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1.
A method is described for the assay of [35S]sulfate reduction in which filter paper wicks are used to trap [35S]sulfide. The simplicity of the technique enables large numbers of samples to be conveniently processed. Enhanced sensitivity is achieved since all acid-volatile [35S]sulfides produced during the incubation period are counted. Recovery of radioactivity from added Na235S is excellent (mean, 100.1%; standard deviation, 1.81; n = 9) and is unaffected by sulfide concentrations of up to 400 μg per sample. Field trial results with anoxic sediment samples are presented. 相似文献
2.
B. Eickmann I. H. Thorseth M. Peters H. Strauss M. Bröcker R. B. Pedersen 《Geobiology》2014,12(4):308-321
Barite chimneys are known to form in hydrothermal systems where barium‐enriched fluids generated by leaching of the oceanic basement are discharged and react with seawater sulfate. They also form at cold seeps along continental margins, where marine (or pelagic) barite in the sediments is remobilized because of subseafloor microbial sulfate reduction. We test the possibility of using multiple sulfur isotopes (δ34S, Δ33S, ?36S) of barite to identify microbial sulfate reduction in a hydrothermal system. In addition to multiple sulfur isotopes, we present oxygen (δ18O) and strontium (87Sr/86Sr) isotopes for one of numerous barite chimneys in a low‐temperature (~20 °C) venting area of the Loki's Castle black smoker field at the ultraslow‐spreading Arctic Mid‐Ocean Ridge (AMOR). The chemistry of the venting fluids in the barite field identifies a contribution of at least 10% of high‐temperature black smoker fluid, which is corroborated by 87Sr/86Sr ratios in the barite chimney that are less radiogenic than in seawater. In contrast, oxygen and multiple sulfur isotopes indicate that the fluid from which the barite precipitated contained residual sulfate that was affected by microbial sulfate reduction. A sulfate reduction zone at this site is further supported by the multiple sulfur isotopic composition of framboidal pyrite in the flow channel of the barite chimney and in the hydrothermal sediments in the barite field, as well as by low SO4 and elevated H2S concentrations in the venting fluids compared with conservative mixing values. We suggest that the mixing of ascending H2‐ and CH4‐rich high‐temperature fluids with percolating seawater fuels microbial sulfate reduction, which is subsequently recorded by barite formed at the seafloor in areas where the flow rate is sufficient. Thus, low‐temperature precipitates in hydrothermal systems are promising sites to explore the interactions between the geosphere and biosphere in order to evaluate the microbial impact on these systems. 相似文献
3.
Two methods are described for the assay of sulfotransferases which are active with sulfate acceptors bearing the hydroxyl functional group. Assays were developed for enzymes which transfer sulfate from 3′-phosphoadenosine–5′-phosphosulfate (PAPS) to sterols, phenols, and simple alcohols thereby forming the corresponding sulfate esters. With a filter binding assay, useful with crude and purified enzyme preparations, a radioactive sterol substrate is used and subsequently separated from labeled product, allowing the determination of between 50 and 400 pmol of product. In a second method, [35S]PAPS is used and the labeled product is separated from PAPS and inorganic sulfate by a thin-layer technique in which product migrates close to the solvent front; the assay is useful with a broad array of substrates and is more sensitive than the filter binding assay. 相似文献
4.
A new assay for phospholipase C activity that uses alkaline phosphatase to convert phosphorylcholine to inorganic phosphate is described. The determination of inorganic phosphate is performed in the presence of phosphatidylcholine and protein after the addition of sodium dodecyl sulfate. Phospholipase C activity determined by this coupled enzyme assay agrees well with data obtained by extracting and measuring phosphoryl[14C]choline produced from phosphatidyl[methyl-14C]choline. The assay is sensitive to 1 nmol of phosphate, requires no removal of protein or phospholipid, and will work with a variety of phospholipid substrates. The assay is faster and more sensitive than previously published procedures. Stimulation of phospholipase C from Clostridium perfringens by ammonium sulfate is also reported. 相似文献
5.
An integrated field and laboratory study was conducted to quantify the effect of environmental determinants on the activity of sulfate reducers in a freshwater aquifer contaminated with petroleum hydrocarbons (PHC). Within the contaminated zone, PHC-supported in␣situ sulfate reduction rates varied from 11.58±3.12 to 636±53 nmol cm−3 d−1 and a linear increase (R
2=0.98) in reduction rate was observed with increasing in situ sulfate concentrations suggesting sulfate limitation. Half-saturation concentration (K
s) for sulfate reduction coupled to PHC mineralization was determined for the first time. At two different sites within the␣aquifer, maximum sulfate reduction rate under␣non-limiting conditions (R
max) was 5,000 nmol cm−3 d−1, whereas the retrieved K
s values were 3.5 and 7.5 mM, respectively. The K
s values are the highest ever reported from a natural environment. Furthermore, the K
s values were significantly higher than in situ sulfate concentrations confirming sulfate limited growth. On addition of lactate and formate, sulfate reduction rate increased indicating that reactivity and bioavailability of organic substrate may also have played a role in rate inhibition in certain parts of the aquifer. Experiments with sulfide amendments show statistically minor decrease in sulfate reduction rates on addition of sulfide and analogous increase in sulfide toxicity with increasing sulfide concentrations (0.5–10 mM) was not apparent. 相似文献
6.
The electron spin resonance (ESR) lines of nitroxide spin labels are broadened by electron spin exchange reactions that take place during collisions with paramagnetic ions. The degree of line broadening is greatly reduced when the paramagnetic ion forms a coordination bond with certain functional groups on organic molecules. These observations form the basis for a spin-label assay for metal ion chelation and complex formation. This paper describes the characteristics of such an assay for divalent nickel ions and the spin label TEMPONE (2,2,6,6-tetramethylpiperidone-N-oxyl). The chelation of Ni2+ by cysteine and the interaction of Ni2+ with sodium dodecyl sulfate micelles and phospholipid vesicles are demonstrated. In addition to monitoring interactions of paramagnetic ions, the assay also allows the detection of interactions of nonparamagnetic ions that compete with the paramagnetic ions for binding sites. A kinetic analysis of competition between Ni2+ and Zn2+ ions for binding sites on phospholipid vesicles is presented. There are several advantages of the spin-label line-broadening assay compared to other conventional assays for metal chelation and complex formation. The line-broadening assay does not require that the sample be optically clear or chemically defined, it requires only very small quantities of material, it can detect as little as 0.4 to 1 μmol of complexing agent, and it may be utilized in complex biological systems including subcellular organelles and macromolecules. 相似文献
7.
Sulfate-reducing bacteria (SRB) are thought to be actively involved in the cycling of sulfur in acidic mine tailings. However, most studies have used circumstantial evidence to assess microbial sulfate activity in such environments. In order to fully ascertain the role of sulfate-reducing bacteria (SRB) in sulfur cycling in acidic mine tailings, we measured sulfate reduction rates, sulfur isotopic composition of reduced sulfide fractions, porewaters and solid-phase geochemistry and SRB populations in four different Cu-Zn tailings located in Timmins, Ontario, Canada. The tailings were sampled in the summer and in the spring, shortly after snowmelt. The results first indicate that all four sites showed very high sulfate reduction rates in the summer (~100–1000 nmol cm? 3d?1), which corresponded to the presence of sulfide in the porewaters and to high SRB populations. In some of the sites, zones of microbial sulfate reduction also corresponded to a decline of organic carbon and to an apparent pyrite (with slightly negative δ34S values) enrichment around the same depth. Microbial sulfate reduction was also important in permanently acidic (pH 2–3) mine tailings sites, suggesting that SRB can be active under very acidic conditions. Secondly, the results showed that microbial sulfate reduction was greatly reduced in the spring, suggesting that temperature might be a key factor in the activity of SRB. However, a closer look at the results indicated that temperature was not the sole factor and that acidic conditions and limited substrate availability in the spring appeared to be important as well in limiting microbial sulfate par reduction in sulfidic mine tailings. Finally, the results indicate that sulfur undergoes rapid cycling throughout the year and that microbial sulfate reduction and metal sulfide precipitation do not appear to be a permanent sink for metals. 相似文献
8.
Carolina Reyes Dominik Schneider Andrea Thürmer Ajinkya Kulkarni Marko Lipka Saar Y. Sztejrenszus 《Geomicrobiology journal》2017,34(10):840-850
In many marine surface sediments, the reduction of manganese (Mn) and iron (Fe) oxides is obscured by sulfate reduction, which is regarded as the predominant anaerobic microbial respiration process. However, many dissimilatory sulfate and sulfur reducing microorganisms are known to utilize alternative electron acceptors such as metal oxides. In this study, we tested whether sulfate and sulfur reducing bacteria are linked to metal oxide reduction based on biogeochemical modeling of porewater concentration profiles of Mn2+ and Fe2+ in Bothnian Bay (BB) and Skagerrak (SK) sediments. Steady-state modeling of Fe2+ and Mn2+ porewater profiles revealed zones of net Fe (0–9 cm BB; ~10 and 20 cm SK) and Mn (0–5 cm BB; 2–8 cm SK) species transformations. 16S rRNA pyrosequencing analysis of the in-situ community showed that Desulfobacteraceae, Desulfuromonadaceae and Desulfobulbaceae were present in the zone of Fe-reduction of both sediments. Rhodobacteraceae were also detected at high relative abundance in both sediments. BB sediments appeared to harbor a greater diversity of potential Fe-reducers compared to SK. Additionally, when the upper 10 cm of sediment from the SK was incubated with lepidocrocite and acetate, Desulfuromonas was the dominant bacteria. Real-time quantitative polymerase chain reaction (qPCR) results showed decreasing dsrA gene copy numbers with depth coincided with decreased Fe-reduction activity. Our results support the idea that sulfur and sulfate reducing bacteria contribute to Fe-reduction in the upper centimeters of both sediments. 相似文献
9.
Flowthrough reactor flasks are described that allow continuous low-level nutrient input to mixed anoxic sediments without dilution of the sediment. The flasks were tested by simulating sulfate inputs into sediments collected from a freshwater eutrophic lake. After an initial 2-day adaptation within the reactor system, rates of methane production and sulfate consumption were constant for the duration of a 12-day incubation. A sulfate input rate of 0.15 mmol liter of sediment−1 day−1 resulted in an equivalent rate of sulfate removal, which was unaffected by inputs of acetate (1.0 mmol liter of sediment−1 day−1). The rate of methane production in control reactors, 0.18 mmol liter of sediment−1 day−1, was doubled by the addition of acetate, whereas sulfate consumption was only stimulated by additions of high concentrations of sulfate plus acetate (1.5 and 1.0 mmol liter of sediment−1 day−1, respectively). The reactor system appears to be effective in maintaining the balance between sulfate reduction and methane production in freshwater sediments and is potentially useful for study of the response of sediment populations to varying inputs of naturally occurring substrates, selected inhibitors, or xenobiotic compounds. 相似文献
10.
A simple assay for analysis of sulfate in a 100-μl volume of serum is described. Selective precipitation of 133Ba after removal of protein with trichloroacetic acid is reproducible and accurate. In particular, no major interference from calcium or phosphate within the physiological range of concentration is found. 相似文献
11.
In situ experiments were conducted to measure sulfate reduction rates and identify rate-limiting factors in a shallow, alluvial aquifer contaminated with municipal landfill leachate. Single-well, push–pull tests conducted in a well adjacent to the landfill with >8 mM dissolved organic carbon (DOC) exhibited a sulfate reduction rate of 3.2 μmol SO4
−2 (L sediment)−1 day−1, a value in close agreement with laboratory-derived estimates. Identical tests conducted in wells located 90 m downgradient where DOC levels remained high (>3 mM) showed no detectable sulfate consumption, and laboratory assays confirmed this observation. However, the rates of sulfate reduction in sediment samples obtained from this site were three times larger when they were amended with filter-sterilized groundwater from the upgradient location. The effect of various amendments on sulfate reduction rates was further examined in laboratory incubations using sediment collected from the downgradient site amended with 35S sulfate. Unamended sediments showed only weak conversion of the tracer to 35S sulfide (5 to 7 cpm/cm2), whereas the addition of Desulfovibrio cells increased 35S sulfide production to 44 cpm/cm2. However, the application of heat-killed Desulfovibrio had a similar stimulatory effect, as did a lactate amendment. Collectively, these findings indicate that the lack of measurable sulfate reduction at the downgradient site was not due to the absence of the necessary metabolic potential, the presence of lower sulfate concentration, or the quantity of electron donor, but by its biodegradability. The findings also indicate that field bioaugmentation attempts should be interpreted with caution. 相似文献
12.
Bacterial sulfate reduction in the surface sediment and the water column of Lake Mendota, Madison, Wis., was studied by using radioactive sulfate (35SO42−). High rates of sulfate reduction were observed at the sediment surface, where the sulfate pool (0.2 mM SO42−) had a turnover time of 10 to 24 h. Daily sulfate reduction rates in Lake Mendota sediment varied from 50 to 600 nmol of SO42− cm−3, depending on temperature and sampling date. Rates of sulfate reduction in the water column were 103 times lower than that for the surface sediment and, on an areal basis, accounted for less than 18% of the total sulfate reduction in the hypolimnion during summer stratification. Rates of bacterial sulfate reduction in the sediment were not sulfate limited at sulfate concentrations greater than 0.1 mM in short-term experiments. Although sulfate reduction seemed to be sulfate limited below 0.1 mM, Michaelis-Menten kinetics were not observed. The optimum temperature (36 to 37°C) for sulfate reduction in the sediment was considerably higher than in situ temperatures (1 to 13°C). The response of sulfate reduction to the addition of various electron donors metabolized by sulfate-reducing bacteria in pure culture was investigated. The degree of stimulation was in this order: H2 > n-butanol > n-propanol > ethanol > glucose. Acetate and lactate caused no stimulation. 相似文献
13.
Microbiological and biogeochemical measurements showed that the intensities of CO2 assimilation, methane oxidation, and sulfate reduction at the Lost City vent field (3° N) reach 3.8 µg C/(1 day), 0.06 µg C/(1 day), and 117 µg S/(1 day), respectively. On the surface of the carbonate structures occurring at this field, two varieties of bacterial mats were found. The first variety, which is specific to the Lost City alkaline vent field, represents jellylike bacterial mats dominated by slime-producing bacteria of several morphotypes. This mat variety also contains chemolithotrophic and heterotrophic microorganisms, either microaerobic or anaerobic. The intensities of CO2 assimilation, methane oxidation, and sulfate reduction in this variety reach 747 µg C/(dm3 day), 0.02 µg C/(dm3 day), and 28000 µg S/(dm3 day), respectively. Bacterial mats of the second variety are formed by nonpigmented filamentous sulfur bacteria, which are close morphologically to Thiothrix. The intensities of CO2 assimilation, methane oxidation, and sulfate reduction in the second mat variety reach 8.2 µg C/(dm3 day), 5.8 µg C/(dm3 day), and 17000 µg S/(dm3 day), respectively. These data suggest the existence of subsurface microflora at the Lost City vent field.Translated from Mikrobiologiya, Vol. 74, No. 1, 2005, pp. 111–118.Original Russian Text Copyright © 2005 by Dulov, Lein, Dubinina, Pimenov. 相似文献
14.
Multiple sulfur isotope constraints on microbial sulfate reduction below an Archean seafloor hydrothermal system
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Microbial sulfate reduction is among the most ubiquitous metabolic processes on earth. The oldest evidence of microbial sulfate reduction appears in the ca. 3.5 Ga Dresser Formation in the North Pole area of Pilbara Craton in Western Australia. That evidence was found through analysis of quadruple sulfur isotopes of sulfate and sulfide minerals deposited on the seafloor. However, the activity of microbial sulfate reduction below the Archean seafloor remains poorly understood. Here, we report the quadruple sulfur isotopic compositions of sulfide minerals within hydrothermally altered seafloor basalt and less altered basaltic komatiite collected from the North Pole Dome area. The Δ33S values of the sulfide minerals were nonzero negative, suggesting that sulfate reduction occurred below the Archean seafloor. To constrain the substrate sulfate sources and sulfate reduction processes, we constructed a numerical model. Comparing the modeled and observed sulfur isotopes, we show that the substrate sulfate comprises seawater sulfate with a negative Δ33S anomaly and 34S‐enriched sulfate with no anomalous Δ33S. The latter component probably represents sulfate produced by local hydrothermal processes. The maximum sulfur isotopic fractionation between the putative substrate sulfate and the observed sulfide minerals within the altered basalt and basaltic komatiite is 35‰, which is consistent with a microbial origin. Alternatively, thermochemical sulfate reduction may also produce sulfide. However, considering the hydrothermal temperature inferred from the metamorphic grade of the altered basalt, the sulfur isotopic fractionation produced by inorganic sulfate reduction is probably below 20‰. Collectively, larger fractionations imply the involvement of biological sulfate reduction processes, both in the hydrothermal system below the seafloor and in less altered subsurface settings. 相似文献
15.
Jonathan R. Seals Jay M. McDonald David Bruns Leonard Jarett 《Analytical biochemistry》1978,90(2):785-795
A manual ATPase assay which measures the release of 32Pi from [γ-32P]ATP is described. Sodium dodecyl sulfate is used to terminate the enzyme reaction and extraction of the phophomolybdate complex into xylene: isobutanol is used to separate 32Pi from [γ-32P]ATP for quantitation by scintillation counting. The three-step assay is rapid (75–90 samples/h) and minimizes hydrolysis of ATP due to exposure to acidie conditions. The extraction procedure separates 10−15 to 10−7 mol of 32Pi from aqueous solution with an efficiency of 100,7 ± 0.62%. Less than 1% of unhydrolyzed [γ-32P]ATP is extracted. Extraction efficiency is not affected by protein or salts commonly present in enzyme incubation mixtures. Results obtained with this assay are precise, with an intraassay coefficient of variation of 0.6% and an interassay coefficient of variation of 1.8%. The results are comparable to results obtained with a spectrophotometric assay, with a correlation coefficient of 0,996, though assay performance and sensitivity are greatly improved with the isotopic assay. 相似文献
16.
Substrates for Sulfate Reduction and Methane Production in Intertidal Sediments 总被引:16,自引:12,他引:4
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The activity of and potential substrates for methane-producing bacteria and sulfate-reducing bacteria were examined in marsh, estuary, and beach intertidal sediments. Slow rates of methane production were detected in all sediments, although rates of sulfate reduction were 100- to 1,000-fold higher. After sulfate was depleted in sediments, the rates of methane production sharply increased. The addition of methylamine stimulated methanogenesis in the presence of sulfate, and [14C]methylamine was rapidly converted to 14CH4 and 14CO2 in freshly collected marsh sediment. Acetate, hydrogen, or methionine additions did not stimulate methanogenesis. [methyl-14C]methionine and [2-14C]acetate were converted to 14CO2 and not to 14CH4 in fresh sediment. No reduction of 14CO2 to 14CH4 occurred in fresh sediment. Molybdate, an inhibitor of sulfate reduction, inhibited [2-14C]acetate metabolism by 98.5%. Fluoracetate, an inhibitor of acetate metabolism, inhibited sulfate reduction by 61%. These results suggest that acetate is a major electron donor for sulfate reduction in marine sediments. In the presence of high concentrations of sulfate, methane may be derived from novel substrates such as methylamine. 相似文献
17.
Kinetics of nitrate and sulfate removal using a mixed microbial culture with or without limited-oxygen fed 总被引:1,自引:0,他引:1
Xi-jun Xu Chuan Chen Ai-jie Wang Hong-liang Guo Ye Yuan Duu-Jong Lee Nan-qi Ren 《Applied microbiology and biotechnology》2014,98(13):6115-6124
The biological degradation of nitrate and sulfate was investigated using a mixed microbial culture and lactate as the carbon source, with or without limited-oxygen fed. It was found that sulfate reduction was slightly inhibited by nitrate, since after nitrate depletion the sulfate reduction rate increased from 0.37 mg SO4 2?/mg VSS d to 0.71 mg SO4 2?/mg VSS d, and the maximum rate of sulfate reduction in the presence of nitrate corresponded to 56 % of the non-inhibited sulfate reduction rate determined after nitrate depleted. However, simultaneous but not sequential reduction of both oxy-anions was observed in this study, unlike some literature reports in which sulfate reduction starts only after depletion of nitrate, and this case might be due to the fact that lactate was always kept above the limiting conditions. At limited oxygen, the inhibited effect on sulfate reduction by nitrate was relieved, and the sulfate reduction rate seemed relatively higher than that obtained without limited-oxygen fed, whereas kept almost constant (0.86–0.89 mg SO4 2?/mg VSS d) cross the six ROS states. In contrast, nitrate reduction rates decreased substantially with the increase in the initial limited-oxygen fed, showing an inhibited effect on nitrate reduction by oxygen. Kinetic parameters determined for the mixed microbial culture showed that the maximum specific sulfate utilization rate obtained (0.098?±?0.022 mg SO4 2?/(mg VSS h)) was similar to the reported typical value (0.1 mg SO4 2?/(mg VSS h)), also indicating a moderate inhibited effect by nitrate. 相似文献
18.
Zhongping Deng Lisa A. Dailey Joleen Soukup Jacqueline Stonehuerner Judy D. Richards Kimberly D. Callaghan Funmei Yang Andrew J. Ghio 《Biometals》2009,22(5):803-815
Despite recurrent exposure to zinc through inhalation of ambient air pollution particles, relatively little information is
known about the homeostasis of this metal in respiratory epithelial cells. We describe zinc uptake and release by respiratory
epithelial cells and test the postulate that Zn2+ transport interacts with iron homeostasis in these same cells. Zn2+ uptake after 4 and 8 h of exposure to zinc sulfate was concentration- and time-dependent. A majority of Zn2+ release occurred in the 4 h immediately following cell exposure to ZnSO4. Regarding metal importers, mRNA for Zip1 and Zip2 showed no change after respiratory epithelial cell exposure to zinc while
mRNA for divalent metal transporter (DMT)1 increased. Western blot assay for DMT1 protein supported an elevated expression
of this transport protein following zinc exposure. RT-PCR confirmed mRNA for the metal exporters ZnT1 and ZnT4 with the former
increasing after ZnSO4. Cell concentrations of ferritin increased with zinc exposure while oxidative stress, measured as lipid peroxides, was decreased
supporting an anti-oxidant function for Zn2+. Increased DMT1 expression, following pre-incubations of respiratory epithelial cells with TNF-α, IFN-γ, and endotoxin, was
associated with significantly decreased intracellular zinc transport. Finally, incubations of respiratory epithelial cells
with both zinc sulfate and ferric ammonium citrate resulted in elevated intracellular concentrations of both metals. We conclude
that exposure to zinc increases iron uptake by respiratory epithelial cells. Elevations in cell iron can possibly affect an
increased expression of DMT1 and ferritin which function to diminish oxidative stress. Comparable to other metal exposures,
changes in iron homeostasis may contribute to the biological effects of zinc in specific cells and tissues. 相似文献
19.
Biofilm Dynamics and Kinetics during High-Rate Sulfate Reduction under Anaerobic Conditions 总被引:7,自引:3,他引:4
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Per Halkjaer Nielsen 《Applied microbiology》1987,53(1):27-32
The sulfate kinetics in an anaerobic, sulfate-reducing biofilm were investigated with an annular biofilm reactor. Biofilm growth, sulfide production, and kinetic constants (Km and Vmax) for the bacterial sulfate uptake within the biofilm were determined. These parameters were used to model the biofilm kinetics, and the experimental results were in good agreement with the model predictions. Typical zero-order volume rate constants for sulfate reduction in a biofilm without substrate limitation ranged from 56 to 93 μmol of SO24-cm−3 h−1 at 20°C. The temperature dependence (Q10) of sulfate reduction was equivalent to 3.4 at between 9 and 20°C. The measured rates of sulfate reduction could explain the relatively high sulfide levels found in sewers and wastewater treatment systems. Furthermore, it has been shown that sulfate reduction in biofilms just a few hundred micrometers thick is limited by sulfate diffusion into biofilm at concentrations below 0.5 mM. This observation might, in some cases, be an explanation for the relatively poor capacity of the sulfate-reducing bacteria to compete with the methanogenic bacteria in anaerobic wastewater treatment in submerged filters. 相似文献
20.
We investigated the effects of sulfate concentration on sulfate reduction and net S storage in lake sediments using34S as a tracer. The water overlying intact sediment cores from the hypolimnion of Mares Pond, MA, was replaced with two Na2
34SO4 solutions at either ambient (70 M) or elevated (260 M) sulfate concentrations. The 34S of the added sulfate was 4974 . Over two months, the net sulfate reduction rate in the ambient sulfate treatment was zero, while the net rate for the high sulfate treatment was 140 moles/m2/d. The water overlying the cores was kept under oxic conditions and the sediment received no fresh carbon inputs, thus the net rate reported may underestimate the in situ rate. Gross sulfate reduction rates calculated by isotope dilution were approximately 350 moles/m2/d for both treatments. While the calculation of gross sulfate reduction rates in intact sediment cores can be complicated by differential diffusion of34S and32S, isotopic fractionation, and the possible formation of ester sulfates, we believe these effects to be small. The results suggest that sulfate reduction is not strongly sulfate-limited in Mares Pond. The difference in net sulfate reduction rates between treatments resulted from a decrease in sulfide oxidation and suggests the importance of reoxidation in controlling net S storage in lake sediments. In both treatments the CRS and organic S fractions were measurably labelled in34S. Below the sediment surface, the CRS fraction was the more heavily labelled storage product for reduced sulfides. 相似文献