Distribution and diversity of autotrophic bacteria in groundwater systems based on the analysis of RubisCO genotypes

A molecular approach, based on the detection of ribulose-1,5-bisphosphate carboxylase/oxygenase (RubisCO) large subunit genes, was applied to investigate the distribution and diversity of autotrophic bacteria in groundwater systems. DNA extracts from 48 sampling stations, including a variety of pristine and polluted, shallow and deep-subsurface groundwater samples obtained from Germany and Austria, served as a template for the PCR amplification of form I (cbbL) and form II (cbbM) large subunit RubisCO genes. The majority of the samples (>80%) contained two different forms of RubisCO. In 17 samples, all three forms of RubisCO were identified. PCR products from four selected groundwater habitats containing all three forms of RubisCO were used to construct clone libraries. Based on restriction fragment length polymorphism (RFLP) analysis, 109 RubisCO-clone-inserts were subjected to sequencing and phylogenetic analysis. With the exception of a form IA RubisCO sequence cluster obtained from deep subsurface samples, which was identical to the RubisCO genes described for Ralstonia metallidurans CH34, most sequences were distantly related to a variety of RubisCO species in chemolithoautotrophic Proteobacteria. Several sequences occurred in isolated lineages. These findings suggest that autotrophic bacteria with the capability to assimilate CO₂ via the Calvin Cycle pathway are widespread inhabitants of groundwater systems.     

Rates of Microbial Metabolism in Deep Coastal Plain Aquifers

Rates of microbial metabolism in deep anaerobic aquifers of the Atlantic coastal plain of South Carolina were investigated by both microbiological and geochemical techniques. Rates of [2-¹⁴C]acetate and [U-¹⁴C]glucose oxidation as well as geochemical evidence indicated that metabolic rates were faster in the sandy sediments composing the aquifers than in the clayey sediments of the confining layers. In the sandy aquifer sediments, estimates of the rates of CO₂ production (millimoles of CO₂ per liter per year) based on the oxidation of [2-¹⁴C] acetate were 9.4 × 10⁻³ to 2.4 × 10⁻¹ for the Black Creek aquifer, 1.1 × 10⁻² for the Middendorf aquifer, and <7 × 10⁻⁵ for the Cape Fear aquifer. These estimates were at least 2 orders of magnitude lower than previously published estimates that were based on the accumulation of CO₂ in laboratory incubations of similar deep subsurface sediments. In contrast, geochemical modeling of groundwater chemistry changes along aquifer flowpaths gave rate estimates that ranged from 10⁻⁴ to 10⁻⁶ mmol of CO₂ per liter per year. The age of these sediments (ca. 80 million years) and their organic carbon content suggest that average rates of CO₂ production could have been no more than 10⁻⁴ mmol per liter per year. Thus, laboratory incubations may greatly overestimate the in situ rates of microbial metabolism in deep subsurface environments. This has important implications for the use of laboratory incubations in attempts to estimate biorestoration capacities of deep aquifers. The rate estimates from geochemical modeling indicate that deep aquifers are among the most oligotrophic aquatic environments in which there is ongoing microbial metabolism.     

Chemolithoautotrophy in the marine,magnetotactic bacterial strains MV-1 and MV-2

Magnetite-producing magnetotactic bacteria collected from the oxic–anoxic transition zone of chemically stratified marine environments characterized by O₂/H₂S inverse double gradients, contained internal S-rich inclusions resembling elemental S globules, suggesting they oxidize reduced S compounds that could support autotrophy. Two strains of marine magnetotactic bacteria, MV-1 and MV-2, isolated from such sites grew in O₂-gradient media with H₂S or thiosulfate (S₂O₃^2–) as electron sources and O₂ as electron acceptor or anaerobically with S₂O₃^2– and N₂O as electron acceptor, with bicarbonate (HCO₃^–)/CO₂ as sole C source. Cells grown with H₂S contained S-rich inclusions. Cells oxidized S₂O₃^2– to sulfate (SO₄^2–). Both strains grew microaerobically with formate. Neither grew microaerobically with tetrathionate (S₄O₆^2–), methanol, or Fe²⁺ as FeS, or siderite (FeCO₃). Growth with S₂O₃^2– and radiolabeled ¹⁴C-HCO₃^– showed that cell C was derived from HCO₃^–/CO₂. Cell-free extracts showed ribulose 1,5-bisphosphate carboxylase/oxygenase (RubisCO) activity. Southern blot analyses indicated the presence of a form II RubisCO (cbbM) but no form I (cbbL) in both strains. cbbM and cbbQ, a putative post-translational activator of RubisCO, were identified in MV-1. MV-1 and MV-2 are thus chemolithoautotrophs that use the Calvin–Benson–Bassham pathway. cbbM was also identified in Magnetospirillum magnetotacticum. Thus, magnetotactic bacteria at the oxic–anoxic transition zone of chemically stratified aquatic environments are important in C cycling and primary productivity.     

Enzymatic and Genetic Characterization of Carbon and Energy Metabolisms by Deep-Sea Hydrothermal Chemolithoautotrophic Isolates of Epsilonproteobacteria

The carbon and energy metabolisms of a variety of cultured chemolithoautotrophic Epsilonproteobacteria from deep-sea hydrothermal environments were characterized by both enzymatic and genetic analyses. All the Epsilonproteobacteria tested had all three key reductive tricarboxylic acid (rTCA) cycle enzymatic activities—ATP-dependent citrate lyase, pyruvate:ferredoxin oxidoreductase, and 2-oxoglutarate:ferredoxin oxidoreductase—while they had no ribulose 1,5-bisphosphate carboxylase (RubisCO) activity, the key enzyme in the Calvin-Benson cycle. These results paralleled the successful amplification of the key rTCA cycle genes aclB, porAB, and oorAB and the lack of success at amplifying the form I and II RubisCO genes, cbbL and cbbM. The combination of enzymatic and genetic analyses demonstrates that the Epsilonproteobacteria tested use the rTCA cycle for carbon assimilation. The energy metabolisms of deep-sea Epsilonproteobacteria were also well specified by the enzymatic and genetic characterization: hydrogen-oxidizing strains had evident soluble acceptor:methyl viologen hydrogenase activity and hydrogen uptake hydrogenase genes (hyn operon), while sulfur-oxidizing strains lacked both the enzyme activity and the genes. Although the energy metabolism of reduced sulfur compounds was not genetically analyzed and was not fully clarified, sulfur-oxidizing Epsilonproteobacteria showed enzyme activity of a potential sulfite:acceptor oxidoreductase for a direct oxidation pathway to sulfate but no activity of AMP-dependent adenosine 5′-phosphate sulfate reductase for a indirect oxidation pathway. No activity of thiosulfate-oxidizing enzymes was detected. The enzymatic and genetic characteristics described here were consistent with cellular carbon and energy metabolisms and suggest that molecular tools may have great potential for in situ elucidation of the ecophysiological roles of deep-sea Epsilonproteobacteria.     

长期施肥对稻田土壤固碳功能菌群落结构和数量的影响

微生物固碳在减缓全球气候变化、实现人类可持续发展方面具有重要的意义,通过揭示长期不同施肥制度对土壤固碳细菌的影响规律,可以为我国稻田土壤科学施肥,稻田固碳和温室气体减排的共轭双赢作用提供重要的理论依据。以湖南宁乡国家级稻田肥力变化长期定位试验为平台,采用PCR-克隆测序和实时荧光定量(Real-time)PCR技术,研究不施肥(CK),氮磷钾肥（NPK）和秸秆还田（NPKS）3种长期施肥制度对稻田土壤固碳细菌群落结构及数量的影响。通过分析固碳细菌cbbL基因文库发现,长期施肥导致土壤固碳细菌种群结构产生了明显差异,NPK和NPKS处理中兼性自养固碳菌群落优势增加而严格自养固碳菌生长受到抑制。LUBSHUFF软件统计分析显示cbbL基因文库在CK、NPK及NPKS处理间均存在显著性差异。 3种施肥处理的稻田土壤细菌cbbL基因拷贝数为3.35?108 —5.61?108每克土,施肥后,土壤细菌cbbL基因数量增加,其中NPKS处理cbbL数量最多,是CK处理的1.5倍左右。稀疏曲线则显示长期施化肥导致细菌cbbL基因多样性高于NPKS,而NPKS高于CK。上述结果表明了长期施肥对土壤固碳细菌群落结构,多样性及数量均有显著的影响。本研究结果可为深入探讨稻田土壤微生物固碳潜力及其影响机理提供有力的依据。     

基于16S rRNA和RubisCO基因对嗜酸硫杆菌的系统发育及多样性北大核心CSCD

【目的】明确不同地理来源的Acidithiobacillus spp.种群是否表现出显著的地域性和异域物种形成;为了解微生物谱系地理、多样性维持机制和微生物分子地理学提供基础数据。【方法】采用16S r RNA基因、核酮糖-1,5-二磷酸羧化酶/加氧酶(Rubis CO)功能基因序列同源性分析构建相应的系统发育树,分析Acidithiobacillus spp.种群的遗传多样性。【结果】从3个不同的地域分离到35株菌聚为5大类群,其中菌株YNTR4-15可能是铁氧化细菌(Leptspirillum ferrooxidans),菌株HBDY3-3被鉴定为另一铁氧化细菌(Leptospirillum ferrodiazotrophum);有4株可能是Acidithiobacillus ferrivorans;6株是Acidithiobacillus ferridurans,其余菌株均被鉴定为Acidithiobacilus ferrooxidan。对26株代表性菌株的Rubis CO I型cbb L基因和II型cbb M基因的分析,发现19株菌具有双拷贝cbb L基因,分别为cbb L1和cbb L2基因;7株菌只检测到了cbb L1。cbb L1和cbb L2基因都有3个序列型;而cbb M基因是单拷贝。Rubis CO基因的密码子偏爱性不强。【结论】分离自3个地域的菌株16S r RNA/Rubis CO基因存在序列差异,Acidithiobacillus spp.种群存在显著的遗传多样性。嗜酸硫杆菌分离菌株基于16S r RNA基因的系统发育树和Rubis CO基因的发育树不一致。     

Long-term field fertilization alters the diversity of autotrophic bacteria based on the ribulose-1,5-biphosphate carboxylase/oxygenase (RubisCO) large-subunit genes in paddy soil

Carbon dioxide (CO₂) assimilation by autotrophic bacteria is an important process in the soil carbon cycle with major environmental implications. The long-term impact of fertilizer on CO₂ assimilation in the bacterial community of paddy soils remains poorly understood. To narrow this knowledge gap, the composition and abundance of CO₂-assimilating bacteria were investigated using terminal restriction fragment length polymorphism and quantitative PCR of the cbbL gene [that encodes ribulose-1,5-biphosphate carboxylase/oxygenase (RubisCO)] in paddy soils. Soils from three stations in subtropical China were used. Each station is part of a long-term fertilization experiment with three treatments: no fertilizer (CK), chemical fertilizers (NPK), and NPK combined with rice straw (NPKM). At all of the stations, the cbbL-containing bacterial communities were dominated by facultative autotrophic bacteria such as Rhodopseudomonas palustris, Bradyrhizobium japonicum, and Ralstonia eutropha. The community composition in the fertilized soil (NPK and NPKM) was distinct from that in unfertilized soil (CK). The bacterial cbbL abundance (3–8?×?10⁸ copies g soil^?1) and RubisCO activity (0.40–1.76 nmol CO₂ g soil^?1 min^?1) in paddy soils were significantly positively correlated, and both increased with the addition of fertilizer. Among the measured soil parameters, soil organic carbon and pH were the most significant factors influencing the community composition, abundance, and activity of the cbbL-containing bacteria. These results suggest that long-term fertilization has a strong impact on the activity and community of cbbL-containing bacterial populations in paddy soils, especially when straw is combined with chemical fertilizers.     

Application of targeted metagenomics to explore abundance and diversity of CO2-fixing bacterial community using cbbL gene from the rhizosphere of Arachis hypogaea

Sequestration of CO₂ by autotrophic bacteria is a key process of biogeochemical carbon cycling in soil ecosystem. Rhizosphere is a rich niche of microbial activity and diversity, influenced by change in atmospheric CO₂. Structural changes in rhizosphere composition influence microbial communities and the nutrient cycling. In the present study, the bacterial diversity and population dynamics were established using cbbL and 16S rRNA gene targeted metagenomics approach from the rhizosphere of Arachis hypogaea. A total of 108 cbbL clones were obtained from the rhizospheric soil which revealed predominance of cbbL sequences affiliated to Rhizobium leguminosarum, Bradyrhizobium sp., Sinorhizobium meliloti, Ochrobactrum anthropi and a variety of uncultured cbbL harboring bacteria. The 16S rRNA gene clone library exhibited the dominance of Firmicutes (34.4%), Proteobacteria (18.3%), Actinobacteria (17.2%) and Bacteroidetes (16.1%). About 43% nucleotide sequences of 16S rRNA gene clone library were novel genera which showed < 95% homology with published sequences. Gene copy number of cbbL and 16S rRNA genes, determined by quantitative real‐time PCR (qRT PCR), was 9.38 ± 0.75 × 10⁷ and 5.43 ± 0.79 × 10⁸ (per g dry soil), respectively. The results exhibited bacterial community structure with high bacterial diversity and abundance of CO₂‐fixing bacteria, which can be explored further for their role in carbon cycling, sustainable agriculture and environment management.     

Abundance and Diversity of CO<Subscript>2</Subscript>-fixing Bacteria in Grassland Soils Close to Natural Carbon Dioxide Springs

Gaseous conditions at natural CO₂ springs (mofettes) affect many processes in these unique ecosystems. While the response of plants to extreme and fluctuating CO₂ concentrations ([CO₂]) is relatively well documented, little is known on microbial life in mofette soil. Therefore, it was the aim of this study to investigate the abundance and diversity of CO₂-fixing bacteria in grassland soils in different distances to a natural carbon dioxide spring. Samples of the same soil type were collected from the Stavešinci mofette, a natural CO₂ spring which is known for very pure CO₂ emissions, at different distances from the CO₂ releasing vents, at locations that clearly differed in soil CO₂ efflux (from 12.5 to over 200 μmol CO₂ m⁻² s⁻¹ yearly average). Bulk and rhizospheric soil samples were included into analyses. The microbial response was followed by a molecular analysis of cbbL genes, encoding for the large subunit of RubisCO, a carboxylase which is of crucial importance for C assimilation in chemolitoautotrophic microbes. In all samples analyzed, the “red-like” type of cbbL genes could be detected. In contrast, the “green-like” type of cbbL could not be measured by the applied technique. Surprisingly, a reduction of “red-like” cbbL genes copies was observed in bulk soil and rhizosphere samples from the sites with the highest CO₂ concentrations. Furthermore, the diversity pattern of “red-like” cbbL genes changed depending on the CO₂ regime. This indicates that only a part of the autotrophic CO₂-fixing microbes could adapt to the very high CO₂ concentrations and adverse life conditions that are governed by mofette gaseous regime. Urška Videmšek, Alexandra Hagn, Michael Schloter, and Dominik Vodnik contributed equally to this study.     

RubisCO Gene Clusters Found in a Metagenome Microarray from Acid Mine Drainage

The enzyme responsible for carbon dioxide fixation in the Calvin cycle, ribulose-1,5-bisphosphate carboxylase/oxygenase (RubisCO), is always detected as a phylogenetic marker to analyze the distribution and activity of autotrophic bacteria. However, such an approach provides no indication as to the significance of genomic content and organization. Horizontal transfers of RubisCO genes occurring in eubacteria and plastids may seriously affect the credibility of this approach. Here, we presented a new method to analyze the diversity and genomic content of RubisCO genes in acid mine drainage (AMD). A metagenome microarray containing 7,776 large-insertion fosmids was constructed to quickly screen genome fragments containing RubisCO form I large-subunit genes (cbbL). Forty-six cbbL-containing fosmids were detected, and six fosmids were fully sequenced. To evaluate the reliability of the metagenome microarray and understand the microbial community in AMD, the diversities of cbbL and the 16S rRNA gene were analyzed. Fosmid sequences revealed that the form I RubisCO gene cluster could be subdivided into form IA and IB RubisCO gene clusters in AMD, because of significant divergences in molecular phylogenetics and conservative genomic organization. Interestingly, the form I RubisCO gene cluster coexisted with the form II RubisCO gene cluster in one fosmid genomic fragment. Phylogenetic analyses revealed that horizontal transfers of RubisCO genes may occur widely in AMD, which makes the evolutionary history of RubisCO difficult to reconcile with organismal phylogeny.     

Depth-Resolved Quantification of Anaerobic Toluene Degraders and Aquifer Microbial Community Patterns in Distinct Redox Zones of a Tar Oil Contaminant Plume

Microbial degradation is the only sustainable component of natural attenuation in contaminated groundwater environments, yet its controls, especially in anaerobic aquifers, are still poorly understood. Hence, putative spatial correlations between specific populations of key microbial players and the occurrence of respective degradation processes remain to be unraveled. We therefore characterized microbial community distribution across a high-resolution depth profile of a tar oil-impacted aquifer where benzene, toluene, ethylbenzene, and xylene (BTEX) degradation depends mainly on sulfate reduction. We conducted depth-resolved terminal restriction fragment length polymorphism fingerprinting and quantitative PCR of bacterial 16S rRNA and benzylsuccinate synthase genes (bssA) to quantify the distribution of total microbiota and specific anaerobic toluene degraders. We show that a highly specialized degrader community of microbes related to known deltaproteobacterial iron and sulfate reducers (Geobacter and Desulfocapsa spp.), as well as clostridial fermenters (Sedimentibacter spp.), resides within the biogeochemical gradient zone underneath the highly contaminated plume core. This zone, where BTEX compounds and sulfate—an important electron acceptor—meet, also harbors a surprisingly high abundance of the yet-unidentified anaerobic toluene degraders carrying the previously detected F1-cluster bssA genes (C. Winderl, S. Schaefer, and T. Lueders, Environ. Microbiol. 9:1035-1046, 2007). Our data suggest that this biogeochemical gradient zone is a hot spot of anaerobic toluene degradation. These findings show that the distribution of specific aquifer microbiota and degradation processes in contaminated aquifers are tightly coupled, which may be of value for the assessment and prediction of natural attenuation based on intrinsic aquifer microbiota.     

Microbial Community in High Arsenic Shallow Groundwater Aquifers in Hetao Basin of Inner Mongolia,China

A survey was carried out on the microbial community of 20 groundwater samples (4 low and 16 high arsenic groundwater) and 19 sediments from three boreholes (two high arsenic and one low arsenic boreholes) in a high arsenic groundwater system located in Hetao Basin, Inner Mongolia, using the 454 pyrosequencing approach. A total of 233,704 sequence reads were obtained and classified into 12–267 operational taxonomic units (OTUs). Groundwater and sediment samples were divided into low and high arsenic groups based on measured geochemical parameters and microbial communities, by hierarchical clustering and principal coordinates analysis. Richness and diversity of the microbial communities in high arsenic sediments are higher than those in high arsenic groundwater. Microbial community structure was significantly different either between low and high arsenic samples or between groundwater and sediments. Acinetobacter, Pseudomonas, Psychrobacter and Alishewanella were the top four genera in high arsenic groundwater, while Thiobacillus, Pseudomonas, Hydrogenophaga, Enterobacteriaceae, Sulfuricurvum and Arthrobacter dominated high arsenic sediments. Archaeal sequences in high arsenic groundwater were mostly related to methanogens. Biota-environment matching and co-inertia analyses showed that arsenic, total organic carbon, SO₄^2-, SO₄^2-/total sulfur ratio, and Fe²⁺ were important environmental factors shaping the observed microbial communities. The results of this study expand our current understanding of microbial ecology in high arsenic groundwater aquifers and emphasize the potential importance of microbes in arsenic transformation in the Hetao Basin, Inner Mongolia.     

Expression of the cbbLcbbS and cbbM genes and distinct organization of the cbb Calvin cycle structural genes of Rhodobacter capsulatus

Rhodobacter capsulatus fixes CO₂ via the Calvin reductive pentose phosphate pathway and, like some other nonsulfur purple bacteria, is known to synthesize two distinct structural forms of ribulose 1,5-bisphosphate carboxylase/oxygenase (RubisCO). Cosmid clones that hybridized to form I (cbbLcbbS) and form II (cbbM) RubisCO gene probes were isolated from a genomic library of R. capsulatus strain SB1003. Southern blotting and hybridization analysis with gene-specific probes derived from Rhodobacter sphaeroides revealed that R. capsulatus cbbM is clustered with genes encoding other enzymes of the Calvin cycle, including fructose 1,6/sedoheptulose 1,7-bisphosphatase (cbbF), phosphoribulokinase (cbbP), transketolase (cbbT), glyceraldehyde-3-phosphate dehydrogenase (cbbG), and fructose 1,6-bisphosphate aldolase (cbbA), as well as a gene (cbbR) encoding a divergently transcribed LysR-type regulatory protein. Surprisingly, a cosmid clone containing the R. capsulatus form I RubisCO genes (cbbL and cbbS) failed to hybridize to the other cbb structural gene probes, unlike the situation with the closely related organism R. sphaeroides. The form I and form II RubisCO genes were cloned into pUC-derived vectors and were expressed in Escherichia coli to yield active recombinant enzyme in each case. Complementation of a RubisCO-deletion strain of R. sphaeroides to photosynthetic growth by R. capsulatus cbbLcbbS or cbbM was achieved using the broad host-range vector, pRK415, and R. sphaeroides expression vector pRPS-1. Received: 6 June 1995 / Accepted: 29 September 1995     

Bacterial and Archaeal Phylogenetic Diversity of a Cold Sulfur-Rich Spring on the Shoreline of Lake Erie,Michigan

Studies of sulfidic springs have provided new insights into microbial metabolism, groundwater biogeochemistry, and geologic processes. We investigated Great Sulphur Spring on the western shore of Lake Erie and evaluated the phylogenetic affiliations of 189 bacterial and 77 archaeal 16S rRNA gene sequences from three habitats: the spring origin (11-m depth), bacterial-algal mats on the spring pond surface, and whitish filamentous materials from the spring drain. Water from the spring origin water was cold, pH 6.3, and anoxic (H₂, 5.4 nM; CH₄, 2.70 μM) with concentrations of S²⁻ (0.03 mM), SO₄²⁻ (14.8 mM), Ca²⁺ (15.7 mM), and HCO₃⁻ (4.1 mM) similar to those in groundwater from the local aquifer. No archaeal and few bacterial sequences were >95% similar to sequences of cultivated organisms. Bacterial sequences were largely affiliated with sulfur-metabolizing or chemolithotrophic taxa in Beta-, Gamma-, Delta-, and Epsilonproteobacteria. Epsilonproteobacteria sequences similar to those obtained from other sulfidic environments and a new clade of Cyanobacteria sequences were particularly abundant (16% and 40%, respectively) in the spring origin clone library. Crenarchaeota sequences associated with archaeal-bacterial consortia in whitish filaments at a German sulfidic spring were detected only in a similar habitat at Great Sulphur Spring. This study expands the geographic distribution of many uncultured Archaea and Bacteria sequences to the Laurentian Great Lakes, indicates possible roles for epsilonproteobacteria in local aquifer chemistry and karst formation, documents new oscillatorioid Cyanobacteria lineages, and shows that uncultured, cold-adapted Crenarchaeota sequences may comprise a significant part of the microbial community of some sulfidic environments.Cold, sulfidic springs upwelling into caves (1, 16-19) or exposed at the land surface (14, 15, 31, 39, 47, 50, 51) have recently been shown to harbor unique microbial communities, reflective of the aqueous sulfur chemistry of the upwelling groundwater or of unique cave conditions. Within these spring and cave ecosystems, new and unique Epsilonproteobacteria 16S rRNA gene sequences associated with a limited number of cultured isolates that carry out oxidation of sulfur compounds have been discovered (7). The abundance of Epsilonproteobacteria sequences in these settings and associated biogeochemical research have led to new interest in the role of microbially mediated sulfuric acid speleogenesis as an important limestone dissolution process that may contribute to the development of karst features in limestone bedrock (19). Additionally, in streamlets from sulfidic springs, unique symbioses between uncultured Euryarchaeota, Crenarchaeota, and Epsilonproteobacteria spp. that grow in whitish, macroscopically visible filaments have been described (31, 51). Sulfur cycling was identified as a major means of energy production and maintenance of microbial communities in cold, saline, perennial springs emanating from permafrost in the Arctic (47). Studies of cold, sulfidic springs have therefore provided new insights into microbial metabolism, ecology, and evolution as well as groundwater biogeochemistry and geologic processes.All studies of sulfidic springs to date have focused on terrestrial landscapes typically associated with limestone (CaCO₃) bedrock. Limestone is one of several carbonate sedimentary rocks deposited by ancient seas, which may contain significant amounts of gypsum (CaSO₄·2H₂O) as well as pockets of hydrocarbon deposits, both a source of sulfur. Water that moves for long distances through such rocks evolves through sequential dissolution and precipitation reactions to a geochemistry that bears little resemblance to freshwater. SO₄²⁻ becomes available for microbial reduction to sulfide in aquifer zones where conditions are appropriate. Where spring waters rich in CaCO₃, CO₂, and sulfide emerge at the surface, carbonate deposition and microbially mediated sulfide oxidation occur. These processes result in tufa deposits and the whitish crusts often noted in sulfidic spring outflows (12, 13). Carbonate bedrock underlies large portions of the lower Laurentian Great Lakes. Caves in contact with lake water occur on islands in Lake Erie and along the Bruce Peninsula in Ontario, Canada. A cold, sulfidic spring is located in Ancaster, Ontario, about 5 km from the Lake Ontario shoreline (13). Recently, plumes of high-conductivity sulfidic groundwater, surrounded by whitish filamentous materials and variously colored microbial mats, were reported to occur at a 93-m depth in Lake Huron (2, 49). However, there have been few molecular surveys of Bacteria or Archaea in any Great Lakes environment, and no reports focusing on the molecular phylogenetic diversity of microorganisms associated with these Great Lakes sulfidic environments.Along the western shoreline of Lake Erie and within Monroe County, MI, sinkholes and springs are abundant in the Silurian-Devonian carbonate bedrock, and Ca²⁺ and Mg²⁺ with SO₄²⁻ or HCO₃⁻ dominate groundwater composition (43). In some areas of Monroe County, sulfide in groundwater prohibits its use as a drinking water source. Great Sulphur Spring (GSS) was first described by Sherzer in 1900 (53) and was named for its sulfide-rich water. The spring arises from Silurian-Devonian carbonate bedrock within 0.5 km of the Lake Erie shoreline and is a convenient location for accessing sulfide-rich groundwater and for exploring potential interactions between groundwater and lake water. As part of a larger study of nearshore groundwater interactions with Lake Erie (27) and to better understand the potential role of microorganisms in sulfur chemistry of nearshore groundwater, we evaluated the chemistry and bacterial and archaeal 16S rRNA gene diversity of GSS. Our study documents a unique microbial community for the Laurentian Great Lakes, comprised in large part of new lineages and uncultivated members of the Archaea, Deltaproteobacteria, Epsilonproteobacteria, and Cyanobacteria. These sequences suggest a microbial community structure driven by (possibly H₂S-based) carbon fixation and chemolithotrophy of reduced compounds such as H₂, H₂S, or reduced nitrogen compounds, all consistent with spring geochemistry.     

Functional metagenomic selection of ribulose 1, 5‐bisphosphate carboxylase/oxygenase from uncultivated bacteria

Ribulose 1,5‐bisphosphate carboxylase/oxygenase (RubisCO) is a critical yet severely inefficient enzyme that catalyses the fixation of virtually all of the carbon found on Earth. Here, we report a functional metagenomic selection that recovers physiologically active RubisCO molecules directly from uncultivated and largely unknown members of natural microbial communities. Selection is based on CO₂‐dependent growth in a host strain capable of expressing environmental deoxyribonucleic acid (DNA), precluding the need for pure cultures or screening of recombinant clones for enzymatic activity. Seventeen functional RubisCO‐encoded sequences were selected using DNA extracted from soil and river autotrophic enrichments, a photosynthetic biofilm and a subsurface groundwater aquifer. Notably, three related form II RubisCOs were recovered which share high sequence similarity with metagenomic scaffolds from uncultivated members of the Gallionellaceae family. One of the Gallionellaceae RubisCOs was purified and shown to possess CO₂/O₂ specificity typical of form II enzymes. X‐ray crystallography determined that this enzyme is a hexamer, only the second form II multimer ever solved and the first RubisCO structure obtained from an uncultivated bacterium. Functional metagenomic selection leverages natural biological diversity and billions of years of evolution inherent in environmental communities, providing a new window into the discovery of CO₂‐fixing enzymes not previously characterized.     

Unravelling the Carbon and Sulphur Metabolism in Coastal Soil Ecosystems Using Comparative Cultivation-Independent Genome-Level Characterisation of Microbial Communities

Bacterial autotrophy contributes significantly to the overall carbon balance, which stabilises atmospheric CO₂ concentration and decelerates global warming. Little attention has been paid to different modes of carbon/sulphur metabolism mediated by autotrophic bacterial communities in terrestrial soil ecosystems. We studied these pathways by analysing the distribution and abundance of the diagnostic metabolic marker genes cbbM, apsA and soxB, which encode for ribulose-1,5-bisphosphate carboxylase/oxygenase, adenosine phosphosulphate reductase and sulphate thiohydrolase, respectively, among different contrasting soil types. Additionally, the abundance of community members was assessed by quantifying the gene copy numbers for 16S rRNA, cbbL, cbbM, apsA and soxB. Distinct compositional differences were observed among the clone libraries, which revealed a dominance of phylotypes associated with carbon and sulphur cycling, such as Gammaproteobacteria (Thiohalomonas, Allochromatium, Chromatium, Thiomicrospira) and Alphaproteobacteria (Rhodopseudomonas, Rhodovulum, Paracoccus). The rhizosphere soil was devoid of sulphur metabolism, as the soxB and apsA genes were not observed in the rhizosphere metagenome, which suggests the absence or inadequate representation of sulphur-oxidising bacteria. We hypothesise that the novel Gammaproteobacteria sulphur oxidisers might be actively involved in sulphur oxidation and inorganic carbon fixation, particularly in barren saline soil ecosystems, suggesting their significant putative ecological role and contribution to the soil carbon pool.     

Biogeochemical Signals from Deep Microbial Life in Terrestrial Crust

In contrast to the deep subseafloor biosphere, a volumetrically vast and stable habitat for microbial life in the terrestrial crust remains poorly explored. For the long-term sustainability of a crustal biome, high-energy fluxes derived from hydrothermal circulation and water radiolysis in uranium-enriched rocks are seemingly essential. However, the crustal habitability depending on a low supply of energy is unknown. We present multi-isotopic evidence of microbially mediated sulfate reduction in a granitic aquifer, a representative of the terrestrial crust habitat. Deep meteoric groundwater was collected from underground boreholes drilled into Cretaceous Toki granite (central Japan). A large sulfur isotopic fractionation of 20–60‰ diagnostic to microbial sulfate reduction is associated with the investigated groundwater containing sulfate below 0.2 mM. In contrast, a small carbon isotopic fractionation (<30‰) is not indicative of methanogenesis. Except for 2011, the concentrations of H₂ ranged mostly from 1 to 5 nM, which is also consistent with an aquifer where a terminal electron accepting process is dominantly controlled by ongoing sulfate reduction. High isotopic ratios of mantle-derived ³He relative to radiogenic ⁴He in groundwater and the flux of H₂ along adjacent faults suggest that, in addition to low concentrations of organic matter (<70 µM), H₂ from deeper sources might partly fuel metabolic activities. Our results demonstrate that the deep biosphere in the terrestrial crust is metabolically active and playing a crucial role in the formation of reducing groundwater even under low-energy fluxes.     

Microbial Stimulation and Succession following a Test Well Injection Simulating CO? Leakage into a Shallow Newark Basin Aquifer

In addition to efforts aimed at reducing anthropogenic production of greenhouse gases, geological storage of CO₂ is being explored as a strategy to reduce atmospheric greenhouse gas emission and mitigate climate change. Previous studies of the deep subsurface in North America have not fully considered the potential negative effects of CO₂ leakage into shallow drinking water aquifers, especially from a microbiological perspective. A test well in the Newark Rift Basin was utilized in two field experiments to investigate patterns of microbial succession following injection of CO₂-saturated water into an isolated aquifer interval, simulating a CO₂ leakage scenario. A decrease in pH following injection of CO₂ saturated aquifer water was accompanied by mobilization of trace elements (e.g. Fe and Mn), and increased bacterial cell concentrations in the recovered water. 16S ribosomal RNA gene sequence libraries from samples collected before and after the test well injection were compared to link variability in geochemistry to changes in aquifer microbiology. Significant changes in microbial composition, compared to background conditions, were found following the test well injections, including a decrease in Proteobacteria, and an increased presence of Firmicutes, Verrucomicrobia and microbial taxa often noted to be associated with iron and sulfate reduction. The concurrence of increased microbial cell concentrations and rapid microbial community succession indicate significant changes in aquifer microbial communities immediately following the experimental CO₂ leakage event. Samples collected one year post-injection were similar in cell number to the original background condition and community composition, although not identical, began to revert toward the pre-injection condition, indicating microbial resilience following a leakage disturbance. This study provides a first glimpse into the in situ successional response of microbial communities to CO₂ leakage after subsurface injection in the Newark Basin and the potential microbiological impact of CO₂ leakage on drinking water resources.     

Activity and Diversity of Methanogens in a Petroleum Hydrocarbon-Contaminated Aquifer

Methanogenic activity was investigated in a petroleum hydrocarbon-contaminated aquifer by using a series of four push-pull tests with acetate, formate, H₂ plus CO₂, or methanol to target different groups of methanogenic Archaea. Furthermore, the community composition of methanogens in water and aquifer material was explored by molecular analyses, i.e., fluorescence in situ hybridization (FISH), denaturing gradient gel electrophoresis (DGGE) of 16S rRNA genes amplified with the Archaea-specific primer set ARCH915 and UNI-b-rev, and sequencing of DNA from dominant DGGE bands. Molecular analyses were subsequently compared with push-pull test data. Methane was produced in all tests except for a separate test where 2-bromoethanesulfonate, a specific inhibitor of methanogens, was added. Substrate consumption rates were 0.11 mM day⁻¹ for methanol, 0.38 mM day⁻¹ for acetate, 0.90 mM day⁻¹ for H₂, and 1.85 mM day⁻¹ for formate. Substrate consumption and CH₄ production during all tests suggested that at least three different physiologic types of methanogens were present: H₂ plus CO₂ or formate, acetate, and methanol utilizers. The presence of 15 to 20 bands in DGGE profiles indicated a diverse archaeal population. High H₂ and formate consumption rates agreed with a high diversity of methanogenic Archaea consuming these substrates (16S rRNA gene sequences related to several members of the Methanomicrobiaceae) and the detection of Methanomicrobiaceae by using FISH (1.4% of total DAPI [4′,6-diamidino-2-phenylindole]-stained microorganisms in one water sample; probe MG1200). Considerable acetate consumption agreed with the presence of sequences related to the obligate acetate degrader Methanosaeata concilii and the detection of this species by FISH (5 to 22% of total microorganisms; probe Rotcl1). The results suggest that both aceticlastic and CO₂-type substrate-consuming methanogens are likely involved in the terminal step of hydrocarbon degradation, while methanogenesis from methanol plays a minor role. DGGE profiles further indicate similar archaeal community compositions in water and aquifer material. The combination of hydrogeological and molecular methods employed in this study provide improved information on the community and the potential activity of methanogens in a petroleum hydrocarbon-contaminated aquifer.     

Molecular characterization of microbial communities in fault-bordered aquifers in the Miocene formation of northernmost Japan

We investigated the diversity and distribution of archaeal and bacterial 16S rRNA gene sequences in deep aquifers of mid‐ to late Miocene hard shale located in the northernmost region of the Japanese archipelago. A major fault in the north‐west–south‐east (NW–SE) direction runs across the studied area. We collected three groundwater samples from boreholes on the south‐west (SW) side of the fault at depths of 296, 374 and 625 m below ground level (m.b.g.l.) and one sample from the north‐east (NE) side of the fault at a depth of 458 m.b.g.l. The groundwater samples were observed to be neutral and weakly saline. The total microbial counts after staining with acridine orange were in the order 10⁵?10⁶ cells mL^?1 and 10³ cells mL^?1 in the aquifers to the SW and to the NE of the fault, respectively. A total of 407 archaeal and bacterial 16S rRNA gene sequences (204 and 203 sequences, respectively) were determined for clone libraries constructed from all groundwater samples. Phylogenetic analyses showed that the libraries constructed from the SW aquifers were generally coherent but considerably different from those constructed from the NE aquifer. All of the archaeal clone libraries from the SW aquifers were predominated by a single sequence closely related to the archaeon Methanoculleus chikugoensis, and the corresponding bacterial libraries were mostly predominated by the sequences related to Bacteroidetes, Firmicutes and δ‐Proteobacteria. In contrast, the libraries from the NE aquifer were dominated by uncultured environmental archaeal clones with no methanogen sequences and by β‐proteobacterial clones with no sequences related to Bacteroidetes and δ‐Proteobacteria. Hence, the possible coexistence of methanogens and sulphate reducers in Horonobe deep borehole (HDB) on the SW side is suggested, particularly in HDB‐6 (374 m.b.g.l.). Moreover, these organisms might play an important geochemical role in the groundwater obtained from the aquifers.