Stable Isotope Fractionation of γ-Hexachlorocyclohexane (Lindane) during Reductive Dechlorination by Two Strains of Sulfate-Reducing Bacteria

2009 ◽  
Vol 43 (9) ◽  
pp. 3155-3161 ◽  
Author(s):  
Silviu-Laurentiu Badea ◽  
Carsten Vogt ◽  
Stefanie Weber ◽  
Andrei-Florin Danet ◽  
Hans-Hermann Richnow
Keyword(s):  
Stable Isotope ◽  
Reductive Dechlorination ◽  
Isotope Fractionation ◽  
Sulfate Reducing Bacteria ◽  
Sulfate Reducing ◽  
Stable Isotope Fractionation ◽  
Reducing Bacteria

scholarly journals Stable Isotope Fractionation of Tetrachloroethene during Reductive Dechlorination by Sulfurospirillum multivorans and Desulfitobacterium sp. Strain PCE-S and Abiotic Reactions with Cyanocobalamin

2005 ◽  
Vol 71 (7) ◽  
pp. 3413-3419 ◽  
Author(s):  
Ivonne Nijenhuis ◽  
Janet Andert ◽  
Kirsten Beck ◽  
Matthias Kästner ◽  
Gabriele Diekert ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Reductive Dechlorination ◽  
Isotope Fractionation ◽  
Field Application ◽  
Carbon Stable Isotope ◽  
Cell Integrity ◽  
Whole Cells ◽  
Stable Isotope Fractionation ◽  
Crude Extracts ◽  
Order Of Magnitude

ABSTRACT Carbon stable isotope fractionation of tetrachloroethene (PCE) during reductive dechlorination by whole cells and crude extracts of Sulfurospirillum multivorans and Desulfitobacterium sp. strain PCE-S and the abiotic reaction with cyanocobalamin (vitamin B12) was studied. Fractionation was largest during the reaction with cyanocobalamin with αC = 1.0132. Stable isotope fractionation was lower but still in a similar order of magnitude for Desulfitobacterium sp. PCE-S (αC = 1.0052 to 1.0098). The isotope fractionation of PCE during dehalogenation by S. multivorans was lower by 1 order of magnitude (αC = 1.00042 to 1.0017). Additionally, an increase in isotope fractionation was observed with a decrease in cell integrity for both strains. For Desulfitobacterium sp. strain PCE-S, the carbon stable isotope fractionation factors were 1.0052 and 1.0089 for growing cells and crude extracts, respectively. For S. multivorans, αC values were 1.00042, 1.00097, and 1.0017 for growing cells, crude extracts, and the purified PCE reductive dehalogenase, respectively. For the field application of stable isotope fractionation, care is needed as fractionation may vary by more than an order of magnitude depending on the bacteria present, responsible for degradation.

Sulfur isotope fractionation during growth of sulfate-reducing bacteria on various carbon sources

2004 ◽  
Vol 68 (23) ◽  
pp. 4891-4904 ◽  
Author(s):  
Jutta Kleikemper ◽  
Martin H. Schroth ◽  
Stefano M. Bernasconi ◽  
Benjamin Brunner ◽  
Josef Zeyer
Keyword(s):  
Isotope Fractionation ◽  
Sulfur Isotope ◽  
Carbon Sources ◽  
Sulfate Reducing Bacteria ◽  
Sulfate Reducing ◽  
Sulfur Isotope Fractionation ◽  
Reducing Bacteria

scholarly journals Stable Carbon Isotope Fractionation by Sulfate-Reducing Bacteria

2003 ◽  
Vol 69 (5) ◽  
pp. 2942-2949 ◽  
Author(s):  
Kathleen L. Londry ◽  
David J. Des Marais
Keyword(s):  
Carbon Isotope ◽  
Isotope Fractionation ◽  
Carbon Isotope Discrimination ◽  
Stable Carbon Isotope ◽  
Reducing Power ◽  
Sulfate Reducing Bacteria ◽  
Organic Substrates ◽  
Isotope Discrimination ◽  
Sulfate Reducing ◽  
Reducing Bacteria

ABSTRACT Biogeochemical transformations occurring in the anoxic zones of stratified sedimentary microbial communities can profoundly influence the isotopic and organic signatures preserved in the fossil record. Accordingly, we have determined carbon isotope discrimination that is associated with both heterotrophic and lithotrophic growth of pure cultures of sulfate-reducing bacteria (SRB). For heterotrophic-growth experiments, substrate consumption was monitored to completion. Sealed vessels containing SRB cultures were harvested at different time intervals, and δ13C values were determined for gaseous CO2, organic substrates, and products such as biomass. For three of the four SRB, carbon isotope effects between the substrates, acetate or lactate and CO2, and the cell biomass were small, ranging from 0 to 2‰. However, for Desulfotomaculum acetoxidans, the carbon incorporated into biomass was isotopically heavier than the available substrates by 8 to 9‰. SRB grown lithoautotrophically consumed less than 3% of the available CO2 and exhibited substantial discrimination (calculated as isotope fractionation factors [α]), as follows: for Desulfobacterium autotrophicum, α values ranged from 1.0100 to 1.0123; for Desulfobacter hydrogenophilus, the α value was 0.0138, and for Desulfotomaculum acetoxidans, the α value was 1.0310. Mixotrophic growth of Desulfovibrio desulfuricans on acetate and CO2 resulted in biomass with a δ13C composition intermediate to that of the substrates. The extent of fractionation depended on which enzymatic pathways were used, the direction in which the pathways operated, and the growth rate, but fractionation was not dependent on the growth phase. To the extent that environmental conditions affect the availability of organic substrates (e.g., acetate) and reducing power (e.g., H2), ecological forces can also influence carbon isotope discrimination by SRB.

The effect of temperature on sulfur and oxygen isotope fractionation by sulfate reducing bacteria (Desulfococcus multivorans)

2020 ◽  
Vol 367 (9) ◽  
Author(s):  
André Pellerin ◽  
Gilad Antler ◽  
Angeliki Marietou ◽  
Alexandra V Turchyn ◽  
Bo Barker Jørgensen
Keyword(s):  
Sulfate Reduction ◽  
Oxygen Isotope ◽  
Isotope Fractionation ◽  
Sulfur Isotope ◽  
Sulfate Reducing Bacteria ◽  
Oxygen Isotope Fractionation ◽  
Sulfate Reducing ◽  
Sulfur Isotope Fractionation ◽  
Reducing Bacteria ◽  
Desulfococcus Multivorans

ABSTRACT Temperature influences microbiological growth and catabolic rates. Between 15 and 35 °C the growth rate and cell specific sulfate reduction rate of the sulfate reducing bacterium Desulfococcus multivorans increased with temperature. Sulfur isotope fractionation during sulfate reduction decreased with increasing temperature from 27.2 ‰ at 15 °C to 18.8 ‰ at 35 °C which is consistent with a decreasing reversibility of the metabolic pathway as the catabolic rate increases. Oxygen isotope fractionation, in contrast, decreased between 15 and 25 °C and then increased again between 25 and 35 °C, suggesting increasing reversibility in the first steps of the sulfate reducing pathway at higher temperatures. This points to a decoupling in the reversibility of sulfate reduction between the steps from the uptake of sulfate into the cell to the formation of sulfite, relative to the whole pathway from sulfate to sulfide. This observation is consistent with observations of increasing sulfur isotope fractionation when sulfate reducing bacteria are living near their upper temperature limit. The oxygen isotope decoupling may be a first signal of changing physiology as the bacteria cope with higher temperatures.

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