline, meromictic Big Soda Lake contains an average 58 mmol sulfate liter−1 and 0.4 µmol dissolved iron liter−1. The monimolimnion, which is permanently anoxic, has a sulfide concentration ranging seasonally from 4 to 7 mmol liter−1. Depth profiles of sulfate reduction in the monimolimnion, assayed with a 35S tracer technique and in situ incubations...
Authors
Richard Smith, Ronald Oremland
Big Soda Lake (Nevada). 3. Pelagic methanogenesis and anaerobic methane oxidation Big Soda Lake (Nevada). 3. Pelagic methanogenesis and anaerobic methane oxidation
In situ rates of methanogenesis and methane oxidation were measured in meromictic Big Soda Lake. Methane production was measured by the accumulation of methane in the headspaces of anaerobically sealed water samples; radiotracer was used to follow methane oxidation. Nearly all the methane oxidation occurred in the anoxic zones of the lake. Rates of anaerobic oxidation exceeded production...
Authors
Niels Iversen, Ronald Oremland, Michael Klug
Reduction of selenate to selenide by sulfate-respiring bacteria: Experiments with cell suspensions and estuarine sediments Reduction of selenate to selenide by sulfate-respiring bacteria: Experiments with cell suspensions and estuarine sediments
Washed cell suspensions of Desulfovibrio desulfuricans subsp. aestuarii were capable of reducing nanomolar levels of selenate to selenide as well as sulfate to sulfide. Reduction of these species was inhibited by 1 mM selenate or tungstate. The addition of 1 mM sulfate decreased the reduction of selenate and enhanced the reduction of sulfate. Increasing concentrations of sulfate...
Authors
J.P. Zehr, Ronald Oremland
Sources and flux of natural gases from Mono Lake, California Sources and flux of natural gases from Mono Lake, California
The ability to identify a formation mechanism for natural gas in a particular environment requires consideration of several geochemical factors when there are multiple sources present. Four primary sources of methane have been identified in Mono Lake. Two of these sources were associated with numerous natural gas seeps which occur at various locations in the lake and extend beyond its...
Authors
Ronald Oremland, L.G. Miller, Michael Whiticar