Methane Reduction Research Articles

A Comparative Study between Microbial Fermentation and Non-Fermentation on Biological Activities of Medicinal Plants, with Emphasis on Enteric Methane Reduction

A Comparative Study between Microbial Fermentation and Non-Fermentation on Biological Activities of Medicinal Plants, with Emphasis on Enteric Methane Reduction

Methane emissions from oil and gas transport facilities – exploring innovative ways to mitigate environmental consequences

Climate change impacts are increasingly becoming more evident e.g. through heavy rainfall episodes and subsequent flooding. Methane is a significant greenhouse gas that has been linked to these impacts and the oil and gas industry is a major source of anthropogenic methane emission. Recent studies have suggested that the tropical region hold some unexpectedly high methane concentration and that the recent changes in the global methane burden are poorly understood. To address this research gap, we present a first effort to quantify methane emissions from one of the most vulnerable oil and gas infrastructures in Nigeria (a tropical country). A combination of the Intergovernmental Panel on Climate Change tier-1 approach and an adapted Greenhouse Gases, Regulated Emissions, and Energy Use in Transportation model was used to estimate methane emissions from the system 2C transport pipeline. We then tested the hypothesis of no significant change in methane emissions trend from the pipeline using the between group t-test inferential analysis. Key findings include: (a) a crude oil throughput of 55,143 to 1,500,500 barrels (8767 to 238,561 m3) emitted methane ranging from 0.04734 to 1.288MT (± 50 to 200%) respectively, and (b) surprisingly, methane emissions along the system 2C pipeline seem to have continued without significant change between 2005, and 2008 to 2012 despite the low crude oil throughput in 2009. This indicates the likelihood of continuous but rising methane emissions from the pipeline network over a six-year period; and only further research can ascertain if similar trend can be observed elsewhere in the tropical region. These findings are unique and contribute to the current global debate on methane emissions from the largely unmonitored tropical region. Therefore, we recommend that stakeholders should set up a study plan for the identification and continuous monitoring of methane emissions from the key oil and gas infrastructure and explore opportunities for geoengineering applications as part of climate change mitigation. Coordinated engagement in international schemes such as the Natural Gas STAR program, Climate and Clean Air Coalition, Global Methane Initiative amongst others would promote strategic and measurable methane reduction plans in Nigeria and other countries within/outside the tropical region.

The effect of incremental levels of dietary nitrate on methane emissions in Holstein steers and performance in Nelore bulls.

Two experiments were conducted to study effects of dietary nitrate on enteric methane production, blood methemoglobin concentration, and growth rate in cattle. In Exp. 1, 36 Holstein steers (288 ± 25 kg BW) were fed increasing levels of dietary nitrate (6 levels; 0 to 3.0% of feed DM) in corn silage-based total mixed rations. Nitrate was introduced gradually in a 25-d adaptation period before methane production was determined in environmentally controlled rooms. In the rooms, feed intake was restricted and similar among all treatments. Methane production (g/d) decreased linearly as dietary nitrate concentration increased (P < 0.01). The apparent efficiency (measured methane reduction divided by potential methane reduction) with which enteric methane was mitigated was 49%. Blood methemoglobin levels increased with increasing nitrate dose. In Exp. 2, 300 Nelore bulls (392 ± 28 kg) were fed increasing levels of nitrate (6 levels; 0 to 2.4% of feed DM) in high-concentrate total mixed rations offered ad libitum. Feed intake decreased linearly with increasing level of dietary nitrate (P < 0.01). However, ADG was not affected by nitrate dose (P = 0.54), resulting in a linear improvement in G:F (P = 0.03) as dietary nitrate level increased. Carcass dressing percentage showed a quadratic response to incremental dietary nitrate, reaching the highest value at 0.96% of NO3/kg DM (P = 0.04).

Role of microorganisms in oceanic anoxic events (OAEs)

The accumulation of organic matter (OM) during oceanic anoxic events (OAEs) that took place in the Mesozoic may reflect different biogeochemical pathways and feedbacks related to palaeoenvironmental changes. It originates from a combination of nutrient cycling, metal concentrations and position of the chemocline and/or pycnocline controlling biological production. Because ocean stagnation cannot induce euxinia, an expanded oxygen minimum zone (OMZ) associated with upwelling and improved hydrological cycles is more commonly accepted. In some depositional settings, it permitted the evolution of anoxia/dysoxia to euxinia (sulphidic waters). The latter is recorded by the presence of anoxygenic phototrophs and involved denitrification, anaerobic oxidation of methane and sulphate reduction. In order to better constrain different OAE palaeoenvironments, models are suggested here that show the evolution from main microbial communities thriving through the water column to bacterial and more complex microbial mats. Therefore, microbial processes have a key role in OM production and metabolization. They directly influence the position of the chemocline. Detailed study of the OM preserved in black shales will be key to understanding OAEs.

Effect of Encapsulating Nitrate in Sesame Gum on In vitro Rumen Fermentation Parameters.

Encapsulation is a method used to protect material from certain undesirable environments, for controlled release at a more favorable time and place. Animal productivity would be enhanced if feed additives are delivered to be utilized at their site of action, bypassing the rumen where they are likely to be degraded by microbial action. A novel method of encapsulation with sesame gum was used to coat nitrate, a known enteric methane mitigating agent, and tested for the effect on methane reduction and other in vitro fermentation parameters using rumen fluid from cannulated Hanwoo steers. Orchard grass was used as basal diet for fermentation. The treatments were matrix (1.1 g sesame gum+0.4 g sesame oil cake) only, encapsulated nitrate (matrix+nitrate [21 mM]), free nitrate (21 mM), and a control that contained no additive. Analyses of fermentation parameters were done at 0, 3, 6, 9, 12, 24, and 48 h time periods. In comparison to control, both free and encapsulated nitrate produced significantly reduced (p<0.01) methane (76% less) and also the total volatile fatty acids were reduced. A significantly higher (p<0.01) concentration of ammonia nitrogen was obtained with the encapsulated nitrate treatment (44%) compared to the free form (28%) and matrix only (20%) (p = 0.014). This might suggest slow release of encapsulated nitrate so that it is fully reduced to ammonia. Thus, this pioneering study found a significant reduction in methane production following the use of sesame gum encapsulated nitrate that shows the potential of a controlled release system in enhancing sustainability of ruminant production while reducing/eliminating the risk of nitrite toxicity.

Efficient anaerobic mono-digestion of N-rich slaughterhouse waste: Influence of ammonia, temperature and trace elements

Three mono-digestion experiments treating slaughterhouse waste with high TKN concentration (∼11g/kg) were applied in lab-scale at mesophilic and psychrophilic conditions to study the impact of high ammonia concentrations and additives. Precipitation of sulphur by addition of ferrous chloride did not influence process behaviour, whereas supplementation of trace elements significantly improved process stability by reducing volatile fatty acid concentration towards zero.The limit of NH4-N concentration causing a rise of VFAs to 19,000mg/l and reduction of methane by 25% was found between 7.7 and 9.1g/kg which correspond to NH3 concentrations of 830–1060mg/l.Psychrophilic operation (25°C) lowered inhibitory NH3 concentration to 140mg/l, but process performance was stable only at low OLR of 0.4kgVS/m3d.Robust performance at highest possible NH4-N concentration (7.7g/kg), low VFA accumulation and satisfying methane yield of about 280Nm3/t COD was observed at OLR of 2.5kgVS/m3d at 37°C.

Sulfate reduction and methane oxidation activity below the sulfate-methane transition zone in Alaskan Beaufort Sea continental margin sediments: Implications for deep sulfur cycling

Two ∼6m long sediment cores were collected along the ∼300m isobath on the Alaskan Beaufort Sea continental margin. Both cores showed distinct sulfate-methane transition zones (SMTZ) at 105 and 120cm below seafloor (cmbsf). Sulfate was not completely depleted below the SMTZ but remained between 30 and 500μM. Sulfate reduction and anaerobic oxidation of methane (AOM) determined by radiotracer incubations were active throughout the methanogenic zone. Although a mass balance could not explain the source of sulfate below the SMTZ, geochemical profiles and correlation network analyses of biotic and abiotic data suggest a cryptic sulfur cycle involving iron, manganese and barite. Inhibition experiments with molybdate and 2-bromoethanesulfonate (BES) indicated decoupling of sulfate reduction and AOM and competition between sulfate reducers and methanogens for substrates. While correlation network analyses predicted coupling of AOM to iron reduction, the addition of manganese or iron did not stimulate AOM. Since none of the classical archaeal anaerobic methanotrophs (ANME) were abundant, the involvement of unknown or unconventional phylotypes in AOM is conceivable. The resistance of AOM activity to inhibitors implies deviation from conventional enzymatic pathways. This work suggests that the classical redox cascade of electron acceptor utilization based on Gibbs energy yields does not always hold in diffusion-dominated systems, and instead biotic processes may be more strongly coupled to mineralogy.

Niobium Carbide Based Catalyst Supports for PEMFC Cathodes

Recent research has shown that alternative compositions such as metal carbides and nitrides can potentially present the required properties of conductivity and (electro)chemical stability to replace the carbon blacks conventionally used as electrocatalyst supports in Proton Exchange Membrane Fuel Cells (PEMFC). We are currently investigating a range of synthesis routes leading to electronically conductive and chemically stable support materials based on NbC with controlled morphologies and porosity. For instance, a template-assisted method associated with specific thermal treatments1 has led to a nanostructured carbide with a high specific surface area (70 m2 g-1) and an electronic conductivity comparable to that of carbon (103 S.m-1), while a synthesis route involving electrospinning and reduction in methane provides niobium carbide nanofibres. Furthermore, hollow structures with controlled porosity can be obtained by varying the synthesis parameters. These various supports have been catalysed by deposition of platinum nanoparticles, synthesised by a microwave assisted polyol method. This contribution will describe the chemical and electrochemical characterisation of Pt on NbC-based supports, and compare the properties to those of other candidate support materials such as titania and tin oxide.1. J. Bernard D'Arbigny, G. Taillades, M. Marrony, D. J. Jones, J. Roziere, Chemical Communications, 47, 7950-7952 (2011).

XANES studies of zirconia-ceria/Ni during partial/total methane oxidation

Zirconia-ceria solid-solutions are extensively used as promoters for three-way catalysts, in addition, these materials can be used as anodes in solid oxide fuel cells (SOFCs) operated with hydrocarbons. The structural features of ZrO2-CeO2 materials in combination with oxygen storage/release capacity (OSC) are crucial for various catalytic reactions. The direct use of hydrocarbons as fuel for the SOFC (instead of pure H2), without the necessity of reforming and purification reactors can improve global efficiency of the system. The samples preparation method was developed using Zr and Ce chloride precursors, HCl aqueous solution, Pluronic P123, NH4OH and a Teflon autoclave. The samples were dried and calcined, until 540°C. The NiO impregnation was made with an ethanol dispersion of Ni(NO3)×6H2O, calcinated in air until 350°C for 2 hours. In-situ XANES experiments are capable to evaluate the reduction/oxidation potencial of Ni and Ce species in ZrO2-CeO2/Ni samples during partial/total methane oxidation and reduction reactions with H2. The experiments at the Ni K-edge/Ce L3-edge were collected at the LNLS D06A-DXAS beam line in transmission mode, using a Si(111) monochromator and a CCD camera as detector. The data were acquired during a series of temperature programmed reduction steps (TPR), under a 5% H2/He until 600°C, and mixtures of 20%CH4:5%O2/He with 2:1, 1:1 and 1:2 ratios. After each process with CH4 and O2, a TPR procedure was performed in order to evaluate the reduction capacity of the sample after reactions with CH4. The results demonstrated that NiO embedded in the porous ZrO2-CeO2 matrix, reduces at lower temperatures than standard NiO, measured in the same conditions, revealing that the mesoporous support improves the reduction of impregnated NiO. For both edges, there was formation of H2 during partial methane oxidation at 600°C. The total oxidation of methane was observed in lower temperatures (500°C). These results reveal that a high ceria content (90%) could be a great candidate for the SOFC anode.

Simultaneous enrichment of denitrifying methanotrophs and anammox bacteria.

Interaction between denitrifying anaerobic methane oxidation (DAMO) and anaerobic ammonium oxidation (anammox) processes may play an important role in global carbon and nitrogen cycles. In this study, a coculture of denitrifying methanotrophs (DAMO archaea and DAMO bacteria) and anammox bacteria, initially sourced from the environment, was enriched with a supply of methane, nitrate, and ammonium. After a 4.5-month enrichment, simultaneous oxidation of methane and ammonium and reduction of nitrate were observed. The highest rate of nitrate reduction in the suspended DAMO culture was 4.84 mmol/L/day, and simultaneously, the highest ammonium removal rate was 4.07 mmol/L/day. Fluorescence in situ hybridization and analysis of 16S rRNA gene clone libraries revealed the coexistence of DAMO archaea, DAMO bacteria, and anammox bacteria. The development of anammox bacteria might reduce the enrichment time of DAMO microorganisms and promote the activity of DAMO archaea. The activity of the reactor fluctuated during the long-term operation, which might be caused by the formation of microbial clusters whereby DAMO archaea grew in aggregates that were surrounded by anammox and DAMO bacteria. This study is the first to demonstrate that it is feasible to establish a coculture of DAMO archaea, DAMO bacteria, and anammox bacteria from environmental inocula.

Low-temperature combustion of methane using PdO/Al2O3 catalyst: Influence of crystalline phase of Al2O3 support

Palladium oxide (PdO) catalysts supported on various alumina supports (θ-, δ-, κ-, η-, and γ-Al2O3) were prepared and the effect of the crystalline phases of the supports on the catalytic performance in methane combustion was investigated. Among the catalysts examined, the PdO/θ-Al2O3 catalyst, which showed the lowest reduction temperature in the temperature-programmed reduction of methane and the highest oxygen capacity in methane pulse experiments, exhibited the highest CH4 conversion and stability for methane combustion. However, all the catalysts were deactivated because of the growth of PdO particles and strong adsorption of water vapor.

Effect of pyrolysis parameters on yield and composition of gaseous products from activated sludge: towards sustainable biorefinery

Pyrolysis of activated sludge from sewage treatment was investigated in the presence and absence of silica and sand under varying conditions (temperature and retention time) in a fixed bed reactor. The presence of silica and sand had a significant impact on the amount of hydrogen and methane generated under the conditions studied, with both of these substances causing a significant reduction in hydrogen and methane yields compared to those obtained in the absence of these substances. The maximum yield of hydrogen was observed under the following conditions: no silica/sand, 1,073 K, 180 min. Maximum methane yield was observed to be under the following conditions: no silica/sand, 1,073 K, 180 min.

Antibiotic treatment of constipation-predominant irritable bowel syndrome.

The antibiotic rifaximin is used to treat non-constipated irritable bowel syndrome (IBS). Methane production is associated with constipation and its severity in constipation-predominant IBS (C-IBS). A previous retrospective study suggested that rifaximin and neomycin was superior to neomycin alone in improving symptoms in methane-positive subjects. To determine the effectiveness of neomycin alone or with rifaximin in improving symptoms in methane-positive C-IBS subjects. A double-blind, randomized, placebo-controlled trial was performed from 2010 to 2013 at three tertiary care centers. Subjects aged 18-65 with C-IBS (Rome II criteria) and breath methane (>3ppm) meeting the inclusion and exclusion criteria were recruited. Subjects completed a baseline symptom questionnaire rating the severity of abdominal and bowel symptoms on a visual analog scale and were randomized to receive neomycin and placebo or neomycin and rifaximin for 14 days. Symptom severity was assessed by weekly questionnaire for 2weeks of therapy and 4 additional weeks of follow-up. Thirty-one subjects (16 neomycin and placebo, 15 neomycin and rifaximin) were included in the intention-to-treat analysis. Constipation severity was significantly lower in the neomycin and rifaximin group (28.6±30.8) compared to neomycin alone (61.2±24.1) (P=0.0042), with greater improvement in constipation (P=0.007), straining (P=0.017) and bloating (P=0.020), but not abdominal pain. In the neomycin and rifaximin group, subjects with methane <3ppm after treatment reported significantly lower constipation severity (30.5±21.8) than subjects with persistent methane (67.2±32.1) (P=0.020). Rifaximin plus neomycin is superior to neomycin alone in improving multiple C-IBS symptoms. This effect is predicted by a reduction in breath methane.

Efficacy of different essential oils in modulating rumen fermentation in vitro using buffalo rumen liquor

Aim: Present study was conducted to examine the modulatory effect of different essential oils on rumen fermentation pattern in vitro using wheat straw based diet (concentrate: wheat straw 50:50). Materials and Methods: Four essential oils i.e. cinnamon, garlic, oregano and rosemary oils were tested at concentration of 0, 30, 300 and 600 mg/litre (ppm) of total culture fluid using in vitro gas production technique. Total gas production, methane production, nutrient degradability, volatile fatty acid (VFA) production and ammonia nitrogen concentration were studied in vitro using buffalo rumen liquor. Results: Results indicated that all four essential oils decreased gas production significantly (P<0.05) at 600ppm concentration. However, in case of garlic oil, 300 ppm concentration was also found to be effective in decreasing total gas production. Reduction in methane production was found maximum (P<0.05) at higher doses in most of the oils. Maximum reduction in methane was noticed with garlic oil at 600ppm dose. Ammonia-N concentration was also decreased significantly (P<0.05) with essential oils and was found minimum with oregano oil at 600 ppm dose. Partition factor was found to be significantly (P<0.05) higher in 600 ppm concentration of garlic and oregano oil. The degradability of dry matter decreased significantly with higher concentration of essential oil in most of treatment combinations.

Evaluation of aviation NOx-induced radiative forcings for 2005 and 2050

Aviation NOx emissions lead to the production of ozone (O3) and an OH increase in the troposphere and lower stratosphere. This OH increase results in a reduction of methane (CH4) which causes a longer-term reduction in O3 concentrations and lower stratospheric water vapor (SWV). Here we report new evaluations of a more comprehensive suite of aviation NOx-induced steady-state radiative forcing (RF) for 2006 aviation NOx emissions and for two different projections of 2050 NOx emissions and compare them with previously published analyses of aviation NOx-induced steady-state RFs. To do so, we evaluate the aviation NOx-induced steady-state RFs using the three-dimensional (3-D) global climate-chemistry Community Atmosphere Model (CAM), CAM4Chem. Moreover, we determine time dependent (transient) RFs for 2005 and the two 2050 emission scenarios by utilizing a parameterization based on specific RFs (steady-state RFs per unit of NOx emission) calculated in the 3-D model simulations, time-dependent NOx emissions data, and considering the lifetime of the perturbed species. For aviation NOx-induced effects we find that the net transient RFs differ from the linearly scaled steady-state RFs (specific steady-state RFs multiplied by NOx emissions) by +10%–36% for the different emission scenarios used in this study. These results indicate the importance of not using the transient and steady-state RF interchangeably, especially when comparing the aviation contribution in RF changes to contributions from other transportation sectors. Also, these results indicate that careful consideration is necessary when choosing whether to use the steady-state or transient RF when evaluating aviation NOx-induced RFs.

EVALUATION OF LACTICIN ADDITION ON GAS PRODUCTION KINETICS AND RUMEN METHANOGENESIS in Vitro

The present study was aimed to investigate the effect of a novel bacteriocin, i.e. lacticin 3147, ongas production kinetics and methane emission under in vitro rumen environment in two consecutiveexperiments. In experiment 1, either no or 10 µM of lacticin was added to hay or hay:concentrate (1:1,w/w) substrate. In experiment 2, the levels of lacticin additions were extended to 0, 10, 25 and 50 µM.Samples were incubated in three replicates in both experiments at 39oC for 24 h. Total gas productionand methane emission were measured during and after the incubation, respectively. Results revealedthat, in general, addition of lacticin had limited significant effects on gas production parameterscompared to control (without lacticin addition). Lacticin addition up to 50 µM did not significantlydecrease CH4 emission, although a tendency of methane reduction existed when lacticin was added at 25µM. Hay diet produced significantly less methane emission than that of hay:concentrate diet both inexperiment 1 and experiment 2 (P&lt;0.05). It can be concluded that lacticin addition up to 50 µM wasunable to decrease CH4 emission in vitro and therefore need to be tested further at higher concentrations.

Lipid biomarkers for anaerobic oxidation of methane and sulphate reduction in cold seep sediments of Nyegga pockmarks (Norwegian margin): discrepancies in contents and carbon isotope signatures

Distributions and carbon isotopic compositions of microbial lipid biomarkers were investigated in sediment cores from the G11 and G12 pockmarks in the Nyegga sector of the Storegga Slide on the mid-Norwegian margin to explore differences in depth zonation, type and carbon assimilation mode of anaerobic methane-oxidizing archaea (ANMEs) and associated sulphate-reducing bacteria responsible for anaerobic oxidation of methane (AOM) in these cold seep environments. While the G11 site is characterised by black reduced sediments colonized by gastropods and Siboglinidae tubeworms, the G12 site has black reduced sediments devoid of fauna but surrounded by a peripheral occurrence of gastropods and white filamentous microbial mats. At both sites, bulk sediments contained abundant archaeal and bacterial lipid biomarkers substantially depleted in 13C, consisting mainly of isoprenoidal hydrocarbons and dialkyl glycerol diethers, fatty acids and non-isoprenoidal monoalkylglycerol ethers. At the G11 site, down-core profiles revealed that lipid biomarkers were in maximum abundance from 10 cm depth to the core bottom at 16 cm depth, associated with δ13C values of −57 to −136‰. At the G12 site, by contrast, lipid biomarkers were in high abundance in the upper 5 cm sediment layer, associated with δ13C values of −43 to −133‰. This suggests that, as expected from the benthic fauna characteristics of the sites, AOM takes place mainly at depth in the G11 pockmark but just below the seafloor in the G12 pockmark. These patterns can be explained largely by variable fluid flow rates. Furthermore, at both sites, a dominance of ANME-2 archaea accompanied by their bacterial partners is inferred based on lipid biomarker distributions and carbon isotope signatures, which is in agreement with recently published DNA analyses for the G11 pockmark. However, the present data reveal high discrepancies in the contents and δ13C values for both archaeal and bacterial lipid profiles, implying the possible involvement of at least two distinct AOM-related microbial consortia at the inferred AOM depth zonation of G11 and G12 pockmark sediments. In both sediment cores, the δ13C profiles for most archaeal lipids suggest a direct assimilation of dissolved inorganic carbon (DIC) in addition to methane by ANMEs (chemoautotrophy); constant and highly depleted δ13C profiles for PMI:3, an archaeal lipid biomarker presumably related to ANME-2, suggest a direct assimilation of 13C-depleted methane-derived carbon via AOM (methanotrophy). Evidently, the common approach of investigating lipid biomarker contents and δ13C signatures in cold seep sediments does not suffice to precisely discriminate between the carbon assimilation mode for each ANME archaeal group and associated bacteria. Rather, this needs to be combined with further specific labelling studies including different carbon sources (methane carbon, methane-derived organic intermediates and DIC) in order to unravel the metabolic pathways of each microbial consortium involved in AOM (ANME-1 vs. ANME-2 vs. ANME-3 archaeal group and associated bacteria).

Influence of Albizia lebbeck Saponin and Its Fractions on In Vitro Gas Production Kinetics, Rumen Methanogenesis, and Rumen Fermentation Characteristics.

The present study was undertaken to investigate the effect of crude seed powder (CSP) and gross saponins extract (GSE) of seeds of Albizia lebbeck on antimicrobial activity by taking two Gram-positive (Staphylococcus aureus and Bacillus cereus), two Gram-negative (Escherichia coli and Salmonella Typhi) bacteria, and two fungi species (Aspergillus niger and Candida butyric) were taken at 25, 50, 100, 250, and 500 µg levels using agar well diffusion method. Zone of inhibition was increased with increasing of concentration of CSP and saponins which indicates that Gram-negative bacteria (E. coli), Gram-positive bacteria (B. cereus), and A. niger were significantly susceptible to inhibition. Another experiment was conducted to study the effect of GSE and saponins fraction A and B of A. lebbeck supplementation at 6% on DM basis on methane production and other rumen fermentation parameters using in vitro gas production test, by taking three different type diets, that is, high fiber diet (D1, 60R : 40C), medium fiber diet (D2, 50R : 50C), and low fiber diet (D3, 40R : 60C). Significant (P ≤ 0.05) increase was seen in IVDMD, methane production; however ammonia nitrogen concentration decreased as compared to control. The methane production was reduced in a range between 12 and 49% by saponin supplemented diets except in case of GSE in D2. Sap A showed the highest methane reduction per 200 mg of truly digested substrate (TDS) than other treatment groups. Results in relation with quantification of methanogens and protozoa by qPCR indicated the decreasing trend with saponins of A. lebbek in comparison with control except total methanogen quantified using mcr-A based primer.

Microbial communities in uranium mine tailings and mine water sediment from Jaduguda U mine, India: A culture independent analysis

Microbial diversity within uranium mine tailings and mine water sediment from the Jaduguda uranium mine, India was characterized by metagenome-derived 16S rRNA gene clone libraries. Samples from fresh tailings (JFT244), abandoned (vegetated) tailings (JOT245) and mine water sediment (J1-5) having wide ranges of pH (5.7 to 10.4), nitrogen, phosphorus and organic carbon [150–5700 ppm, 800–9100 ppm and 0.18–6.5% (w/w)] and elevated metals (Ni, Cu, Zn and U) were used to explore the inhabitant bacterial and archaeal community structures. Consistent to the sample's physicochemical properties, up to four orders of magnitude variation in bacterial CFU counts was observed. The data showed that with increasing metal and decreasing nutrient (organic C, N, P, etc.) contents, microbial diversity indices decrease within the samples. Culture-independent analyses revealed predominance of phyla Proteobacteria and/or Acidobacteria within the samples along with members of Actinobacteria, Cyanobacteria, Chloroflexi, Genera incertae sedis OP10, Firmicutes and Planctomycete as relatively minor groups. Abundance of Crenarchaeota in tailings samples and Euryachaeota in mine water sediment was noted. Diversity of dissimilatory sulfate reductase gene (dsr) was studied. Putative metabolic properties as derived from taxonomy and phylogenetic lineages indicated presence of chemolithotrophic and heteotrophic aerobic and anaerobic organisms capable of nitrogen fixation, nitrate reduction and biogeochemical cycling of metals, sulfur and methane. The data indicated that indigenous microbial populations are capable of maintaining self-sustenance in these highly hazardous environments and possess catalytic potential for their use in in situ bioremediation.

Microbial activity and carbonate isotope signatures as a tool for identification of spatial differences in methane advection: a case study at the Pacific Costa Rican margin

Abstract. The forearc of the convergent margin offshore Costa Rica is a region characterized by strong advection of methane-charged fluids causing the formation of ubiquitous cold seeps (mounds). Presented here are the first measurements of microbial anaerobic oxidation of methane (AOM) and sulfate reduction (SR) rates in sediments from two mounds (11 and 12), applying radiotracer techniques in combination with numerical modelling. In addition, analysis of microbial, methane-dependent carbonate δ18O, δ13C, and 87Sr / 86Sr signatures constrained the origin of the carbonate-precipitating fluid. Average rates of microbial activities differed by a factor of ~5 to 6 between Mound 11 (AOM 140.71 (±40.84 SD) mmol m−2 d−1, SR 117.25 (±82.06 SD) mmol m−2 d−1) and Mound 12 (AOM 22.37 (±0.85 SD) mmol m−2 d−1, SR 23.99 (±5.79 SD) mmol m−2 d−1). Modelling results yielded upward fluid advection velocities of 200 cm yr−1 at Mound 11 and 15 cm yr−1 at Mound 12. Analysis of oxygen and carbon isotope variations of authigenic carbonates from the two locations revealed more enriched values for Mound 11 (δ18O : 3.18 to 6.15‰; δ13C: −14.14 to −29.56‰) compared to Mound 12 (δ18O : 3.09 to 4.48‰; δ13C : −39.53 to −48.98‰). The variation of carbonate 87Sr / 86Sr indicated considerable admixture of deep-source fluid at Mound 11, while seawater 87Sr / 86Sr characteristics prevailed at Mound 12 during precipitation. The present study is in accordance with previous work supporting considerable differences of methane flux between the two mounds. It also strengthens the hypothesis of a dominant deep fluid source with thermogenic methane at Mound 11 versus a shallow source of biogenic methane at Mound 12. The results demonstrate that measurements of methane-driven microbial activity in combination with numerical modelling are a valid tool for constraining recent methane fluxes in the study area. In addition, the analysis of methane-derived authigenic carbonates provides an independent line of evidence for long-term fluid contribution to the porewater chemistry of shallow sediments in the study area.