scholarly journals Taxonomically and metabolically distinct microbial communities with depth and across a hillslope to riparian zone transect

2019 ◽  
Author(s):  
Adi Lavy ◽  
Paula B. Matheus Carnevali ◽  
Ray Keren ◽  
Markus Bill ◽  
Jiamin Wan ◽  
...  
Keyword(s):  
Stable Isotopes ◽  
Microbial Communities ◽  
Carbon Fixation ◽  
Riparian Zone ◽  
Genomic Variation ◽  
Metabolic Potential ◽  
Mancos Shale ◽  
East River ◽  
Species Overlap ◽  
Different Depths

SummaryWatersheds are important for supplying fresh water, the quality of which depends on complex interplay involving physical, chemical and biological processes. As water percolates through the soil and underlying weathering rock en route to the river corridor, microorganisms mediate key geochemical transformations, yet the distribution and functional capacities of subsurface microbial communities remain little understood. We have studied metabolic capacities of microbial communities along a meadow to floodplain hillslope transect within the East-River watershed, Colorado, using genome resolved metagenomics and carbon and hydrogen stable isotopes. Very limited strain/species overlap was found at different depths below the ground surface and at different distances along the hillslope, possibly due to restricted hydraulic connectivity after early stages of snowmelt. Functions such as carbon fixation and selenate reduction were prevalent at multiple sites, although the lineages of organisms responsible tend to be location-specific. Based on its abundance, sulfur is significantly more important for microbial metabolism at the floodplain compared to on the hillslope. Nitrification and methylamine oxidation are likely only occurring within the floodplain, with nitrification capacity in shallow soil, and methylamine oxidation in deeper unsaturated sediment. Biogenic methane was detected in deep surface samples, but methanogenic organisms were not identified.Originality-Significance StatementIn a previous study within a hillslope to riparian zone transect of a sub-alpine watershed, the community structure was explored using ribosomal protein S3 genes, and the metabolic potential was hypothesized based on the presence of metabolism related genes. However, tying specific strains and species to metabolic functioning was not discussed as resolved genomes were not available.In the current study, we use genome-resolved metagenomics along with carbon and hydrogen stable isotopes to explore the spatial distribution of biogeochemical processes. By linking taxonomy and function, using multiple functional genes indicative of full metabolic pathways, we detect heterogeneity in the distribution of metabolic potential and the organisms involved with depth and landscape position. Thus, we infer how microbiome genomic variation impacts biogeochemical cycling across the watershed.We found very limited strain/species overlap at different depths below the surface and along the hillslope, possibly due to the restricted site to site hydraulic connectivity, and show that communities are largely distinct in their metabolic capacities. Both proximity to the river and the underlying Mancos shale apparently control species distribution and metabolic potential.Functions such as carbon fixation and selenate reduction were prevalent at multiple sites, although the lineages of organisms responsible tend to be location-specific. Arsenate detoxification was found to be prevalent in the riparian zone whereas selenate reduction was detected within weathered Mancos shale. We conclude that important ecosystem functions are strongly associated with the riparian zone, some of which may have crucial implications as to water quality and human health.

scholarly journals Microbial communities across a hillslope-riparian transect shaped by proximity to the stream, groundwater table, and weathered bedrock

2018 ◽  
Author(s):  
Adi Lavy ◽  
David Geller McGrath ◽  
Paula B. Matheus Carnevali ◽  
Jiamin Wan ◽  
Wenming Dong ◽  
...  
Keyword(s):  
Microbial Communities ◽  
Riparian Zone ◽  
Limited Information ◽  
Metabolic Potential ◽  
Carbon And Nitrogen ◽  
East River ◽  
Mountainous Watersheds ◽  
Geochemical Analyses ◽  
Selenium Reduction ◽  
And Function

AbstractWatersheds are important suppliers of freshwater for human societies. Within mountainous watersheds, microbial communities impact water chemistry and element fluxes as water from precipitation events discharges through soils and underlying weathered rock, yet there is limited information regarding the structure and function of these communities. Within the East River, CO watershed, we conducted a depth-resolved, hillslope to riparian zone transect study to identify factors that control how microorganisms are distributed and their functions. Metagenomic and geochemical analyses indicate that distance from the East River and proximity to groundwater and underlying weathered shale strongly impact microbial community structure and metabolic potential. Riparian zone microbial communities are compositionally distinct from all hillslope communities. Bacteria from phyla lacking isolated representatives consistently increase in abundance with increasing depth, but only in the riparian zone saturated sediments did we find Candidate Phyla Radiation bacteria. Riparian zone microbial communities are functionally differentiated from hillslope communities based on their capacities for carbon and nitrogen fixation and sulfate reduction. Selenium reduction is prominent at depth in weathered shale and saturated riparian zone sediments. We anticipate that the drivers of community composition and metabolic potential identified throughout the studied transect will predict patterns across the larger watershed hillslope system.

scholarly journals The Composition and Primary Metabolic Potential of Microbial Communities Inhabiting the Surface Water in the Equatorial Eastern Indian Ocean

Biology ◽  
2021 ◽  
Vol 10 (3) ◽  
pp. 248
Author(s):  
Changling Ding ◽  
Chao Wu ◽  
Congcong Guo ◽  
Jiang Gui ◽  
Yuqiu Wei ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Microbial Communities ◽  
High Throughput Sequencing ◽  
Carbon Fixation ◽  
Calvin Cycle ◽  
Nitrite Reduction ◽  
16S Rrna Genes ◽  
Eastern Indian Ocean ◽  
Rrna Genes ◽  
Metabolic Potential

Currently, there is scant information about the biodiversity and functional diversity of microbes in the eastern Indian Ocean (EIO). Here, we used a combination of high-throughput sequencing of 16S rRNA genes and a metagenomic approach to investigate the microbial population structure and its metabolic function in the equatorial EIO. Our results show that Cyanobacterial Prochlorococcus made up the majority of the population. Interestingly, there were fewer contributions from clades SAR11 (Alphaproteobacteria) and SAR86 (Gammaproteobacteria) to microbial communities than contributions from Prochlorococcus. Based on functional gene analysis, functional genes rbcL, narB, and nasA were relatively abundant among the relevant genes. The abundance of Prochlorococcus implies its typically ecological adaptation in the local ecosystem. The microbial metabolic potential shows that in addition to the main carbon fixation pathway Calvin cycle, the rTCA cycle and the 3-HP/4-HB cycle have potential alternative carbon fixation contributions to local ecosystems. For the nitrogen cycle, the assimilatory nitrate and nitrite reduction pathway is potentially the crucial form of nitrogen utilization; unexpectedly, nitrogen fixation activity was relatively weak. This study extends our knowledge of the roles of microbes in energy and resource cycling in the EIO and provides a foundation for revealing profound biogeochemical processes driven by the microbial community in the ocean.

scholarly journals Metabolic Potential of Microbial Communities in the Hypersaline Sediments of the Bonneville Salt Flats

2021 ◽  
Author(s):  
Julia M McGonigle ◽  
Jeremiah A Bernau ◽  
Brenda B Bowen ◽  
William J Brazelton
Keyword(s):  
Microbial Communities ◽  
Metabolic Pathways ◽  
Carbon Fixation ◽  
Sulfide Oxidation ◽  
Anaerobic Respiration ◽  
Ecosystem Functions ◽  
Metabolic Potential ◽  
Shallow Subsurface ◽  
Microbial Ecosystems ◽  
Salt Flats

The Bonneville Salt Flats (BSF) appear to be entirely desolate when viewed from above, but in reality they host rich microbial communities just below the surface salt crust. In this study, we investigate the metabolic potential of the BSF microbial ecosystem. The predicted and measured metabolic activities provide new insights into the ecosystem functions of evaporite landscapes and are an important analog for potential subsurface microbial ecosystems on ancient and modern Mars. Hypersaline and evaporite systems have been investigated previously as astrobiological analogs for Mars and other salty celestial bodies. Still, these studies have generally focused on aquatic systems and cultivation-dependent approaches. Here, we present an ecosystem-level examination of metabolic pathways within the shallow subsurface of evaporites. We detected aerobic and anaerobic respiration as well as methanogenesis in BSF sediments. Metagenome-assembled genomes (MAGs) of diverse bacteria and archaea encoded a remarkable diversity of metabolic pathways, including those associated with carbon fixation, carbon monoxide oxidation, acetogenesis, methanogenesis, sulfide oxidation, denitrification, and nitrogen fixation. These results demonstrate the potential for multiple energy sources and metabolic pathways in BSF and highlight the possibility for vibrant microbial ecosystems in the shallow subsurface of evaporites.

scholarly journals Diversity and Metabolic Potential of Microbial Communities in a Serpentinite-Hosted Spring at the Tablelands

2021 ◽  
Author(s):  
Emily Dart ◽  
William J. Brazelton
Keyword(s):  
Microbial Communities ◽  
Carbon Fixation ◽  
Hydrogen Oxidation ◽  
Sampling Technique ◽  
16S Rrna Gene Sequencing ◽  
Direct Access ◽  
Rrna Gene ◽  
Metabolic Potential ◽  
Rrna Gene Sequencing ◽  
Community Dissimilarity

The geochemical process of serpentinization releases energy and organic carbon: two of the basic requirements needed to support life. Sites of active serpentinization in the deep subsurface provide the intriguing possibility of a non-photosynthetically-supported biosphere. However, serpentinization also creates conditions, such as high pH and limited electron acceptors, which may limit microbial growth and diversity. Gaining an understanding of the identity and metabolic potential of microbes that thrive in these environments may provide insight as to whether serpentinization is sufficient to independently support life. Tablelands Ophiolite in Gros Morne National Park, Newfoundland, Canada is a continental site of serpentinization where serpentinite springs form surface pools. These pools provide easy sampling access to subsurface fluids and may allow for sampling of the subsurface microbial community. However, identification of members of the subsurface community in these pools is complicated by both surface contamination and contamination by organisms that inhabit the transition zone where hydrogen-rich subsurface fluids meet oxygen-rich surface fluids. This study was designed to distinguish among these potential sources of microorganisms by using a sampling technique that more effectively samples subsurface fluids. Community dissimilarity comparisons using environmental 16S rRNA gene sequencing indicate that the sampling design led to more direct access to subsurface fluids. These results are supported by metagenomic analyses that show metabolic pathways consistent with non-photosynthetic carbon fixation in the samples expected to represent subsurface fluids and that show hydrogen oxidation pathways in samples associated with the surface sources. These results provide a clearer picture of the diversity and metabolic potential of microbial communities potentially inhabiting subsurface, serpentinite-hosted habitats.

scholarly journals Genome-reconstruction for eukaryotes from complex natural microbial communities

2017 ◽  
Author(s):  
Patrick T. West ◽  
Alexander J. Probst ◽  
Igor V. Grigoriev ◽  
Brian C. Thomas ◽  
Jillian F. Banfield
Keyword(s):  
Organic Carbon ◽  
Microbial Communities ◽  
Environmental Samples ◽  
Carbon Fixation ◽  
Sulfur Oxidation ◽  
Metabolic Potential ◽  
Microbial Eukaryotes ◽  
Sequence Identification ◽  
Ecosystem Studies ◽  
Almost All

AbstractMicrobial eukaryotes are integral components of natural microbial communities and their inclusion is critical for many ecosystem studies yet the majority of published metagenome analyses ignore eukaryotes. In order to include eukaryotes in environmental studies we propose a method to recover eukaryotic genomes from complex metagenomic samples. A key step for genome recovery is separation of eukaryotic and prokaryotic fragments. We developed a kmer-based strategy, EukRep, for eukaryotic sequence identification and applied it to environmental samples to show that it enables genome recovery, genome completeness evaluation and prediction of metabolic potential. We used this approach to test the effect of addition of organic carbon on a geyser-associated microbial community and detected a substantial change of the community metabolism, with selection against almost all candidate phyla bacteria and archaea and for eukaryotes. Near complete genomes were reconstructed for three fungi placed within the eurotiomycetes and an arthropod. While carbon fixation and sulfur oxidation were important functions in the geyser community prior to carbon addition, the organic carbon impacted community showed enrichment for secreted proteases, secreted lipases, cellulose targeting CAZymes, and methanol oxidation. We demonstrate the broader utility of EukRep by reconstructing and evaluating relatively high quality fungal, protist, and rotifer genomes from complex environmental samples. This approach opens the way for cultivation-independent analyses of whole microbial communities.

scholarly journals The keystone species of Precambrian deep bedrock biosphere belong to <i>Burkholderiales</i> and <i>Clostridiales</i>

2015 ◽  
Vol 12 (21) ◽  
pp. 18103-18150 ◽  
Author(s):  
L. Purkamo ◽  
M. Bomberg ◽  
R. Kietäväinen ◽  
H. Salavirta ◽  
M. Nyyssönen ◽  
...  
Keyword(s):  
Microbial Communities ◽  
Carbon Fixation ◽  
Keystone Species ◽  
Carbon Assimilation ◽  
Sugar Metabolism ◽  
Archaeal Community ◽  
Amino Sugar ◽  
Amplicon Sequencing ◽  
Fracture Zones ◽  
Crystalline Bedrock

Abstract. The bacterial and archaeal community composition and the possible carbon assimilation processes and energy sources of microbial communities in oligotrophic, deep, crystalline bedrock fractures is yet to be resolved. In this study, intrinsic microbial communities from six fracture zones from 180–2300 m depths in Outokumpu bedrock were characterized using high-throughput amplicon sequencing and metagenomic prediction. Comamonadaceae-, Anaerobrancaceae- and Pseudomonadaceae-related OTUs form the core community in deep crystalline bedrock fractures in Outokumpu. Archaeal communities were mainly composed of Methanobacteraceae-affiliating OTUs. The predicted bacterial metagenomes showed that pathways involved in fatty acid and amino sugar metabolism were common. In addition, relative abundance of genes coding the enzymes of autotrophic carbon fixation pathways in predicted metagenomes was low. This indicates that heterotrophic carbon assimilation is more important for microbial communities of the fracture zones. Network analysis based on co-occurrence of OTUs revealed the keystone genera of the microbial communities belonging to Burkholderiales and Clostridiales. Bacterial communities in fractures resemble those found from oligotrophic, hydrogen-enriched environments. Serpentinization reactions of ophiolitic rocks in Outokumpu assemblage may provide a source of energy and organic carbon compounds for the microbial communities in the fractures. Sulfate reducers and methanogens form a minority of the total microbial communities, but OTUs forming these minor groups are similar to those found from other deep Precambrian terrestrial bedrock environments.

scholarly journals Microbial dark carbon fixation fueled by nitrate enrichment

2021 ◽  
Author(s):  
Joseph H. Vineis ◽  
Ashley N. Bulseco ◽  
Jennifer L. Bowen
Keyword(s):  
Microbial Communities ◽  
Marine Sediments ◽  
Salt Marshes ◽  
Carbon Fixation ◽  
Niche Partitioning ◽  
Coastal Marine Sediments ◽  
Functional Relationships ◽  
Coastal Marine ◽  
Dark Carbon Fixation ◽  
The Impact

Anthropogenic nitrate amendment to coastal marine sediments can increase rates of heterotrophic mineralization and autotrophic dark carbon fixation (DCF). DCF may be favored in sediments where organic matter is biologically unavailable, leading to a microbial community supported by chemoautotrophy. Niche partitioning among DCF communities and adaptations for nitrate metabolism in coastal marine sediments remain poorly characterized, especially within salt marshes. We used genome-resolved metagenomics, phylogenetics, and comparative genomics to characterize the potential niche space, phylogenetic relationships, and adaptations important to microbial communities within nitrate enriched sediment. We found that nitrate enrichment of sediment from discrete depths between 0-25 cm supported both heterotrophs and chemoautotrophs that use sulfur oxidizing denitrification to drive the Calvin-Benson-Bassham (CBB) or reductive TCA (rTCA) DCF pathways. Phylogenetic reconstruction indicated that the nitrate enriched community represented a small fraction of the phylogenetic diversity contained in coastal marine environmental genomes, while pangenomics revealed close evolutionary and functional relationships with DCF microbes in other oligotrophic environments. These results indicate that DCF can support coastal marine microbial communities and should be carefully considered when estimating the impact of nitrate on carbon cycling in these critical habitats.

scholarly journals Composition and predictive functional analysis of bacterial communities in the surface seawater of the Changjiang Estuary

2017 ◽  
Author(s):  
Dong-Mei Wu ◽  
Jian-Xin Wang ◽  
Xiao-Hui Liu ◽  
Ying-Ping Fan ◽  
Ran Jiang ◽  
...  
Keyword(s):  
Dissolved Oxygen ◽  
Microbial Communities ◽  
Bacterial Communities ◽  
High Throughput Sequencing ◽  
Carbon Fixation ◽  
Oxygen Demand ◽  
Environmental Parameters ◽  
Changjiang Estuary ◽  
Surface Seawater ◽  
The Changjiang Estuary

The objective of this study was to characterize the structure and function of microbial communities in surface seawater from the Changjiang Estuary and adjacent areas, China. Sample water was collected at 12 sites and environmental parameters were measured. Community structure was analyzed using high-throughput sequencing of 16S rDNA genes. Predictive metagenomic approach was used to predict the function of bacterial communities. Result showed that sample site A0102 had the highest bacterial abundance and diversity. The heatmap indicated that different samples could be clustered into six groups. Phylogenetic analysis showed that Proteobacteria was the predominant phylum in all samples, followed by Bacteroidetes and Actinobacteria. Alphaproteobacteria and Gammaproteobacteria were the dominant classes. The analysis of predictive metagenomic showed carbon fixation pathways in prokaryotes, nitrogen metabolism, carbon fixation in photosynthetic organisms, photosynthesis and polycyclic aromatic hydrocarbon degradation were enriched in all samples. Redundancy analysis (RDA) identified that dissolved oxygen (DO) and PO43– concentration had positive correlations with the bacterial communities while chemical oxygen demand (COD), dissolved oxygen (DO) and PO43– concentration were significantly associated with microbial functional diversity. This study adds to our knowledge of functional and taxonomic composition of microbial communities.

scholarly journals Metagenome assembled genomes of novel taxa from an acid mine drainage environment

2021 ◽  
Author(s):  
Christen L. Grettenberger ◽  
Trinity L. Hamilton
Keyword(s):  
Acid Mine Drainage ◽  
16S Rrna ◽  
16S Rrna Gene ◽  
Microbial Communities ◽  
Mine Drainage ◽  
Biogeochemical Cycling ◽  
Rrna Gene ◽  
Metabolic Potential ◽  
Carbon And Nitrogen ◽  
Acid Mine

Acid mine drainage (AMD) is a global problem in which iron sulfide minerals oxidize and generate acidic, metal-rich water. Bioremediation relies on understanding how microbial communities inhabiting an AMD site contribute to biogeochemical cycling. A number of studies have reported community composition in AMD sites from 16S rRNA gene amplicons but it remains difficult to link taxa to function, especially in the absence of closely related cultured species or those with published genomes. Unfortunately, there is a paucity of genomes and cultured taxa from AMD environments. Here, we report 29 novel metagenome assembled genomes from Cabin Branch, an AMD site in the Daniel Boone National Forest, KY, USA. The genomes span 11 bacterial phyla and one Archaea and include taxa that contribute to carbon, nitrogen, sulfur, and iron cycling. These data reveal overlooked taxa that contribute to carbon fixation in AMD sites as well as uncharacterized Fe(II)-oxidizing bacteria. These data provide additional context for 16S rRNA gene studies, add to our understanding of the taxa involved in biogeochemical cycling in AMD environments, and can inform bioremediation strategies. IMPORTANCE Bioremediating acid mine drainage requires understanding how microbial communities influence geochemical cycling of iron and sulfur and biologically important elements like carbon and nitrogen. Research in this area has provided an abundance of 16S rRNA gene amplicon data. However, linking these data to metabolisms is difficult because many AMD taxa are uncultured or lack published genomes. Here, we present metagenome assembled genomes from 29 novel AMD taxa and detail their metabolic potential. These data provide information on AMD taxa that could be important for bioremediation strategies including taxa that are involved in cycling iron, sulfur, carbon, and nitrogen.

scholarly journals Soil Depth Determines the Composition and Diversity of Bacterial and Archaeal Communities in a Poplar Plantation

Forests ◽  
2019 ◽  
Vol 10 (7) ◽  
pp. 550 ◽  
Author(s):  
Huili Feng ◽  
Jiahuan Guo ◽  
Weifeng Wang ◽  
Xinzhang Song ◽  
Shuiqiang Yu
Keyword(s):  
16S Rrna ◽  
16S Rrna Gene ◽  
Microbial Communities ◽  
Relative Abundance ◽  
Rrna Gene ◽  
Poplar Plantation ◽  
Plantation Forest ◽  
Bacterial And Archaeal Communities ◽  
Different Depths ◽  
Archaeal Communities

Understanding the composition and diversity of soil microorganisms that typically mediate the soil biogeochemical cycle is crucial for estimating greenhouse gas flux and mitigating global changes in plantation forests. Therefore, the objectives of this study were to investigate changes in diversity and relative abundance of bacteria and archaea with soil profiles and the potential factors influencing the vertical differentiation of microbial communities in a poplar plantation. We investigated soil bacterial and archaeal community compositions and diversities by 16S rRNA gene Illumina MiSeq sequencing at different depths of a poplar plantation forest in Chenwei forest farm, Sihong County, Jiangsu, China. More than 882,422 quality-filtered 16S rRNA gene sequences were obtained from 15 samples, corresponding to 34 classified phyla and 68 known classes. Ten major bacterial phyla and two archaeal phyla were found. The diversity of bacterial and archaeal communities decreased with depth of the plantation soil. Analysis of variance (ANOVA) of relative abundance of microbial communities exhibited that Nitrospirae, Verrucomicrobia, Latescibacteria, GAL15, SBR1093, and Euryarchaeota had significant differences at different depths. The transition zone of the community composition between the surface and subsurface occurred at 10–20 cm. Overall, our findings highlighted the importance of depth with regard to the complexity and diversity of microbial community composition in plantation forest soils.

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