The distribution and activity of sulphate reducing bacteria in estuarine and coastal marine sediments

Sulphate-reducing bacteria (SRB) play a vital role both the carbon and sulphur cycles and thus are extremely important components of the global microbial community. However, it is clear that the ecology, the distribution and activity of different SRB groups is poorly understood. Probing of rRNA suggests that different sediments have distinctly different patterns of SRB with complex factors controlling the activity of these organisms. The linking of community structure and function using sediment slurry microcosms suggests that certain groups of SRB, e.g., Desulfobacter and Desulfobulbus, can be linked to the use of specific substrates in situ. However, it is still unclear what environmental substrates are utilised by the majority of known SRBs. The work to date has greatly enhanced our understanding of the ecology of these organisms and is beginning to suggest patterns in their distribution and activity that may be relevant to understanding microbial ecology in general. This revised version was published online in August 2006 with corrections to the Cover Date.     

Bicarbonate-dependent production and methanogenic consumption of acetate in anoxic paddy soil

Abstract Acetate turnover was measured in slurries of anoxic methanogenic paddy soil after addition of carrier-free [2-¹⁴C]-acetate. Acetate concentrations stayed fairly constant for about 1–2 days indicating steady state between production and consumption reactions. Depending on the experiment, acetate concentrations were between 100 and 3000 μM. Turnover rates were determined from the logarithmic decrease of [2-¹⁴C]-acetate or from the accumulation of acetate in the presence of chloroform resulting in similar values, i.e. 12–13 nmol h⁻¹g⁻¹d.w. soil at 17°C and 36–88 nmol h⁻¹g⁻¹d.w. at 30°C. Acetate consumption was completely inhibited by chloroform. The respiratory index (RI) was < 0.27. Hence, acetate was apparently consumed by methanogenic bacteria. About 80–90% of the CH₄ produced originated from the methyl group of acetate. The role of homoacetogenesis for acetate production was studied by measuring the incorporation of radioactive bicarbonate into acetate. In different experiments, CO₂ incorporation accounted for fractions of 1–60% of the acetate produced, about 10% being the most likely value for steady-state conditions. The fraction increased at high H₂ concentrations and decreased at high acetate concentrations. The rate of H₂ production that was required for chemolithotrophic acetate production from CO₂ was two orders of magnitude higher than the actually measured rate. Hence, most of the CO₂ incorporation into acetate was caused by electron donors other than H₂ (e.g., carbohydrates) and/or by exchange reactions.     

Bacterial abundance in relation to surface area and organic content of marine sediments

Based on direct measurements on surface sediments collected from an intertidal salt marsh, a positive relationship was demonstrated between bacterial abundance and specific surface area of sediment. While this relationship has been postulated previously, this is the first direct confirmation that it holds over a wide range of sediment types. A laboratory experiment was conducted to determine the effects of specific surface area, distribution of surface area, and organic loading on bacterial colonization. Model sediments included angular silica particles, kaolin, and spherical glass beads, used singly or in mixtures. Organic loading resulted in substantial enhancement of bacterial colonization. Distribution of surface area controlled by textural, shape, and sorting, had a complex effect, with glass bead sediments generally supporting better colonization than silica particles or kaolin. The effect of specific surface area was noted only in restricted comparisons of similarly shaped glass beads.     

Uptake and turnover of acetate in hypersaline environments

Abstract: Acetate uptake and turnover rates were determined for the heterotrophic community in hypersaline environments (saltern crystallizer ponds, the Dead Sea) dominated by halpphilic Archaea. Acetate was formed from glycerol, which is potentially the major available carbon source for natural communities of halophilic Archaea. Values of [ K _t+ S _n] (the sum of the substrate affinity and the substrate concentration present in situ) for acetate measured in saltern crystallizer ponds were around 4.5–11.5 μM, while in the Dead Sea during a Dunaliella bloom values up to 12.8 μM were found. Maximal theoretical rates ( V _max) of acetate uptake in saltern crystallizer ponds were 12–56 nmol l⁻¹ h⁻¹, with estimated turnover times for acetate ( T _t) between 127–730 h at 35°C. V _max values measured in the Dead Sea were between 0.8 and 12.8 nmol l⁻¹ h⁻¹, with turnover times in the range of 320–2190 h. V _max values for acetate were much lower than those for glycerol. Comparisons with pure cultures of halophilic Archaea grown under different conditions showed that the natural communities were not adapted for preferential use of acetate. Both in natural brines and in pure cultures of halophilic Archaea, acetate incorporation rates rapidly decreased above the optimum pH value, probably since acetate enters the cell only in its unionized form. The low affinity for acetate, together with low potential utilization rates result in the long acetate turnover times, which explains the accumulation of acetate observed when low concentrations of glycerol are supplied as a nutrient to natural communities of halophilic Archaea.     

Sulfide-induced dissimilatory nitrate reduction to ammonia in anaerobic freshwater sediments

Abstract: Different reduced sulfur compounds (H₂S, FeS, S₂O₃²⁻) were tested as electron donors for dissimilatory nitrate reduction in nitrate-amended sediment slurries. Only in the free sulfide-enriched slurries was nitrate appreciably reduced to ammonia (     ), with concomitant oxidation of sulfide to S⁰ (     ). The initial concentration of free sulfide appears as a factor determining the type of nitrate reduction. At extremely low concentrations of free S²⁻ (metal sulfides) nitrate was reduced via denitrification whereas at higher S²⁻ concentrations, dissimilatory nitrate reduction to ammonia (DNRA) and incomplete denitrification to gaseous nitrogen oxides took place. Sulfide inhibition of NO- and N₂O- reductases is proposed as being responsible for the driving part of the electron flow from S²⁻ to NH₄⁺.     

Measure of microbial turnover of carbon in anoxic freshwater sediments: cautionary comments

Small sediment cores were used to determine the turnover of a range of carbon substrates, particularly volatile fatty acids, by bentic bacteria. Volatile fatty acids were determined using an HPLC sytem in cojunction with a conductivity detector. At the low eluent strength used 1 μM acetate was detected with ease. Small cores were used in an attempt to maintain the natural partial pressure of hydrogen, an important factor in the control of anerobic metabolism of fatty acids. Although this is preferable to the disturbance of the sediment which occurs if it is resuspended a a slurry, problems are encountered at low substrate concentrations. The time taken for the added substrate to equilibrate in both radial and vertical planes may result in turnover times which vary with the incubation time used. Reduction of the qunatity of added substrate and increased replication may improve the accuracy of the estimates obtained, but more serious consideration must be given to the availability of the substrates to the benthic bacteria.     

Comparative study of enrichment methods for the isolation of autotrophic nitrifying bacteria from soil, estuarine and marine sediments

Abstract A comparative study has been undertaken to determine the efficiency of methods for the enrichment and isolation of autotrophic nitrifying bacteria from soils and estuarine and marine sediments. Chemostat enrichments proved to be the most efficient means of isolating autotrophic NH⁺₄ oxidisers whereas NO⁻₂ oxidising bacteria were never successfully enriched by this method. In contrast, gel enrichment and traditional batch culture enrichments of nitrifying bacteria were comparatively time consuming procedures and the degree of enrichment obtained for NH⁺₄ oxidising bacteria never approached that obtained with continuous culture enrichments. Gel enrichments, however, because they have continuous physicochemical gradients provide qualitative advantages in that morphologically distinct types of nitrifying bacteria can be isolated from the same gel.     

Mechanisms of acetate formation and acetate activation in halophilic archaea

The halophilic archaea Halococcus (Hc.) saccharolyticus, Haloferax (Hf.) volcanii, and Halorubrum (Hr.) saccharovorum were found to generate acetate during growth on glucose and to utilize acetate as a growth substrate. The mechanisms of acetate formation from acetyl-CoA and of acetate activation to acetyl-CoA were studied. Hc. saccharolyticus, exponentially growing on complex medium with glucose, formed acetate and contained ADP-forming acetyl-CoA synthetase (ADP-ACS) rather than acetate kinase and phosphate acetyltransferase or AMP-forming acetyl-CoA synthetase. In the stationary phase, the excreted acetate was completely consumed, and cells contained AMP-forming acetyl-CoA synthetase (AMP-ACS) and a significantly reduced ADP-ACS activity. Hc. saccharolyticus, grown on acetate as carbon and energy source, contained only AMP-ACS rather than ADP-ACS or acetate kinase. Cell suspensions of Hc. saccharolyticus metabolized acetate only when they contained AMP-ACS activity, i.e., when they were obtained after growth on acetate or from the stationary phase after growth on glucose. Suspensions of exponential glucose-grown cells, containing only ADP-ACS but not AMP-ACS, did not consume acetate. Similar results were obtained for the phylogenetic distantly related halophilic archaea Hf. volcanii and Hf. saccharovorum. We conclude that, in halophilic archaea, the formation of acetate from acetyl-CoA is catalyzed by ADP-ACS, whereas the activation of acetate to acetyl-CoA is mediated by an inducible AMP-ACS.Abbreviations. Hc. Halococcus - Hf. Haloferax - Hr. Halorubrum - Hb. Halobacterium An erratum to this article can be found at     

Bioremediation of organic and metal contaminants with dissimilatory metal reduction

PCR fingerprinting offers a practical molecular means to quickly and reliably differentiate bacteria for microbial products screening. A combination of low resolution and high resolution PCR fingerprinting provides a hirarchical system which allows the discrimination of bacteria at species and subspecies level within 7 h. DNA was extracted from cells by incubating them in water at 95°C for 30 min. A sample of 1 l of the cell-free aqueous extract then was used as a source of template DNA in the PCR. The PCR products were separated by electrophoresis on an acrylamide gel and visualized by ethidium bromide staining. The band patterns generated for each different culture were unique, reproducible, and independent of cultivation conditions. Band patterns may be compared visually or by using imaging and pattern matching software. In our laboratory, bacteria such as actinomycetes, Gram-negative and Gram-positive soil eubacteria, and photosynthetic non-sulfur bacteria have been differentiated using PCR fingerprinting.     

The effect of long-term nitrate treatment on SRB activity,corrosion rate and bacterial community composition in offshore water injection systems

Biogenic production of hydrogen sulphide (H₂S) is a problem for the oil industry as it leads to corrosion and reservoir souring. Continuous injection of a low nitrate concentration (0.25–0.33 mM) replaced glutaraldehyde as corrosion and souring control at the Veslefrikk and Gullfaks oil field (North Sea) in 1999. The response to nitrate treatment was a rapid reduction in number and activity of sulphate-reducing bacteria (SRB) in the water injection system biofilm at both fields. The present long-term study shows that SRB activity has remained low at ≤0.3 and ≤0.9 μg H₂S/cm²/day at Veslefrikk and Gullfaks respectively, during the 7–8 years with continuous nitrate injection. At Veslefrikk, 16S rRNA gene based community analysis by PCR–DGGE showed that bacteria affiliated to nitrate-reducing sulphide-oxidizing Sulfurimonas (NR–SOB) formed major populations at the injection well head throughout the treatment period. Downstream of deaerator the presence of Sulfurimonas like bacteria was less pronounced, and were no longer observed 40 months into the treatment period. The biofilm community during nitrate treatment was highly diverse and relative stable for long periods of time. At the Gullfaks field, a reduction in corrosion of up to 40% was observed after switch to nitrate treatment. The present study show that nitrate injection may provide a stable long-term inhibition of SRB in sea water injection systems, and that corrosion may be significantly reduced when compared to traditional biocide treatment.     

Ommatidial structure in relation to turnover of photoreceptor membrane in the locust

Summary In the compound eye of the locust, Locusta, the cross-sectional area of the rhabdoms increases at dusk by 4.7-fold due to the rapid assembly of new microvillar membrane, and decreases at dawn by a corresponding amount as a result of pinocytotic shedding from the microvilli. The rhabdoms at night have more and longer photoreceptor microvilli than rhabdoms during the day. The orientations of the six rhabdomeres that comprise the distal rhabdom also change. The density of intramembrane particles on the P-face of the microvillar membrane, putatively representing mostly rhodopsin molecules, or aggregates thereof, does not change.An alteration in the size of the ommatidial field-stop, produced by the primary pigment cells, is concomitant with the change in rhabdom size. At night the increase in size of the field-stop must widen the angular acceptance of a rhabdom, increasing the capture of photons from an extended field. Conversely, during the day, when photons are more abundant, its decrease must narrow the acceptance angle, increasing angular resolution. Because of the presence of this field-stop, the optics of the ommatidium would not be greatly affected if the rhabdom were to remain always at its night size. It is argued, therefore, that the variable-size rhabdom must have resulted from some demand other than that of light/dark adaptation.Changes in size and organisation of the rhabdoms in response to various light regimes indicate that: (1) Rapid shedding of photoreceptor membrane is induced by the onset of light, but shedding also occurs slowly in darkness during the day. (2) Microvillar assembly is initiated by the onset of darkness, but also occurs at the normal time of dusk without a change in ambient lighting, provided there has been some light during the day. Therefore, both shedding and assembly of microvillar membrane are affected by the state of illumination, but also appear to be under some endogenous control.     

Selective inhibition of methanogenesis to enhance ethanol and n-butyrate production through acetate reduction in mixed culture fermentation

Acetate reduction is an alternative digestion process to convert organic waste into ethanol. Using acetate for fuel ethanol production offers the opportunity to use organic waste materials instead of sugar-containing feedstock. Methanogenesis, however, competes with acetate reduction for acetate and hydrogen and lowers the final efficiency. The aim of this research is to selectively inhibit methanogenesis and to enhance acetate reduction. Acetate reduction was stimulated in batch tests at pH between 4.5 and 8; and at pH 6 with and without thermal pre-treatment. It was found that methanogenesis was selectively inhibited while acetate reduction was enhanced after thermal pre-treatment incubated at pH 6. Initially the acetate reduction yielded 7.7 ± 3.2 mM ethanol with an efficiency of 60.2 ± 8.7%, but later on it was consumed to form 7.02 ± 0.85 mM n-butyrate with an efficiency of 76.2 ± 14.0%. It was the first time demonstrated that n-butyrate can be produced by mixed cultures from only acetate and hydrogen.     

Influence of bioturbation on denitrification and dissimilatory nitrate reduction to ammonium (DNRA) in freshwater sediments

Intensive agriculture leads to increased nitrogen fluxes (mostly as nitrate, NO₃ ^?) to aquatic ecosystems, which in turn creates ecological problems, including eutrophication and associated harmful algal blooms. These problems have focused scientific attention on understanding the controls on nitrate reduction processes such as denitrification and dissimilatory nitrate reduction to ammonium (DNRA). Our objective was to determine the effects of nutrient-tolerant bioturbating invertebrates (tubificid oligochaetes) on nitrogen cycling processes, specifically coupled nitrification–denitrification, net denitrification, DNRA, and biogeochemical fluxes (O₂, NO₃ ^?, NH₄ ⁺, CO₂, N₂O, and CH₄) in freshwater sediments. A mesocosm experiment determined how tubificid density and increasing NO₃ ^? concentrations (using N¹⁵ isotope tracing) interact to affect N cycling processes. At the lowest NO₃ ^? concentration and in the absence of bioturbation, the relative importance of denitrification to DNRA was similar (i.e., 49.6 and 50.4 ± 8.1 %, respectively). Increasing NO₃ ^? concentrations in the control cores (without fauna) stimulated denitrification, but did not enhance DNRA, which significantly altered the relative importance of denitrification compared to DNRA (94.6 vs. 5.4 ± 0.9 %, respectively). The presence of tubificid oligochaetes enhanced O₂, NO₃ ^?, NH₄ ⁺ fluxes, greenhouse gas production, and N cycling processes. The relative importance of denitrification to DNRA shifted towards favoring denitrification with both the increase in NO₃ ^? concentrations and the increase of bioturbation activity. Our study highlights that understanding the interactions between nutrient-tolerant bioturbating species and nitrate contamination is important for determining the nitrogen removal capacity of eutrophic freshwater ecosystems.     

Acetate, lactate, propionate, and isobutyrate as electron donors for iron and sulfate reduction in Arctic marine sediments, Svalbard

The contribution of volatile fatty acids (VFA) as e(-)-donors for anaerobic terminal oxidation of organic carbon through iron and sulfate reduction was studied in Arctic fjord sediment. Dissolved inorganic carbon, Fe(2+), VFA concentrations, and sulfate reduction were monitored in slurries from the oxidized (0-2 cm) and the reduced (5-9 cm) zone. In the 0-2 cm layer, 2/3 of the mineralization could be attributed to sulfate reduction and 1/3 to iron reduction. In the 5-9 cm layer, sulfate reduction was the sole mineralization process. Acetate and lactate turnover rates were measured by radiotracer. Inhibition of sulfate reduction with selenate resulted in the accumulation of acetate, propionate, and isobutyrate. The acetate turnover rates determined by radiotracer and accumulation after inhibition were similar. VFA turnover accounted for 21% and 52% of the mineralization through sulfate reduction in the 0-2 and 5-9 cm layer, respectively. Acetate and lactate turnover in the inhibited 0-2 cm slurry was attributed to iron reduction and accounted for 10% and 2% of the iron reduction. Therefore, 88% and 79% of the iron and sulfate reduction in the 0-2 cm layer, respectively, must be fueled by alternative e(-)-donors. The accumulation of VFA in the selenate-inhibited 0-2 cm slurry did not enhance iron reduction, indicating that iron reducers were not limited by VFA availability.     

Occurrence of sulphate-reducing bacteria in human faeces and the relationship of dissimilatory sulphate reduction to methanogenesis in the large gut

Sulphate-reducing bacteria (SRB) were enumerated in 40 faecal samples obtained from two different human populations in the United Kingdom and rural South Africa. Species able to metabolize acetate, lactate, propionate, butyrate, H2/CO2, succinate, pyruvate, valerate, ethanol and a glutamate/serine/alanine mixture were found in faeces from both populations. Although a variety of nutritionally and morphologically distinct species of SRB belonging to the genera Desulfotomaculum, Desulfobacter, Desulfomonas and Desulfobulbus were identified, Desulfovibrio types always predominated. Significant numbers of SRB were present only in faecal samples from subjects whose breath methane excretion was low or undetectable. Reduced or absent methanogenesis in the presence of SRB was confirmed in fermentation studies with faecal slurries. Fourteen of 20 (70%) British faecal samples contained SRB and the remainder produced methane. The reverse was the case with 20 rural black South Africans, where only three (15%) of the samples had significant levels of SRB; the remaining 85% produced methane. These results suggest that to a large extent, dissimilatory sulphate reduction and methanogenesis are mutually exclusive in the human large gut.     

Occurrence of sulphate-reducing bacteria in human faeces and the relationship of dissimilatory sulphate reduction to methanogenesis in the large gut

Sulphate-reducing bacteria (SRB) were enumerated in 40 faecal samples obtained from two different human populations in the United Kingdom and rural South Africa. Species able to metabolize acetate, lactate, propionate, butyrate, H₂/CO₂, succinate, pyruvate, valerate, ethanol and a glutamate/serine/alanine mixture were found in faeces from both populations. Although a variety of nutritionally and morphologically distinct species of SRB belonging to the genera Desulfotomaculum, Desulfobacter, Desulfomonas and Desulfobulbus were identified, Desulfovibrio types always predominated. Significant numbers of SRB were present only in faecal samples from subjects whose breath methane excretion was low or undetectable. Reduced or absent methanogenesis in the presence of SRB was confirmed in fermentation studies with faecal slurrries. Fourteen of 20 (70%) British faecal samples contained SRB and the remainder produced methane. The reverse was the case with 20 rural black South Africans, where only three (15%) of the samples had significant levels of SRB; the remaining 85% produced methane. These results suggest that to a large extent, dissimilatory sulphate reduction and methanogenesis are mutually exclusive in the human large gut.