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Turrini P, Chebbi A, Riggio FP, Visca P. The geomicrobiology of limestone, sulfuric acid speleogenetic, and volcanic caves: basic concepts and future perspectives. Front Microbiol 2024; 15:1370520. [PMID: 38572233 PMCID: PMC10987966 DOI: 10.3389/fmicb.2024.1370520] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/14/2024] [Accepted: 03/07/2024] [Indexed: 04/05/2024] Open
Abstract
Caves are ubiquitous subterranean voids, accounting for a still largely unexplored surface of the Earth underground. Due to the absence of sunlight and physical segregation, caves are naturally colonized by microorganisms that have developed distinctive capabilities to thrive under extreme conditions of darkness and oligotrophy. Here, the microbiomes colonizing three frequently studied cave types, i.e., limestone, sulfuric acid speleogenetic (SAS), and lava tubes among volcanic caves, have comparatively been reviewed. Geological configurations, nutrient availability, and energy flows in caves are key ecological drivers shaping cave microbiomes through photic, twilight, transient, and deep cave zones. Chemoheterotrophic microbial communities, whose sustenance depends on nutrients supplied from outside, are prevalent in limestone and volcanic caves, while elevated inorganic chemical energy is available in SAS caves, enabling primary production through chemolithoautotrophy. The 16S rRNA-based metataxonomic profiles of cave microbiomes were retrieved from previous studies employing the Illumina platform for sequencing the prokaryotic V3-V4 hypervariable region to compare the microbial community structures from different cave systems and environmental samples. Limestone caves and lava tubes are colonized by largely overlapping bacterial phyla, with the prevalence of Pseudomonadota and Actinomycetota, whereas the co-dominance of Pseudomonadota and Campylobacterota members characterizes SAS caves. Most of the metataxonomic profiling data have so far been collected from the twilight and transient zones, while deep cave zones remain elusive, deserving further exploration. Integrative approaches for future geomicrobiology studies are suggested to gain comprehensive insights into the different cave types and zones. This review also poses novel research questions for unveiling the metabolic and genomic capabilities of cave microorganisms, paving the way for their potential biotechnological applications.
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Affiliation(s)
- Paolo Turrini
- Department of Science, Roma Tre University, Rome, Italy
| | - Alif Chebbi
- Department of Science, Roma Tre University, Rome, Italy
| | | | - Paolo Visca
- Department of Science, Roma Tre University, Rome, Italy
- National Biodiversity Future Center, Palermo, Italy
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Li C, Liao H, Xu L, Wang C, Yao M, Wang J, Li X. Comparative genomics reveals the adaptation of ammonia-oxidising Thaumarchaeota to arid soils. Environ Microbiol 2024; 26:e16601. [PMID: 38454574 DOI: 10.1111/1462-2920.16601] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/08/2023] [Accepted: 02/09/2024] [Indexed: 03/09/2024]
Abstract
Thaumarchaeota are predominant in oligotrophic habitats such as deserts and arid soils, but their adaptations to these arid conditions are not well understood. In this study, we assembled 23 Thaumarchaeota genomes from arid and semi-arid soils collected from the Inner Mongolia Steppe and the Qinghai-Tibet Plateau. Using a comparative genomics approach, integrated with 614 Thaumarchaeota genomes from public databases, we identified the traits and evolutionary forces that contribute to their adaptations to aridity. Our results showed that the newly assembled genomes represent an early diverging group within the lineage of ammonia-oxidising Thaumarchaeota. While the genomic functions previously identified in arid soil lineages were conserved across terrestrial, shallow-ocean and deep-ocean lineages, several traits likely contribute to Thaumarchaeota's adaptation to aridity. These include chlorite dismutase, arsenate reductase, V-type ATPase and genes dealing with oxidative stresses. The acquisition and loss of traits at the last common ancestor of arid soil lineages may have facilitated the specialisation of Thaumarchaeota in arid soils. Additionally, the acquisition of unique adaptive traits, such as a urea transporter, Ca2+ :H+ antiporter, mannosyl-3-phosphoglycerate synthase and phosphatase, DNA end-binding protein Ku and phage shock protein A, further distinguishes arid soil Thaumarchaeota. This study provides evidence for the adaptations of Thaumarchaeota to arid soil, enhancing our understanding of the nitrogen and carbon cycling driven by Thaumarchaeota in drylands.
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Affiliation(s)
- Chaonan Li
- Ecological Security and Protection Key Laboratory of Sichuan Province, Mianyang Normal University, Mianyang, China
| | - Haijun Liao
- Engineering Research Center of Chuanxibei RHS Construction at Mianyang Normal University of Sichuan Province, Mianyang Normal University, Mianyang, China
| | - Lin Xu
- National Forestry and Grassland Administration Key Laboratory of Forest Resources Conservation and Ecological Safety on the Upper Reaches of the Yangtze River & Forestry Ecological Engineering in the Upper Reaches of the Yangtze River Key Laboratory of Sichuan Province, Sichuan Agricultural University, Chengdu, China
| | - Changting Wang
- Institute of Qinghai-Tibet Plateau, Southwest Minzu University, Chengdu, China
| | - Minjie Yao
- Engineering Research Center of Soil Remediation of Fujian Province University, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, China
| | - Junming Wang
- Section of Climate Science, Illinois State Water Survey, Prairie Research Institute, University of Illinois at Urbana-Champaign, Champaign, Illinois, USA
| | - Xiangzhen Li
- Engineering Research Center of Soil Remediation of Fujian Province University, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, China
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Samanta B, Sharma S, Budhwar R. Metagenome Analysis of Speleothem Microbiome from Subterranean Cave Reveals Insight into Community Structure, Metabolic Potential, and BGCs Diversity. Curr Microbiol 2023; 80:317. [PMID: 37561193 DOI: 10.1007/s00284-023-03431-9] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/26/2023] [Accepted: 07/26/2023] [Indexed: 08/11/2023]
Abstract
The Borra caves, the second largest subterranean karst cave ecosystem in the Indian sub-continent, are located at the Ananthagiri hills of Araku Valley in the Alluri district of Andhra Pradesh, India. The present investigation applied a shotgun metagenomic approach to gain insights into the microbial community structure, metabolic potential, and biosynthetic gene cluster (BGC) diversity of the microbes colonizing the surface of the speleothems from the aphotic zone of Borra caves. The taxonomic analysis of the metagenome data illustrated that the speleothem-colonizing core microbial community was dominated mainly by Alpha-, Beta-, and Gamma-Proteobacteria, Actinobacteria, Firmicutes, and Bacteroidetes. The key energy metabolic pathways analysis provides strong evidence of chemolithoautotrophic and chemoheterotrophic modes of nutrition in the speleothem-colonizing microbial community. Metagenome data suggests that sulfur reducers and sulfur-disproportionating microbes might play a vital role in energy generation in this ecosystem. Our metagenome data also suggest that the dissimilatory nitrifiers and nitrifying denitrifiers might play an essential role in conserving nitrogen pools in the ecosystem. Furthermore, metagenome-wide BGCs mining retrieved 451 putative BGCs; NRPS was the most abundant (24%). Phylogenetic analysis of the C domain of NRPS showed that sequences were distributed across all six function categories of the known C domain, including several novel subclades. For example, a novel subclade had been recovered within the LCL domain clade as a sister subclade of immunosuppressant cyclosporin encoding C domain sequences. Our result suggested that subterranean cave microbiomes might be a potential reservoir of novel microbial metabolites.
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Affiliation(s)
- Brajogopal Samanta
- Department of Microbiology and FST, GITAM School of Science, GITAM (Deemed to Be University), Rushikonda, Visakhapatnam, Andhra Pradesh, 530045, India.
| | - Shivasmi Sharma
- Bionivid Technology Private Limited, Bengaluru, Karnataka, 560043, India
| | - Roli Budhwar
- Bionivid Technology Private Limited, Bengaluru, Karnataka, 560043, India
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Liu X, Wang H, Wang W, Cheng X, Wang Y, Li Q, Li L, Ma L, Lu X, Tuovinen OH. Nitrate determines the bacterial habitat specialization and impacts microbial functions in a subsurface karst cave. Front Microbiol 2023; 14:1115449. [PMID: 36846803 PMCID: PMC9947541 DOI: 10.3389/fmicb.2023.1115449] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/04/2022] [Accepted: 01/19/2023] [Indexed: 02/11/2023] Open
Abstract
Karst caves are usually considered as natural laboratories to study pristine microbiomes in subsurface biosphere. However, effects of the increasingly detected nitrate in underground karst ecosystem due to the acid rain impact on microbiota and their functions in subsurface karst caves have remained largely unknown. In this study, samples of weathered rocks and sediments were collected from the Chang Cave, Hubei province and subjected to high-throughput sequencing of 16S rRNA genes. The results showed that nitrate significantly impacted bacterial compositions, interactions, and functions in different habitats. Bacterial communities clustered according to their habitats with distinguished indicator groups identified for each individual habitat. Nitrate shaped the overall bacterial communities across two habitats with a contribution of 27.2%, whereas the pH and TOC, respectively, structured bacterial communities in weathered rocks and sediments. Alpha and beta diversities of bacterial communities increased with nitrate concentration in both habitats, with nitrate directly affecting alpha diversity in sediments, but indirectly on weathered rocks by lowering pH. Nitrate impacted more on bacterial communities in weathered rocks at the genus level than in sediments because more genera significantly correlated with nitrate concentration in weathered rocks. Diverse keystone taxa involved in nitrogen cycling were identified in the co-occurrence networks such as nitrate reducers, ammonium-oxidizers, and N2-fixers. Tax4Fun2 analysis further confirmed the dominance of genes involved in nitrogen cycling. Genes of methane metabolism and carbon fixation were also dominant. The dominance of dissimilatory and assimilatory nitrate reduction in nitrogen cycling substantiated nitrate impact on bacterial functions. Our results for the first time revealed the impact of nitrate on subsurface karst ecosystem in terms of bacterial compositions, interactions, and functions, providing an important reference for further deciphering the disturbance of human activities on the subsurface biosphere.
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Affiliation(s)
- Xiaoyan Liu
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China
| | - Hongmei Wang
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China,*Correspondence: Hongmei Wang, ;
| | - Weiqi Wang
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China
| | - Xiaoyu Cheng
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China
| | - Yiheng Wang
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Qing Li
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Lu Li
- State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Liyuan Ma
- School of Environmental Studies, China University of Geosciences, Wuhan, China
| | - Xiaolu Lu
- School of Environmental Studies, China University of Geosciences, Wuhan, China
| | - Olli H. Tuovinen
- Department of Microbiology, Ohio State University, Columbus, OH, United States
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Cheng X, Xiang X, Yun Y, Wang W, Wang H, Bodelier PLE. Archaea and their interactions with bacteria in a karst ecosystem. Front Microbiol 2023; 14:1068595. [PMID: 36814573 PMCID: PMC9939782 DOI: 10.3389/fmicb.2023.1068595] [Citation(s) in RCA: 7] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/13/2022] [Accepted: 01/19/2023] [Indexed: 02/08/2023] Open
Abstract
Karst ecosystems are widely distributed around the world, accounting for 15-20% of the global land area. However, knowledge on microbial ecology of these systems does not match with their global importance. To close this knowledge gap, we sampled three niches including weathered rock, sediment, and drip water inside the Heshang Cave and three types of soils overlying the cave (forest soil, farmland soil, and pristine karst soil). All these samples were subjected to high-throughput sequencing of V4-V5 region of 16S rRNA gene and analyzed with multivariate statistical analysis. Overall, archaeal communities were dominated by Thaumarchaeota, whereas Actinobacteria dominated bacterial communities. Thermoplasmata, Nitrosopumilaceae, Aenigmarchaeales, Crossiella, Acidothermus, and Solirubrobacter were the important predictor groups inside the Heshang Cave, which were correlated to NH4 + availability. In contrast, Candidatus Nitrososphaera, Candidatus Nitrocosmicus, Thaumarchaeota Group 1.1c, and Pseudonocardiaceae were the predictors outside the cave, whose distribution was correlated with pH, Ca2+, and NO2 -. Tighter network structures were found in archaeal communities than those of bacteria, whereas the topological properties of bacterial networks were more similar to those of total prokaryotic networks. Both chemolithoautotrophic archaea (Candidatus Methanoperedens and Nitrosopumilaceae) and bacteria (subgroup 7 of Acidobacteria and Rokubacteriales) were the dominant keystone taxa within the co-occurrence networks, potentially playing fundamental roles in obtaining energy under oligotrophic conditions and thus maintaining the stability of the cave ecosystem. To be noted, all the keystone taxa of karst ecosystems were related to nitrogen cycling, which needs further investigation, particularly the role of archaea. The predicted ecological functions in karst soils mainly related to carbohydrate metabolism, biotin metabolism, and synthesis of fatty acid. Our results offer new insights into archaeal ecology, their potential functions, and archaeal interactions with bacteria, which enhance our understanding about the microbial dark matter in the subsurface karst ecosystems.
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Affiliation(s)
- Xiaoyu Cheng
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China,Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands
| | - Xing Xiang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China,College of Life Science, Shangrao Normal University, Shangrao, China
| | - Yuan Yun
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China,College of Life Sciences, Nankai University, Tianjin, China
| | - Weiqi Wang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China
| | - Hongmei Wang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China,School of Environmental Studies, China University of Geosciences, Wuhan, China,*Correspondence: Hongmei Wang, ✉ ; ✉
| | - Paul L. E. Bodelier
- Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands
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Convergent Community Assembly among Globally Separated Acidic Cave Biofilms. Appl Environ Microbiol 2023; 89:e0157522. [PMID: 36602326 PMCID: PMC9888236 DOI: 10.1128/aem.01575-22] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/06/2023] Open
Abstract
Acidophilic bacteria and archaea inhabit extreme geochemical "islands" that can tell us when and how geographic barriers affect the biogeography of microorganisms. Here, we describe microbial communities from extremely acidic (pH 0 to 1) biofilms, known as snottites, from hydrogen sulfide-rich caves. Given the extreme acidity and subsurface location of these biofilms, and in light of earlier work showing strong geographic patterns among snottite Acidithiobacillus populations, we investigated their structure and diversity in order to understand how geography might impact community assembly. We used 16S rRNA gene cloning and fluorescence in situ hybridization (FISH) to investigate 26 snottite samples from four sulfidic caves in Italy and Mexico. All samples had very low biodiversity and were dominated by sulfur-oxidizing bacteria in the genus Acidithiobacillus. Ferroplasma and other archaea in the Thermoplasmatales ranged from 0 to 50% of total cells, and relatives of the bacterial genera Acidimicrobium and Ferrimicrobium were up to 15% of total cells. Rare phylotypes included Sulfobacillus spp. and members of the phyla "Candidatus Dependentiae" and "Candidatus Saccharibacteria" (formerly TM6 and TM7). Although the same genera of acidophiles occurred in snottites on separate continents, most members of those genera represent substantially divergent populations, with 16S rRNA genes that are only 95 to 98% similar. Our findings are consistent with a model of community assembly where sulfidic caves are stochastically colonized by microorganisms from local sources, which are strongly filtered through environmental selection for extreme acid tolerance, and these different colonization histories are maintained by dispersal restrictions within and among caves. IMPORTANCE Microorganisms that are adapted to extremely acidic conditions, known as extreme acidophiles, are catalysts for rock weathering, metal cycling, and mineral formation in naturally acidic environments. They are also important drivers of large-scale industrial processes such as biomining and contaminant remediation. Understanding the factors that govern their ecology and distribution can help us better predict and utilize their activities in natural and engineered systems. However, extremely acidic habitats are unusual in that they are almost always isolated within circumneutral landscapes. So where did their acid-adapted inhabitants come from, and how do new colonists arrive and become established? In this study, we took advantage of a unique natural experiment in Earth's subsurface to show how isolation may have played a role in the colonization history, community assembly, and diversity of highly acidic microbial biofilms.
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Tang S, Rao Y, Huang S, Xu Y, Zeng K, Liang X, Ling Q, Liu K, Ma J, Yu F, Li Y. Impact of environmental factors on the ammonia-oxidizing and denitrifying microbial community and functional genes along soil profiles from different ecologically degraded areas in the Siding mine. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 326:116641. [PMID: 36343494 DOI: 10.1016/j.jenvman.2022.116641] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/26/2022] [Revised: 10/08/2022] [Accepted: 10/25/2022] [Indexed: 06/16/2023]
Abstract
Ammonia oxidizers (ammonia-oxidizing bacteria (AOB amoA) and ammonia-oxidizing archaea (AOA amoA)) and denitrifiers (encoded by nirS, nirK and nosZ) in the soil nitrogen cycle exist in a variety of natural ecosystems. However, little is known about the contribution of these five N-related functional genes to nitrification and denitrification in the soil profile in severely ecologically degraded areas. Therefore, in the present study, the abundance, diversity and community composition of AOA, AOB, nirS, nirK and nosZ were investigated in the soil profiles of different ecologically degraded areas in the Siding mine. The results indicated that, at the phylum level, the dominant archaea were Crenarchaeota and Thaumarchaeota and the dominant bacteria were Proteobacteria. Heavy metal contents had a great impact on AOA amoA, nirS and nirK gene abundances. AOA amoA contributed more during the ammonia oxidation process and was better adapted for survival in heavy metal-contaminated environments. In addition to heavy metals, the soil organic matter (SOM) content and C/N ratio had strong effects on the AOA and AOB community diversity and structure. In addition, variations in the net ammonification and nitrification rates were proportional to AOA amoA abundance along the soil profile. The soil C/N ratio, soil available phosphorus content and soil moisture influenced the denitrification process. Both soil available phosphorus and moisture were more strongly related to nosZ than to nirS and nirK. In addition, nosZ presented a higher correlation with the nosZ/(nirS + nirK) ratio. Moreover, nosZ/(nirS + nirK) was the key functional gene group that drove the major processes for NH4+-N and NO3--N transformation. This study demonstrated the role and importance of soil property impacts on N-related microbes in the soil profile and provided a better understanding of the role and importance of N-related functional genes and their contribution to soil nitrification and denitrification processes in highly degraded areas in the Siding mine.
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Affiliation(s)
- Shuting Tang
- Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, China; College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Yin Rao
- College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Shulian Huang
- College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Yue Xu
- College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Kaiyue Zeng
- College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Xin Liang
- Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, China; College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Qiujie Ling
- College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China
| | - Kehui Liu
- Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, China; Guangxi Key Laboratory of Landscape Resources Conservation and Sustainable Utilization in Lijiang River Basin, Guangxi Normal University, 541004, Guilin, China; College of Life Science, Guangxi Normal University, 541004, Guilin, China
| | - Jiangming Ma
- Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, China; Guangxi Key Laboratory of Landscape Resources Conservation and Sustainable Utilization in Lijiang River Basin, Guangxi Normal University, 541004, Guilin, China; College of Life Science, Guangxi Normal University, 541004, Guilin, China
| | - Fangming Yu
- Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, China; Guangxi Key Laboratory of Landscape Resources Conservation and Sustainable Utilization in Lijiang River Basin, Guangxi Normal University, 541004, Guilin, China; College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China.
| | - Yi Li
- Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, China; Guangxi Key Laboratory of Landscape Resources Conservation and Sustainable Utilization in Lijiang River Basin, Guangxi Normal University, 541004, Guilin, China; College of Environment and Resources, Guangxi Normal University, 541004, Guilin, China.
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Ahamada Rachid N, Doğruöz Güngör N. Major impacts of caving activities on cave microbial diversity: case study of Morca Cave, Turkey. Int Microbiol 2022; 26:179-190. [PMID: 36331653 DOI: 10.1007/s10123-022-00287-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/11/2021] [Revised: 06/18/2022] [Accepted: 10/20/2022] [Indexed: 11/06/2022]
Abstract
Some of microorganisms identified in cave ecosystems have been reported to play a permanent and strategic role for maintaining life of these environments. Human entrance into caves can induce some changes of cave physicochemical parameters which ultimately impacts the living organisms. In these facts, for the first time, Morca Cave was explored in a purpose to evaluate the impacts that can be caused by the human activities on microbial diversity in a limited period of time. Morca is a karts cave located in the Taşeli Plateau in the Middle Taurus mountains in Turkey. The first entrance into this cave was in 2018, and expeditors reached to - 500 m. During the second expedition in 2019, a camp was established at the - 1040-m depth during 4 days. In order to evaluate the human impacts in a new explored cave, this camping depth is chosen to be our studied area because it was its first entrance. Before the installation and at the end of the camp, sediments and surface samples were taken from different points of the camp area and around. Sequencing of 16 s rRNA of each sample to isolate DNA by using the next-generation sequencing (NGS) method was performed. The profile of the microbial diversity before the camping revealed that the class Thermoplasmata was dominated the archaea group and Gammaproteobacteria and Alphaproteobacteria were the most dominant bacterial classes. After the camp, most studied sites were noted with a decrease of microbial diversity especially the previous cited classes strains. Bacteria belonging to Bacilli class have increased after the camp. Increase of bacteria that are belonging to Bacteroidia has also observed in the most active areas. This present study highlight how cave microbial diversity can respond to the human activities within a short period inside a closed cave. Furthermore, it may constitute a solid basis and support on the improvement of techniques for cave management and expedition planning for the conservation of cave nature.
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Affiliation(s)
- Nahdhoit Ahamada Rachid
- Institute of Graduate Studies in Sciences, Istanbul University, 34134 Vezneciler Fatih, Istanbul, Turkey
| | - Nihal Doğruöz Güngör
- Department of Biology, Faculty of Science, Istanbul University, 34134 Vezneciler Fatih, Istanbul, Turkey.
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Zhu HZ, Jiang CY, Liu SJ. Microbial roles in cave biogeochemical cycling. Front Microbiol 2022; 13:950005. [PMID: 36246268 PMCID: PMC9554484 DOI: 10.3389/fmicb.2022.950005] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/22/2022] [Accepted: 09/14/2022] [Indexed: 11/23/2022] Open
Abstract
Among fundamental research questions in subterranean biology, the role of subterranean microbiomes playing in key elements cycling is a top-priority one. Karst caves are widely distributed subsurface ecosystems, and cave microbes get more and more attention as they could drive cave evolution and biogeochemical cycling. Research have demonstrated the existence of diverse microbes and their participance in biogeochemical cycling of elements in cave environments. However, there are still gaps in how these microbes sustain in caves with limited nutrients and interact with cave environment. Cultivation of novel cave bacteria with certain functions is still a challenging assignment. This review summarized the role of microbes in cave evolution and mineral deposition, and intended to inspire further exploration of microbial performances on C/N/S biogeocycles.
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Affiliation(s)
- Hai-Zhen Zhu
- State Key Laboratory of Microbial Resources and Environmental Microbiology Research Center, Institute of Microbiology, Chinese Academy of Sciences, Beijing, China
| | - Cheng-Ying Jiang
- State Key Laboratory of Microbial Resources and Environmental Microbiology Research Center, Institute of Microbiology, Chinese Academy of Sciences, Beijing, China
- College of Life Sciences, University of Chinese Academy of Sciences, Beijing, China
| | - Shuang-Jiang Liu
- State Key Laboratory of Microbial Resources and Environmental Microbiology Research Center, Institute of Microbiology, Chinese Academy of Sciences, Beijing, China
- College of Life Sciences, University of Chinese Academy of Sciences, Beijing, China
- State Key Laboratory of Microbial Technology, Shandong University, Qingdao, China
- *Correspondence: Shuang-Jiang Liu,
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Prescott RD, Zamkovaya T, Donachie SP, Northup DE, Medley JJ, Monsalve N, Saw JH, Decho AW, Chain PSG, Boston PJ. Islands Within Islands: Bacterial Phylogenetic Structure and Consortia in Hawaiian Lava Caves and Fumaroles. Front Microbiol 2022; 13:934708. [PMID: 35935195 PMCID: PMC9349362 DOI: 10.3389/fmicb.2022.934708] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/03/2022] [Accepted: 06/16/2022] [Indexed: 11/15/2022] Open
Abstract
Lava caves, tubes, and fumaroles in Hawai‘i present a range of volcanic, oligotrophic environments from different lava flows and host unexpectedly high levels of bacterial diversity. These features provide an opportunity to study the ecological drivers that structure bacterial community diversity and assemblies in volcanic ecosystems and compare the older, more stable environments of lava tubes, to the more variable and extreme conditions of younger, geothermally active caves and fumaroles. Using 16S rRNA amplicon-based sequencing methods, we investigated the phylogenetic distinctness and diversity and identified microbial interactions and consortia through co-occurrence networks in 70 samples from lava tubes, geothermal lava caves, and fumaroles on the island of Hawai‘i. Our data illustrate that lava caves and geothermal sites harbor unique microbial communities, with very little overlap between caves or sites. We also found that older lava tubes (500–800 yrs old) hosted greater phylogenetic diversity (Faith's PD) than sites that were either geothermally active or younger (<400 yrs old). Geothermally active sites had a greater number of interactions and complexity than lava tubes. Average phylogenetic distinctness, a measure of the phylogenetic relatedness of a community, was higher than would be expected if communities were structured at random. This suggests that bacterial communities of Hawaiian volcanic environments are phylogenetically over-dispersed and that competitive exclusion is the main driver in structuring these communities. This was supported by network analyses that found that taxa (Class level) co-occurred with more distantly related organisms than close relatives, particularly in geothermal sites. Network “hubs” (taxa of potentially higher ecological importance) were not the most abundant taxa in either geothermal sites or lava tubes and were identified as unknown families or genera of the phyla, Chloroflexi and Acidobacteria. These results highlight the need for further study on the ecological role of microbes in caves through targeted culturing methods, metagenomics, and long-read sequence technologies.
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Affiliation(s)
- Rebecca D. Prescott
- Department of Environmental Health Sciences, Arnold School of Public Health, University of South Carolina, Columbia, SC, United States
- School of Life Sciences, University of Hawai‘i at Mānoa, Honolulu, HI, United States
- *Correspondence: Rebecca D. Prescott
| | - Tatyana Zamkovaya
- Department of Microbiology and Cell Science, University of Florida, Gainesville, FL, United States
| | - Stuart P. Donachie
- School of Life Sciences, University of Hawai‘i at Mānoa, Honolulu, HI, United States
| | - Diana E. Northup
- Department of Biology, University of New Mexico, Albuquerque, NM, United States
| | - Joseph J. Medley
- Department of Biology, University of New Mexico, Albuquerque, NM, United States
| | - Natalia Monsalve
- Department of Biological Sciences, The George Washington University, Washington, DC, United States
| | - Jimmy H. Saw
- Department of Biological Sciences, The George Washington University, Washington, DC, United States
| | - Alan W. Decho
- Department of Environmental Health Sciences, Arnold School of Public Health, University of South Carolina, Columbia, SC, United States
| | - Patrick S. G. Chain
- Biosciences Division, Los Alamos National Laboratory, Los Alamos, NM, United States
| | - Penelope J. Boston
- National Aeronautics and Space Administration (NASA) Ames Research Center, Moffett Field, CA, United States
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11
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Zheng Y, Yu S, Wang G, Xie F, Xu H, Du S, Zhao H, Sang X, Lu J, Jiang W. Comparative microbial antibiotic resistome between urban and deep forest environments. ENVIRONMENTAL MICROBIOLOGY REPORTS 2021; 13:503-508. [PMID: 33751816 DOI: 10.1111/1758-2229.12942] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/28/2020] [Revised: 02/25/2021] [Accepted: 02/25/2021] [Indexed: 06/12/2023]
Abstract
A paradoxical result of using antibiotics to eradicate microbial pathogens is the emergence of a vast number of resistant microbes in various environments. The concern that environmental microbes will inevitably become resistant to virtually every clinically usable antibiotics has been exacerbated by the spread of these resistance genes across different environments and the emergence of multidrug resistant phenotypes. Here, we provide metagenomic insights into the microbiomes and resistomes of 16 soil samples collected from hospitals, residential areas, and forest parks in the megacity of Beijing and deep forests in the Yunnan province. Using Illumina HiSeq sequencing, we investigated the microbial diversity within the metagenomic shotgun reads and identified 486 antibiotic-resistant genes (ARGs) classified into 30 types from these samples, among which multidrug resistance genes were the most abundant. Our results present an important reference and direct comparison of microbial antibiotic resistomes of soil samples from a megacity and deep forests and extend our understanding of the spread of ARGs in modern urban and natural environments.
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Affiliation(s)
- Yongchang Zheng
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Si Yu
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Guanqun Wang
- School of Life Sciences, Tsinghua University, Beijing, 100084, China
| | - Fucun Xie
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Haifeng Xu
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Shunda Du
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Haitao Zhao
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Xinting Sang
- Department of Liver Surgery, Peking Union Medical College Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College, Beijing, 100730, China
| | - Jizhou Lu
- Department of Liver Surgery, The Third People's Hospital of Gansu Province, Lanzhou, 730020, China
| | - Wenjun Jiang
- Department of Plant Pathology and Ministry of Agriculture and Rural Affairs Key Laboratory of Pest Monitoring and Green Management, College of Plant Protection, China Agricultural University, Beijing, 100193, China
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12
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Bacteria and Metabolic Potential in Karst Caves Revealed by Intensive Bacterial Cultivation and Genome Assembly. Appl Environ Microbiol 2021; 87:AEM.02440-20. [PMID: 33452024 DOI: 10.1128/aem.02440-20] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/05/2020] [Accepted: 01/05/2021] [Indexed: 12/26/2022] Open
Abstract
Karst caves are widely distributed subsurface systems, and the microbiomes therein are proposed to be the driving force for cave evolution and biogeochemical cycling. In past years, culture-independent studies on the microbiomes of cave systems have been conducted, yet intensive microbial cultivation is still needed to validate the sequence-derived hypothesis and to disclose the microbial functions in cave ecosystems. In this study, the microbiomes of two karst caves in Guizhou Province in southwest China were examined. A total of 3,562 bacterial strains were cultivated from rock, water, and sediment samples, and 329 species (including 14 newly described species) of 102 genera were found. We created a cave bacterial genome collection of 218 bacterial genomes from a karst cave microbiome through the extraction of 204 database-derived genomes and de novo sequencing of 14 new bacterial genomes. The cultivated genome collection obtained in this study and the metagenome data from previous studies were used to investigate the bacterial metabolism and potential involvement in the carbon, nitrogen, and sulfur biogeochemical cycles in the cave ecosystem. New N2-fixing Azospirillum and alkane-oxidizing Oleomonas species were documented in the karst cave microbiome. Two pcaIJ clusters of the β-ketoadipate pathway that were abundant in both the cultivated microbiomes and the metagenomic data were identified, and their representatives from the cultivated bacterial genomes were functionally demonstrated. This large-scale cultivation of a cave microbiome represents the most intensive collection of cave bacterial resources to date and provides valuable information and diverse microbial resources for future cave biogeochemical research.IMPORTANCE Karst caves are oligotrophic environments that are dark and humid and have a relatively stable annual temperature. The diversity of bacteria and their metabolisms are crucial for understanding the biogeochemical cycling in cave ecosystems. We integrated large-scale bacterial cultivation with metagenomic data mining to explore the compositions and metabolisms of the microbiomes in two karst cave systems. Our results reveal the presence of a highly diversified cave bacterial community, and 14 new bacterial species were described and their genomes sequenced. In this study, we obtained the most intensive collection of cultivated microbial resources from karst caves to date and predicted the various important routes for the biogeochemical cycling of elements in cave ecosystems.
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13
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Kimeklis AK, Gladkov GV, Zverev AO, Kichko AA, Andronov EE, Ergina EI, Kostenko IV, Abakumov EV. Microbiomes of different ages in Rendzic Leptosols in the Crimean Peninsula. PeerJ 2021; 9:e10871. [PMID: 33643711 PMCID: PMC7897411 DOI: 10.7717/peerj.10871] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/21/2020] [Accepted: 01/10/2021] [Indexed: 01/04/2023] Open
Abstract
Rendzic Leptosols are intrazonal soils formed on limestone bedrock. The specialty of these soils is that parent rock material is more influential in shaping soil characteristics than zonal factors such as climate, especially during soil formation. Unlike fast evolving Podzols due to their leaching regime, Leptosols do not undergo rapid development due to the nature of the limestone. Little is known how microbiome reflects this process, so we assessed microbiome composition of Rendzic Leptosols of different ages, arising from disruption and subsequent reclamation. The mountains and foothills that cover much of the Crimean Peninsula are ideal for this type of study, as the soils were formed on limestone and have been subjected to anthropogenic impacts through much of human history. Microbiomes of four soil sites forming a chronosequence, including different soil horizons, were studied using sequencing of 16S rRNA gene libraries and quantitative PCR. Dominant phyla for all soil sites were Actinobacteria, Proteobacteria, Acidobacteria, Bacteroidetes, Thaumarchaeota, Planctomycetes, Verrucomicrobia and Firmicutes. Alpha diversity was similar across sites and tended to be higher in topsoil. Beta diversity showed that microbiomes diverged according to the soil site and the soil horizon. The oldest and the youngest soils had the most similar microbiomes, which could have been caused by their geographic proximity. Oligotrophic bacteria from Chitinophagaceae, Blastocatellaceae and Rubrobacteriaceae dominated the microbiome of these soils. The microbiome of 700-year old soil was the most diverse. This soil was from the only study location with topsoil formed by plant litter, which provided additional nutrients and could have been the driving force of this differentiation. Consistent with this assumption, this soil was abundant in copiotrophic bacteria from Proteobacteria and Actinobacteria phyla. The microbiome of 50-year old Leptosol was more similar to the microbiome of benchmark soil than the microbiome of 700-year old soil, especially by weighted metrics. CCA analysis, in combination with PERMANOVA, linked differences in microbiomes to the joint change of all soil chemical parameters between soil horizons. Local factors, such as parent material and plant litter, more strongly influenced the microbiome composition in Rendzic Leptosols than soil age.
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Affiliation(s)
- Anastasiia K Kimeklis
- Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia.,Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia
| | - Grigory V Gladkov
- Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia.,Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia
| | - Aleksei O Zverev
- Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia.,Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia
| | - Arina A Kichko
- Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia.,Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia
| | - Evgeny E Andronov
- Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia.,Genetics and Biotechnology, St. Petersburg State University, Saint-Petersburg, Russia.,V.V. Dokuchaev Soil Science Institute, Moscow, Russia
| | - Elena I Ergina
- V.I. Vernadsky Crimean Federal University, Simferopol, Russia
| | - Igor V Kostenko
- Nikitsky Botanical Garden -National Scientific Center, Yalta, Russia
| | - Evgeny V Abakumov
- Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia.,Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia
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14
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Mammola S, Amorim IR, Bichuette ME, Borges PAV, Cheeptham N, Cooper SJB, Culver DC, Deharveng L, Eme D, Ferreira RL, Fišer C, Fišer Ž, Fong DW, Griebler C, Jeffery WR, Jugovic J, Kowalko JE, Lilley TM, Malard F, Manenti R, Martínez A, Meierhofer MB, Niemiller ML, Northup DE, Pellegrini TG, Pipan T, Protas M, Reboleira ASPS, Venarsky MP, Wynne JJ, Zagmajster M, Cardoso P. Fundamental research questions in subterranean biology. Biol Rev Camb Philos Soc 2020; 95:1855-1872. [DOI: 10.1111/brv.12642] [Citation(s) in RCA: 51] [Impact Index Per Article: 12.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/09/2020] [Revised: 07/31/2020] [Accepted: 07/31/2020] [Indexed: 12/27/2022]
Affiliation(s)
- Stefano Mammola
- Laboratory for Integrative Biodiversity Research (LIBRe), Finnish Museum of Natural History (LUOMUS) University of Helsinki Pohjoinen Rautatiekatu 13 Helsinki 00100 Finland
- Molecular Ecology Group (MEG) Water Research Institute (IRSA), National Research Council (CNR) Corso Tonolli, 50 Pallanza 28922 Italy
| | - Isabel R. Amorim
- cE3c – Centre for Ecology Evolution and Environmental Changes/Azorean Biodiversity Group and Universidade dos Açores, Faculty of Agrarian and Environmental Sciences, Rua Capitão João d'Àvila Pico da Urze Angra do Heroísmo Azores 9700‐042 Portugal
| | - Maria E. Bichuette
- Laboratory of Subterranean Studies Federal University of São Carlos Rodovia Washington Luís km 235 São Carlos São Paulo 13565‐905 Brazil
| | - Paulo A. V. Borges
- cE3c – Centre for Ecology Evolution and Environmental Changes/Azorean Biodiversity Group and Universidade dos Açores, Faculty of Agrarian and Environmental Sciences, Rua Capitão João d'Àvila Pico da Urze Angra do Heroísmo Azores 9700‐042 Portugal
| | - Naowarat Cheeptham
- Department of Biological Sciences, Faculty of Science Thompson Rivers University 805 TRU Way Kamloops British Columbia Canada
| | - Steven J. B. Cooper
- Evolutionary Biology Unit South Australian Museum North Terrace Adelaide South Australia 5000 Australia
- Australian Centre for Evolutionary Biology and Biodiversity, and Environment Institute, School of Biological Sciences University of Adelaide Adelaide South Australia 5005 Australia
| | - David C. Culver
- Department of Environmental Science American University 4400 Massachusetts Avenue, N.W. Washington DC 20016 U.S.A
| | - Louis Deharveng
- UMR7205 – ISYEB Museum national d'Histoire naturelle 45 rue Buffon (CP50) Paris 75005 France
| | - David Eme
- IFREMER Centre Atlantique Unité Ecologie et Modèles pour l'Halieutique Rue de l'Île d'Yeu Nantes 44980 France
| | - Rodrigo Lopes Ferreira
- Center of Studies in Subterranean Biology, Biology Department Federal University of Lavras Campus Universitário Lavras Minas Gerais CEP 37202‐553 Brazil
| | - Cene Fišer
- SubBio Lab, Department of Biology, Biotechnical Faculty University of Ljubljana Jamnikarjeva 101, PO BOX 2995 Ljubljana SI‐1000 Slovenia
| | - Žiga Fišer
- SubBio Lab, Department of Biology, Biotechnical Faculty University of Ljubljana Jamnikarjeva 101, PO BOX 2995 Ljubljana SI‐1000 Slovenia
| | - Daniel W. Fong
- Department of Biology American University 4400 Massachusetts Avenue, N.W. Washington DC 20016 U.S.A
| | - Christian Griebler
- Department of Functional and Evolutionary Ecology, Division of Limnology University of Vienna Althanstrasse 14 Vienna 1090 Austria
| | - William R. Jeffery
- Department of Biology University of Maryland College Park MD 20742 U.S.A
| | - Jure Jugovic
- Department of Biodiversity, Faculty of Mathematics, Natural Sciences and Information Technologies University of Primorska Glagoljaška 8 Koper SI‐6000 Slovenia
| | - Johanna E. Kowalko
- Harriet L. Wilkes Honors College Florida Atlantic University 5353 Parkside Dr Jupiter FL 33458 U.S.A
| | - Thomas M. Lilley
- BatLab Finland, Finnish Museum of Natural History University of Helsinki Pohjoinen Rautatiekatu 13 Helsinki 00100 Finland
| | - Florian Malard
- UMR5023 Ecologie des Hydrosystèmes Naturels et Anthropisés Univ. Lyon 1, ENTPE, CNRS, Université de Lyon, Bat. Forel 6 rue Raphaël Dubois Villeurbanne cedex 69622 France
| | - Raoul Manenti
- Department of Environmental Science and Policy Università degli Studi di Milano Via Celoria 26 Milan 20113 Italy
| | - Alejandro Martínez
- Molecular Ecology Group (MEG) Water Research Institute (IRSA), National Research Council (CNR) Corso Tonolli, 50 Pallanza 28922 Italy
| | - Melissa B. Meierhofer
- BatLab Finland, Finnish Museum of Natural History University of Helsinki Pohjoinen Rautatiekatu 13 Helsinki 00100 Finland
- Department of Rangeland, Wildlife and Fisheries Management Texas A&M University 534 John Kimbrough Blvd. College Station TX 77843 U.S.A
| | - Matthew L. Niemiller
- Department of Biological Sciences The University of Alabama in Huntsville 301 Sparkman Drive NW Huntsville AL 35899 U.S.A
| | - Diana E. Northup
- Department of Biology University of New Mexico Albuquerque NM 87131‐0001 U.S.A
| | - Thais G. Pellegrini
- Center of Studies in Subterranean Biology, Biology Department Federal University of Lavras Campus Universitário Lavras Minas Gerais CEP 37202‐553 Brazil
| | - Tanja Pipan
- ZRC SAZU Karst Research Institute Novi trg 2 Ljubljana SI‐1000 Slovenia
- UNESCO Chair on Karst Education University of Nova Gorica Vipavska cesta Nova Gorica 5000 Slovenia
| | - Meredith Protas
- Department of Natural Sciences and Mathematics Domenicas University of California 50 Acacia Avenue San Rafael CA 94901 U.S.A
| | - Ana Sofia P. S. Reboleira
- Natural History Museum of Denmark University of Copenhagen Universitetsparken 15 Copenhagen 2100 Denmark
| | - Michael P. Venarsky
- Australian Rivers Institute Griffith University 170 Kessels Road Nathan Queensland 4111 Australia
| | - J. Judson Wynne
- Department of Biological Sciences, Center for Adaptable Western Landscapes Northern Arizona University Box 5640 Flagstaff AZ 86011 U.S.A
| | - Maja Zagmajster
- SubBio Lab, Department of Biology, Biotechnical Faculty University of Ljubljana Jamnikarjeva 101, PO BOX 2995 Ljubljana SI‐1000 Slovenia
| | - Pedro Cardoso
- Laboratory for Integrative Biodiversity Research (LIBRe), Finnish Museum of Natural History (LUOMUS) University of Helsinki Pohjoinen Rautatiekatu 13 Helsinki 00100 Finland
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15
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Marlow JJ, Colocci I, Jungbluth SP, Weber NM, Gartman A, Kallmeyer J. Mapping metabolic activity at single cell resolution in intact volcanic fumarole sediment. FEMS Microbiol Lett 2020; 367:5736014. [DOI: 10.1093/femsle/fnaa031] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/20/2019] [Accepted: 02/13/2020] [Indexed: 12/11/2022] Open
Abstract
ABSTRACT
Interactions among microorganisms and their mineralogical substrates govern the structure, function and emergent properties of microbial communities. These interactions are predicated on spatial relationships, which dictate metabolite exchange and access to key substrates. To quantitatively assess links between spatial relationships and metabolic activity, this study presents a novel approach to map all organisms, the metabolically active subset and associated mineral grains, all while maintaining spatial integrity of an environmental microbiome. We applied this method at an outgassing fumarole of Vanuatu's Marum Crater, one of the largest point sources of several environmentally relevant gaseous compounds, including H2O, CO2 and SO2. With increasing distance from the sediment-air surface and from mineral grain outer boundaries, organism abundance decreased but the proportion of metabolically active organisms often increased. These protected niches may provide more stable conditions that promote consistent metabolic activity of a streamlined community. Conversely, exterior surfaces accumulate more organisms that may cover a wider range of preferred conditions, implying that only a subset of the community will be active under any particular environmental regime. More broadly, the approach presented here allows investigators to see microbial communities ‘as they really are’ and explore determinants of metabolic activity across a range of microbiomes.
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Affiliation(s)
- Jeffrey J Marlow
- Department of Organismic and Evolutionary Biology, Harvard University, 16 Divinity Ave., Cambridge, MA, 02138, USA
| | - Isabella Colocci
- Department of Organismic and Evolutionary Biology, Harvard University, 16 Divinity Ave., Cambridge, MA, 02138, USA
| | - Sean P Jungbluth
- United States Department of Energy, Joint Genome Institute, 2800 Mitchell Dr, Walnut Creek, California, 94598, USA
| | - Nils Moritz Weber
- GFZ German Research Centre for Geosciences, Section 3.7 Geomicrobiology, Telegrafenberg, 14473 Potsdam, Germany
| | - Amy Gartman
- United States Geological Survey, 2885 Mission Street Santa Cruz, CA 95060, USA
| | - Jens Kallmeyer
- GFZ German Research Centre for Geosciences, Section 3.7 Geomicrobiology, Telegrafenberg, 14473 Potsdam, Germany
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16
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Yan D, Gellie NJC, Mills JG, Connell G, Bissett A, Lowe AJ, Breed MF. A soil archaeal community responds to a decade of ecological restoration. Restor Ecol 2019. [DOI: 10.1111/rec.13033] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Affiliation(s)
- DongFeng Yan
- College of Forestry Henan Agricultural University, Nongye Road Zhengzhou 450002 China
- School of Biological Sciences and the Environment Institute University of Adelaide Adelaide SA 5005 Australia
| | - Nicholas J. C. Gellie
- School of Biological Sciences and the Environment Institute University of Adelaide Adelaide SA 5005 Australia
| | - Jacob G. Mills
- School of Biological Sciences and the Environment Institute University of Adelaide Adelaide SA 5005 Australia
| | - Gemma Connell
- School of Biological Sciences and the Environment Institute University of Adelaide Adelaide SA 5005 Australia
| | | | - Andrew J. Lowe
- School of Biological Sciences and the Environment Institute University of Adelaide Adelaide SA 5005 Australia
| | - Martin F. Breed
- School of Biological Sciences and the Environment Institute University of Adelaide Adelaide SA 5005 Australia
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