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Viladomat Jasso M, García-Ulloa M, Zapata-Peñasco I, Eguiarte LE, Souza V. Metagenomic insight into taxonomic composition, environmental filtering and functional redundancy for shaping worldwide modern non-lithifying microbial mats. PeerJ 2024; 12:e17412. [PMID: 38827283 PMCID: PMC11144394 DOI: 10.7717/peerj.17412] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/30/2023] [Accepted: 04/26/2024] [Indexed: 06/04/2024] Open
Abstract
Modern microbial mats are relictual communities mostly found in extreme environments worldwide. Despite their significance as representatives of the ancestral Earth and their important roles in biogeochemical cycling, research on microbial mats has largely been localized, focusing on site-specific descriptions and environmental change experiments. Here, we present a global comparative analysis of non-lithifying microbial mats, integrating environmental measurements with metagenomic data from 62 samples across eight sites, including two new samples from the recently discovered Archaean Domes from Cuatro Ciénegas, Mexico. Our results revealed a notable influence of environmental filtering on both taxonomic and functional compositions of microbial mats. Functional redundancy appears to confer resilience to mats, with essential metabolic pathways conserved across diverse and highly contrasting habitats. We identified six highly correlated clusters of taxa performing similar ecological functions, suggesting niche partitioning and functional specialization as key mechanisms shaping community structure. Our findings provide insights into the ecological principles governing microbial mats, and lay the foundation for future research elucidating the intricate interplay between environmental factors and microbial community dynamics.
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Affiliation(s)
- Mariette Viladomat Jasso
- Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional Autónoma de México, Ciudad de México, Mexico
| | | | - Icoquih Zapata-Peñasco
- Dirección de Investigación en Transformación de Hidrocarburos, Instituto Mexicano del Petróleo, Ciudad de México, Mexico
| | - Luis E. Eguiarte
- Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional Autónoma de México, Ciudad de México, Mexico
| | - Valeria Souza
- Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional Autónoma de México, Ciudad de México, Mexico
- Centro de Estudios del Cuaternario de Fuego-Patagonia y Antártica (CEQUA), Punta Arenas, Chile
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2
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Águila B, Yanez-Montalvo A, Mercado-Juárez RA, Montejano GA, Becerra-Absalón I, Falcón LI. Microbialites show a distinct cyanobacterial phylogenetic structure and functional redundancy in Bacalar lagoon and Cenote Azul sinkhole, Yucatan peninsula, Mexico. FEMS Microbiol Ecol 2022; 98:6564597. [PMID: 35388893 DOI: 10.1093/femsec/fiac039] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/23/2021] [Revised: 02/03/2022] [Accepted: 04/05/2022] [Indexed: 11/13/2022] Open
Abstract
Cyanobacterial components of microbialites from two geographically close systems, the Bacalar lagoon (BL) and the Cenote Azul sinkhole (CA) in Quintana Roo, Mexico, were characterized. BL and CA systems were studied along a longitudinal gradient (north to south) and a depth gradient (5 to 30 m), respectively. Microscopic observations, 16S rRNA amplicon sequencing, and shotgun metagenomics were used to characterize Cyanobacteria. Both systems showed similar metabolic/functional profiles but harbored completely different cyanobacterial taxa. BL was dominated by Nostocales, including a population of previously undescribed Chakia sp., while CA was dominated by an unknown taxon of Chroococcales, comprising 70% of relative abundance through all depths. Interestingly, cyanobacterial assemblages in microbialites exhibited phylogenetic overdispersion in most of the BL sites, while CA sites exhibited phylogenetic clustering, these differences were attributed to depth/light conditions and possibly different times of geological formation for BL and CA systems.
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Affiliation(s)
- B Águila
- Instituto de Ecología, UNAM Campus Yucatán, Parque Científico y Tecnológico de Yucatán, 97302, México.,Instituto de Ecología, UNAM, Coyoacán, CdMx 04510, México.,Posgrado en Ciencias Biológicas, Unidad de Posgrado, Edificio A, 1° Piso, Circuito de Posgrados CU, Coyoacán, CdMx 04510, México
| | - A Yanez-Montalvo
- El Colegio de la Frontera Sur Unidad Chetumal, Av. Centenario Km. 5.5, Chetumal, Quintana Roo, 77014, México
| | - R A Mercado-Juárez
- Instituto de Ecología, UNAM Campus Yucatán, Parque Científico y Tecnológico de Yucatán, 97302, México.,Instituto de Ecología, UNAM, Coyoacán, CdMx 04510, México.,Posgrado en Ciencias Biológicas, Unidad de Posgrado, Edificio A, 1° Piso, Circuito de Posgrados CU, Coyoacán, CdMx 04510, México
| | - G A Montejano
- UNAM, Laboratorio de Ficología, Facultad de Ciencias, Av. Universidad 3000, CdMx 04510, México
| | - I Becerra-Absalón
- UNAM, Laboratorio de Ficología, Facultad de Ciencias, Av. Universidad 3000, CdMx 04510, México
| | - L I Falcón
- Instituto de Ecología, UNAM Campus Yucatán, Parque Científico y Tecnológico de Yucatán, 97302, México.,Instituto de Ecología, UNAM, Coyoacán, CdMx 04510, México
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3
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Medina Ferrer F, Rosen MR, Feyhl-Buska J, Russell VV, Sønderholm F, Loyd S, Shapiro R, Stamps BW, Petryshyn V, Demirel-Floyd C, Bailey JV, Johnson HA, Spear JR, Corsetti FA. Potential role for microbial ureolysis in the rapid formation of carbonate tufa mounds. GEOBIOLOGY 2022; 20:79-97. [PMID: 34337850 DOI: 10.1111/gbi.12467] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/23/2021] [Accepted: 07/10/2021] [Indexed: 06/13/2023]
Abstract
Modern carbonate tufa towers in the alkaline (~pH 9.5) Big Soda Lake (BSL), Nevada, exhibit rapid precipitation rates (exceeding 3 cm/year) and host diverse microbial communities. Geochemical indicators reveal that carbonate precipitation is, in part, promoted by the mixing of calcium-rich groundwater and carbonate-rich lake water, such that a microbial role for carbonate precipitation is unknown. Here, we characterize the BSL microbial communities and evaluate their potential effects on carbonate precipitation that may influence fast carbonate precipitation rates of the active tufa mounds of BSL. Small subunit rRNA gene surveys indicate a diverse microbial community living endolithically, in interior voids, and on tufa surfaces. Metagenomic DNA sequencing shows that genes associated with metabolisms that are capable of increasing carbonate saturation (e.g., photosynthesis, ureolysis, and bicarbonate transport) are abundant. Enzyme activity assays revealed that urease and carbonic anhydrase, two microbial enzymes that promote carbonate precipitation, are active in situ in BSL tufa biofilms, and urease also increased calcium carbonate precipitation rates in laboratory incubation analyses. We propose that, although BSL tufas form partially as a result of water mixing, tufa-inhabiting microbiota promote rapid carbonate authigenesis via ureolysis, and potentially via bicarbonate dehydration and CO2 outgassing by carbonic anhydrase. Microbially induced calcium carbonate precipitation in BSL tufas may generate signatures preserved in the carbonate microfabric, such as stromatolitic layers, which could serve as models for developing potential biosignatures on Earth and elsewhere.
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Affiliation(s)
- Fernando Medina Ferrer
- Department of Earth & Environmental Sciences, University of Minnesota, Twin Cities, Minneapolis, Minnesota, USA
| | - Michael R Rosen
- US Geological Survey, California Water Science Center, Carson City, Nevada, USA
| | - Jayme Feyhl-Buska
- Department of Earth Sciences, University of Southern California, Los Angeles, California, USA
| | - Virginia V Russell
- Department of Plant and Microbial Biology, University of California, Berkeley, Berkeley, California, USA
| | - Fredrik Sønderholm
- Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, Denmark
| | - Sean Loyd
- Department of Geological Sciences, California State University Fullerton, Fullerton, California, USA
| | | | - Blake W Stamps
- 711th Human Performance Wing, Air Force Research Laboratory, Wright-Patterson Air Force Base, Dayton, Ohio, USA
- UES, Inc., Dayton, Ohio, USA
| | - Victoria Petryshyn
- Environmental Studies Program, University of Southern California, Los Angeles, California, USA
| | | | - Jake V Bailey
- Department of Earth & Environmental Sciences, University of Minnesota, Twin Cities, Minneapolis, Minnesota, USA
| | - Hope A Johnson
- Department of Biological Science, California State University Fullerton, Fullerton, California, USA
| | - John R Spear
- Department of Civil and Environmental Engineering, Colorado School of Mines, Golden, Colorado, USA
| | - Frank A Corsetti
- Department of Earth Sciences, University of Southern California, Los Angeles, California, USA
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4
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Waterworth SC, Isemonger EW, Rees ER, Dorrington RA, Kwan JC. Conserved bacterial genomes from two geographically isolated peritidal stromatolite formations shed light on potential functional guilds. ENVIRONMENTAL MICROBIOLOGY REPORTS 2021; 13:126-137. [PMID: 33369160 PMCID: PMC8408775 DOI: 10.1111/1758-2229.12916] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/01/2020] [Revised: 11/17/2020] [Accepted: 12/06/2020] [Indexed: 05/24/2023]
Abstract
Stromatolites are complex microbial mats that form lithified layers. Fossilized stromatolites are the oldest evidence of cellular life on Earth, dating back over 3.4 billion years. Modern stromatolites are relatively rare but may provide clues about the function and evolution of their ancient counterparts. In this study, we focus on peritidal stromatolites occurring at Cape Recife and Schoenmakerskop on the southeastern South African coastline, the former being morphologically and structurally similar to fossilized phosphatic stromatolites formations. Using assembled shotgun metagenomic analysis, we obtained 183 genomic bins, of which the most dominant taxa were from the Cyanobacteria phylum. We identified functional gene sets in genomic bins conserved across two geographically isolated stromatolite formations, which included relatively high copy numbers of genes involved in the reduction of nitrates and phosphatic compounds. Additionally, we found little evidence of Archaeal species in these stromatolites, suggesting that they may not play an important role in peritidal stromatolite formations, as proposed for hypersaline formations.
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Affiliation(s)
- Samantha C. Waterworth
- Division of Pharmaceutical Sciences, University of Wisconsin, Madison, Wisconsin 53705, USA
| | - Eric W. Isemonger
- Department of Biochemistry and Microbiology, Rhodes University, Grahamstown, South Africa
| | - Evan R. Rees
- Division of Pharmaceutical Sciences, University of Wisconsin, Madison, Wisconsin 53705, USA
| | - Rosemary A. Dorrington
- Department of Biochemistry and Microbiology, Rhodes University, Grahamstown, South Africa
| | - Jason C. Kwan
- Division of Pharmaceutical Sciences, University of Wisconsin, Madison, Wisconsin 53705, USA
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5
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Iniesto M, Moreira D, Reboul G, Deschamps P, Benzerara K, Bertolino P, Saghaï A, Tavera R, López-García P. Core microbial communities of lacustrine microbialites sampled along an alkalinity gradient. Environ Microbiol 2020; 23:51-68. [PMID: 32985763 DOI: 10.1111/1462-2920.15252] [Citation(s) in RCA: 15] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/31/2020] [Revised: 08/26/2020] [Accepted: 09/23/2020] [Indexed: 11/28/2022]
Abstract
Microbialites are usually carbonate-rich sedimentary rocks formed by the interplay of phylogenetically and metabolically complex microbial communities with their physicochemical environment. Yet, the biotic and abiotic determinants of microbialite formation remain poorly constrained. Here, we analysed the structure of prokaryotic and eukaryotic communities associated with microbialites occurring in several crater lakes of the Trans-Mexican volcanic belt along an alkalinity gradient. Microbialite size and community structure correlated with lake physicochemical parameters, notably alkalinity. Although microbial community composition varied across lake microbialites, major taxa-associated functions appeared quite stable with both, oxygenic and anoxygenic photosynthesis and, to less extent, sulphate reduction, as major putative carbonatogenic processes. Despite interlake microbialite community differences, we identified a microbial core of 247 operational taxonomic units conserved across lake microbialites, suggesting a prominent ecological role in microbialite formation. This core mostly encompassed Cyanobacteria and their typical associated taxa (Bacteroidetes, Planctomycetes) and diverse anoxygenic photosynthetic bacteria, notably Chloroflexi, Alphaproteobacteria (Rhodobacteriales, Rhodospirilalles), Gammaproteobacteria (Chromatiaceae) and minor proportions of Chlorobi. The conserved core represented up to 40% (relative abundance) of the total community in lakes Alchichica and Atexcac, displaying the highest alkalinities and the most conspicuous microbialites. Core microbialite communities associated with carbonatogenesis might be relevant for inorganic carbon sequestration purposes.
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Affiliation(s)
- Miguel Iniesto
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - David Moreira
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Guillaume Reboul
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Philippe Deschamps
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Karim Benzerara
- Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, CNRS, Muséum National d'Histoire Naturelle, Sorbonne Université, Paris, France
| | - Paola Bertolino
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Aurélien Saghaï
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France.,Department of Forest Mycology and Plant Pathology, Swedish University of Agricultural Sciences, Uppsala, Sweden
| | - Rosaluz Tavera
- Departamento de Ecología y Recursos Naturales, Universidad Nacional Autónoma de México, DF Mexico, Mexico
| | - Purificación López-García
- Unité d'Ecologie Systématique et Evolution, CNRS, Université Paris-Saclay, AgroParisTech, Orsay, France
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6
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White RA, Soles SA, Brady AL, Southam G, Lim DS, Slater GF. Biosignatures Associated with Freshwater Microbialites. Life (Basel) 2020; 10:life10050066. [PMID: 32429118 PMCID: PMC7281397 DOI: 10.3390/life10050066] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/31/2020] [Revised: 05/11/2020] [Accepted: 05/11/2020] [Indexed: 12/18/2022] Open
Abstract
Freshwater microbialites (i.e., lithifying microbial mats) are quite rare in northern latitudes of the North American continent, with two lakes (Pavilion and Kelly Lakes) of southeastern BC containing a morphological variety of such structures. We investigated Kelly Lake microbialites using carbon isotope systematics, phospholipid fatty acids (PLFAs) and quantitative PCR to obtain biosignatures associated with microbial metabolism. δ13CDIC values (mean δ13CDIC −4.9 ± 1.1‰, n = 8) were not in isotopic equilibrium with the atmosphere; however, they do indicate 13C-depleted inorganic carbon into Kelly Lake. The values of carbonates on microbialite surfaces (δ13C) fell within the range predicted for equilibrium precipitation from ambient lake water δ13CDIC (−2.2 to −5.3‰). Deep microbialites (26 m) had an enriched δ13Ccarb value of −0.3 ± 0.5‰, which is a signature of photoautotrophy. The deeper microbialites (>20 m) had higher biomass estimates (via PLFAs), and a greater relative abundance of cyanobacteria (measured by 16S copies via qPCR). The majority of PLFAs constituted monounsaturated and saturated PLFAs, which is consistent with gram-negative bacteria, including cyanobacteria. The central PLFA δ13C values were highly depleted (−9.3 to −15.7‰) relative to δ13C values of bulk organic matter, suggesting a predominance of photoautotrophy. A heterotrophic signature was also detected via the depleted iso- and anteiso-15:0 lipids (−3.2 to −5.2‰). Based on our carbonate isotopic biosignatures, PLFA, and qPCR measurements, photoautotrophy is enriched in the microbialites of Kelly Lake. This photoautotrophy enrichment is consistent with the microbialites of neighboring Pavilion Lake. This indication of photoautotrophy within Kelly Lake at its deepest depths raises new insights into the limits of measurable carbonate isotopic biosignatures under light and nutrient limitations.
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Affiliation(s)
- Richard Allen White
- Department of Plant Pathology, Washington State University, Pullman, WA 99163, USA;
- RAW Molecular Systems (RMS) LLC, Spokane, WA 99218, USA
- Australian Centre for Astrobiology, University of New South Wales, Sydney, NSW 2052, Australia
| | - Sarah A. Soles
- School of Geography and Earth Sciences, McMaster University, Hamilton, ON L8S 4K1, Canada; (S.A.S.); (A.L.B.)
| | - Allyson L. Brady
- School of Geography and Earth Sciences, McMaster University, Hamilton, ON L8S 4K1, Canada; (S.A.S.); (A.L.B.)
| | - Gordon Southam
- School of Earth and Environmental Sciences, University of Queensland, QLD 4072, Australia;
| | | | - Greg F. Slater
- School of Geography and Earth Sciences, McMaster University, Hamilton, ON L8S 4K1, Canada; (S.A.S.); (A.L.B.)
- Correspondence: ; Tel.: +1-905-525-9140 (ext. 26388)
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7
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Unexpected Abundance and Diversity of Phototrophs in Mats from Morphologically Variable Microbialites in Great Salt Lake, Utah. Appl Environ Microbiol 2020; 86:AEM.00165-20. [PMID: 32198176 DOI: 10.1128/aem.00165-20] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/20/2020] [Accepted: 03/15/2020] [Indexed: 11/20/2022] Open
Abstract
Microbial mat communities are associated with extensive (∼700 km2) and morphologically variable carbonate structures, termed microbialites, in the hypersaline Great Salt Lake (GSL), Utah. However, whether the composition of GSL mat communities covaries with microbialite morphology and lake environment is unknown. Moreover, the potential adaptations that allow the establishment of these extensive mat communities at high salinity (14% to 17% total salts) are poorly understood. To address these questions, microbial mats were sampled from seven locations in the south arm of GSL representing different lake environments and microbialite morphologies. Despite the morphological differences, microbialite-associated mats were taxonomically similar and were dominated by the cyanobacterium Euhalothece and several heterotrophic bacteria. Metagenomic sequencing of a representative mat revealed Euhalothece and subdominant Thiohalocapsa populations that harbor the Calvin cycle and nitrogenase, suggesting they supply fixed carbon and nitrogen to heterotrophic bacteria. Fifteen of the next sixteen most abundant taxa are inferred to be aerobic heterotrophs and, surprisingly, harbor reaction center, rhodopsin, and/or bacteriochlorophyll biosynthesis proteins, suggesting aerobic photoheterotrophic (APH) capabilities. Importantly, proteins involved in APH are enriched in the GSL community relative to that in microbialite mat communities from lower salinity environments. These findings indicate that the ability to integrate light into energy metabolism is a key adaptation allowing for robust mat development in the hypersaline GSL.IMPORTANCE The earliest evidence of life on Earth is from organosedimentary structures, termed microbialites, preserved in 3.481-billion-year-old (Ga) rocks. Phototrophic microbial mats form in association with an ∼700-km2 expanse of morphologically diverse microbialites in the hypersaline Great Salt Lake (GSL), Utah. Here, we show taxonomically similar microbial mat communities are associated with morphologically diverse microbialites across the lake. Metagenomic sequencing reveals an abundance and diversity of autotrophic and heterotrophic taxa capable of harvesting light energy to drive metabolism. The unexpected abundance of and diversity in the mechanisms of harvesting light energy observed in GSL mat populations likely function to minimize niche overlap among coinhabiting taxa, provide a mechanism(s) to increase energy yield and osmotic balance during salt stress, and enhance fitness. Together, these physiological benefits promote the formation of robust mats that, in turn, influence the formation of morphologically diverse microbialite structures that can be imprinted in the rock record.
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8
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DeMott LM, Napieralski SA, Junium CK, Teece M, Scholz CA. Microbially influenced lacustrine carbonates: A comparison of Late Quaternary Lahontan tufa and modern thrombolite from Fayetteville Green Lake, NY. GEOBIOLOGY 2020; 18:93-112. [PMID: 31682069 DOI: 10.1111/gbi.12367] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/02/2019] [Revised: 09/15/2019] [Accepted: 10/09/2019] [Indexed: 06/10/2023]
Abstract
Carbonate microbialites in lakes can serve as valuable indicators of past environments, so long as the biogenicity and depositional setting of the microbialite can be accurately determined. Late Pleistocene to Early Holocene frondose draping tufa deposits from Winnemucca Dry Lake (Nevada, USA), a subbasin of pluvial Lake Lahontan, were examined in outcrop, petrographically, and geochemically to determine whether microbially induced precipitation is a dominant control on deposition. These observations were compared to modern, actively accumulating microbialites from Fayetteville Green Lake (New York, USA) using similar methods. In addition, preserved microbial DNA was extracted from the Lahontan tufa and sequenced to provide a more complete picture of the microbial communities. Tufas are texturally and geochemically similar to modern thrombolitic microbialites from Fayetteville Green Lake, and the stable isotopic composition of organic C, N, inorganic C, and O supports deposition associated with a lacustrine microbial mat environment dominated by photosynthetic processes. DNA extraction and sequencing indicate that photosynthetic microbial builders were present during tufa deposition, primarily Chloroflexi and Proteobacteria with minor abundances of Cyanobacteria and Acidobacteria. Based on the sequencing results, the depositional environment of the tufas can be constrained to the photic zone of the lake, contrasting with some previous interpretations that put tufa formation in deeper waters. Additionally, the presence of a number of mesothermophilic phyla, including Deinococcus-Thermus, indicates that thermal groundwater may have played a role in tufa deposition at sites not previously associated with groundwater influx. The interpretation of frondose tufas as microbially influenced deposits provides new context to interpretations of lake level and past environments in the Lahontan lake basins.
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Affiliation(s)
- Laura M DeMott
- Department of Earth Sciences, Syracuse University, Syracuse, New York, USA
| | | | | | - Mark Teece
- Chemistry Department, State University of New York College of Environmental Science and Forestry, Syracuse, New York, USA
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9
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Methods for extracting 'omes from microbialites. J Microbiol Methods 2019; 160:1-10. [PMID: 30877015 DOI: 10.1016/j.mimet.2019.02.014] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/23/2018] [Revised: 02/21/2019] [Accepted: 02/21/2019] [Indexed: 11/20/2022]
Abstract
Microbialites are organo-sedimentary structures formed by complex microbial communities that interact with abiotic factors to form carbonate rich fabrics. Extraction of DNA or total RNA from microbialites can be difficult because of the high carbonate mineral concentration and exopolymeric substances. The methods employed until now include substances such as cetyltrimethylammonium bromide, sodium dodecyl sulfate, xanthogenate, lysozyme and proteinase K, as well as mechanical disruption. Additionally, several commercial kits have been used to improve DNA and total RNA extraction. This minireview presents different methods applied for DNA and RNA extraction from microbialites and discusses their advantages and disadvantages. Moreover, extraction of all 'omes (DNA, RNA, Protein, Lipids, polar metabolites) using multiomic extraction methods (MPlex), as well as the state of art for extraction of viruses from microbialites, are also discussed.
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10
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Johnson DB, Beddows PA, Flynn TM, Osburn MR. Microbial diversity and biomarker analysis of modern freshwater microbialites from Laguna Bacalar, Mexico. GEOBIOLOGY 2018; 16:319-337. [PMID: 29656514 DOI: 10.1111/gbi.12283] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/01/2017] [Accepted: 02/12/2018] [Indexed: 06/08/2023]
Abstract
Laguna Bacalar is a sulfate-rich freshwater lake on the Yucatan Peninsula that hosts large microbialites. High sulfate concentrations distinguish Laguna Bacalar from other freshwater microbialite sites such as Pavilion Lake and Alchichica, Mexico, as well as from other aqueous features on the Yucatan Peninsula. While cyanobacterial populations have been described here previously, this study offers a more complete characterization of the microbial populations and corresponding biogeochemical cycling using a three-pronged geobiological approach of microscopy, high-throughput DNA sequencing, and lipid biomarker analyses. We identify and compare diverse microbial communities of Alphaproteobacteria, Deltaproteobacteria, and Gammaproteobacteria that vary with location along a bank-to-bank transect across the lake, within microbialites, and within a neighboring mangrove root agglomeration. In particular, sulfate-reducing bacteria are extremely common and diverse, constituting 7%-19% of phylogenetic diversity within the microbialites, and are hypothesized to significantly influence carbonate precipitation. In contrast, Cyanobacteria account for less than 1% of phylogenetic diversity. The distribution of lipid biomarkers reflects these changes in microbial ecology, providing meaningful biosignatures for the microbes in this system. Polysaturated short-chain fatty acids characteristic of cyanobacteria account for <3% of total abundance in Laguna Bacalar microbialites. By contrast, even short-chain and monounsaturated short-chain fatty acids attributable to both Cyanobacteria and many other organisms including types of Alphaproteobacteria and Gammaproteobacteria constitute 43%-69% and 17%-25%, respectively, of total abundance in microbialites. While cyanobacteria are the largest and most visible microbes within these microbialites and dominate the mangrove root agglomeration, it is clear that their smaller, metabolically diverse associates are responsible for significant biogeochemical cycling in this microbialite system.
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Affiliation(s)
- D B Johnson
- Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL, USA
| | - P A Beddows
- Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL, USA
| | - T M Flynn
- Biosciences Division, Argonne National Laboratory, Argonne, IL, USA
| | - M R Osburn
- Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL, USA
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11
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Valdespino-Castillo PM, Hu P, Merino-Ibarra M, López-Gómez LM, Cerqueda-García D, González-De Zayas R, Pi-Puig T, Lestayo JA, Holman HY, Falcón LI. Exploring Biogeochemistry and Microbial Diversity of Extant Microbialites in Mexico and Cuba. Front Microbiol 2018; 9:510. [PMID: 29666607 PMCID: PMC5891642 DOI: 10.3389/fmicb.2018.00510] [Citation(s) in RCA: 13] [Impact Index Per Article: 2.2] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/30/2017] [Accepted: 03/06/2018] [Indexed: 01/23/2023] Open
Abstract
Microbialites are modern analogs of ancient microbial consortia that date as far back as the Archaean Eon. Microbialites have contributed to the geochemical history of our planet through their diverse metabolic capacities that mediate mineral precipitation. These mineral-forming microbial assemblages accumulate major ions, trace elements and biomass from their ambient aquatic environments; their role in the resulting chemical structure of these lithifications needs clarification. We studied the biogeochemistry and microbial structure of microbialites collected from diverse locations in Mexico and in a previously undescribed microbialite in Cuba. We examined their structure, chemistry and mineralogy at different scales using an array of nested methods including 16S rRNA gene high-throughput sequencing, elemental analysis, X-Ray fluorescence (XRF), X-Ray diffraction (XRD), Scanning Electron Microscopy-Energy Dispersive Spectroscopy (SEM-EDS), Fourier Transformed Infrared (FTIR) spectroscopy and Synchrotron Radiation-based Fourier Transformed Infrared (SR-FTIR) spectromicroscopy. The resulting data revealed high biological and chemical diversity among microbialites and specific microbe to chemical correlations. Regardless of the sampling site, Proteobacteria had the most significant correlations with biogeochemical parameters such as organic carbon (Corg), nitrogen and Corg:Ca ratio. Biogeochemically relevant bacterial groups (dominant phototrophs and heterotrophs) showed significant correlations with major ion composition, mineral type and transition element content, such as cadmium, cobalt, chromium, copper and nickel. Microbial-chemical relationships were discussed in reference to microbialite formation, microbial metabolic capacities and the role of transition elements as enzyme cofactors. This paper provides an analytical baseline to drive our understanding of the links between microbial diversity with the chemistry of their lithified precipitations.
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Affiliation(s)
- Patricia M Valdespino-Castillo
- Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, Berkeley, CA, United States
| | - Ping Hu
- Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, Berkeley, CA, United States
| | - Martín Merino-Ibarra
- Unidad Académica de Ecología y Biodiversidad Acuática, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Mexico City, Mexico
| | - Luz M López-Gómez
- Unidad Académica de Ecología y Biodiversidad Acuática, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Mexico City, Mexico
| | - Daniel Cerqueda-García
- Laboratorio de Ecología Bacteriana, Instituto de Ecología, Universidad Nacional Autónoma de México, Mexico City, Mexico
| | | | - Teresa Pi-Puig
- Instituto de Geología, Universidad Nacional Autónoma de México, Mexico City, Mexico.,Laboratorio Nacional de Geoquímica y Mineralogía, Universidad Nacional Autónoma de México, Mexico City, Mexico
| | - Julio A Lestayo
- Centro de Investigaciones de Ecosistemas Costeros, Cayo Coco, Cuba
| | - Hoi-Ying Holman
- Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, Berkeley, CA, United States.,Molecular Biophysics and Integrated Bioimaging Division, Lawrence Berkeley National Laboratory, University of California, Berkeley, Berkeley, CA, United States
| | - Luisa I Falcón
- Laboratorio de Ecología Bacteriana, Instituto de Ecología, Universidad Nacional Autónoma de México, Mexico City, Mexico
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12
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Louyakis AS, Gourlé H, Casaburi G, Bonjawo RME, Duscher AA, Foster JS. A year in the life of a thrombolite: comparative metatranscriptomics reveals dynamic metabolic changes over diel and seasonal cycles. Environ Microbiol 2017; 20:842-861. [DOI: 10.1111/1462-2920.14029] [Citation(s) in RCA: 15] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/09/2017] [Revised: 12/12/2017] [Accepted: 12/12/2017] [Indexed: 12/01/2022]
Affiliation(s)
- Artemis S. Louyakis
- Department of Microbiology and Cell Science; University of Florida, Space Life Sciences Lab; Merritt Island FL USA
| | - Hadrien Gourlé
- Department of Microbiology and Cell Science; University of Florida, Space Life Sciences Lab; Merritt Island FL USA
- Department of Animal Breeding and Genetics; Global Bioinformatics Centre, Swedish University of Agricultural Sciences; Uppsala Sweden
| | - Giorgio Casaburi
- Department of Microbiology and Cell Science; University of Florida, Space Life Sciences Lab; Merritt Island FL USA
| | - Rachelle M. E. Bonjawo
- Department of Microbiology and Cell Science; University of Florida, Space Life Sciences Lab; Merritt Island FL USA
| | - Alexandrea A. Duscher
- Department of Microbiology and Cell Science; University of Florida, Space Life Sciences Lab; Merritt Island FL USA
| | - Jamie S. Foster
- Department of Microbiology and Cell Science; University of Florida, Space Life Sciences Lab; Merritt Island FL USA
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13
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Farias ME, Rasuk MC, Gallagher KL, Contreras M, Kurth D, Fernandez AB, Poiré D, Novoa F, Visscher PT. Prokaryotic diversity and biogeochemical characteristics of benthic microbial ecosystems at La Brava, a hypersaline lake at Salar de Atacama, Chile. PLoS One 2017; 12:e0186867. [PMID: 29140980 PMCID: PMC5687714 DOI: 10.1371/journal.pone.0186867] [Citation(s) in RCA: 36] [Impact Index Per Article: 5.1] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/28/2017] [Accepted: 10/09/2017] [Indexed: 11/19/2022] Open
Abstract
Benthic microbial ecosystems of Laguna La Brava, Salar de Atacama, a high altitude hypersaline lake, were characterized in terms of bacterial and archaeal diversity, biogeochemistry, (including O2 and sulfide depth profiles and mineralogy), and physicochemical characteristics. La Brava is one of several lakes in the Salar de Atacama where microbial communities are growing in extreme conditions, including high salinity, high solar insolation, and high levels of metals such as lithium, arsenic, magnesium, and calcium. Evaporation creates hypersaline conditions in these lakes and mineral precipitation is a characteristic geomicrobiological feature of these benthic ecosystems. In this study, the La Brava non-lithifying microbial mats, microbialites, and rhizome-associated concretions were compared to each other and their diversity was related to their environmental conditions. All the ecosystems revealed an unusual community where Euryarchaeota, Crenarchaeota, Acetothermia, Firmicutes and Planctomycetes were the most abundant groups, and cyanobacteria, typically an important primary producer in microbial mats, were relatively insignificant or absent. This suggests that other microorganisms, and possibly novel pathways unique to this system, are responsible for carbon fixation. Depth profiles of O2 and sulfide showed active production and respiration. The mineralogy composition was calcium carbonate (as aragonite) and increased from mats to microbialites and rhizome-associated concretions. Halite was also present. Further analyses were performed on representative microbial mats and microbialites by layer. Different taxonomic compositions were observed in the upper layers, with Archaea dominating the non-lithifying mat, and Planctomycetes the microbialite. The bottom layers were similar, with Euryarchaeota, Crenarchaeota and Planctomycetes as dominant phyla. Sequences related to Cyanobacteria were very scarce. These systems may contain previously uncharacterized community metabolisms, some of which may be contributing to net mineral precipitation. Further work on these sites might reveal novel organisms and metabolisms of biotechnological interest.
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Affiliation(s)
- Maria Eugenia Farias
- Laboratorio de Investigaciones Microbiológicas de Lagunas Andinas (LIMLA), Planta Piloto de Procesos Industriales Microbiológicos (PROIMI), CCT-Tucumán, CONICET, Tucumán, Argentina
- * E-mail:
| | - Maria Cecilia Rasuk
- Laboratorio de Investigaciones Microbiológicas de Lagunas Andinas (LIMLA), Planta Piloto de Procesos Industriales Microbiológicos (PROIMI), CCT-Tucumán, CONICET, Tucumán, Argentina
| | - Kimberley L. Gallagher
- Department of Marine Sciences, University of Connecticut, Groton, Connecticut, United States of America
| | | | - Daniel Kurth
- Laboratorio de Investigaciones Microbiológicas de Lagunas Andinas (LIMLA), Planta Piloto de Procesos Industriales Microbiológicos (PROIMI), CCT-Tucumán, CONICET, Tucumán, Argentina
| | - Ana Beatriz Fernandez
- Laboratorio de Investigaciones Microbiológicas de Lagunas Andinas (LIMLA), Planta Piloto de Procesos Industriales Microbiológicos (PROIMI), CCT-Tucumán, CONICET, Tucumán, Argentina
| | - Daniel Poiré
- Centro de Investigaciones Geológicas, Universidad Nacional de La Plata-Conicet, La Plata, Argentina
| | - Fernando Novoa
- Centro de Ecología Aplicada (CEA), Ñuñoa, Santiago, Chile
| | - Pieter T. Visscher
- Department of Marine Sciences, University of Connecticut, Groton, Connecticut, United States of America
- Australian Centre for Astrobiology, University of New South Wales, Sydney, New South Wales, Australia
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14
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Louyakis AS, Mobberley JM, Vitek BE, Visscher PT, Hagan PD, Reid RP, Kozdon R, Orland IJ, Valley JW, Planavsky NJ, Casaburi G, Foster JS. A Study of the Microbial Spatial Heterogeneity of Bahamian Thrombolites Using Molecular, Biochemical, and Stable Isotope Analyses. ASTROBIOLOGY 2017; 17:413-430. [PMID: 28520472 PMCID: PMC5767104 DOI: 10.1089/ast.2016.1563] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/07/2023]
Abstract
Thrombolites are buildups of carbonate that exhibit a clotted internal structure formed through the interactions of microbial mats and their environment. Despite recent advances, we are only beginning to understand the microbial and molecular processes associated with their formation. In this study, a spatial profile of the microbial and metabolic diversity of thrombolite-forming mats of Highborne Cay, The Bahamas, was generated by using 16S rRNA gene sequencing and predictive metagenomic analyses. These molecular-based approaches were complemented with microelectrode profiling and in situ stable isotope analysis to examine the dominant taxa and metabolic activities within the thrombolite-forming communities. Analyses revealed three distinctive zones within the thrombolite-forming mats that exhibited stratified populations of bacteria and archaea. Predictive metagenomics also revealed vertical profiles of metabolic capabilities, such as photosynthesis and carboxylic and fatty acid synthesis within the mats that had not been previously observed. The carbonate precipitates within the thrombolite-forming mats exhibited isotopic geochemical signatures suggesting that the precipitation within the Bahamian thrombolites is photosynthetically induced. Together, this study provides the first look at the spatial organization of the microbial populations within Bahamian thrombolites and enables the distribution of microbes to be correlated with their activities within modern thrombolite systems. Key Words: Thrombolites-Microbial diversity-Metagenome-Stable isotopes-Microbialites. Astrobiology 17, 413-430.
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Affiliation(s)
- Artemis S. Louyakis
- Department of Microbiology and Cell Science, University of Florida, Space Life Sciences Lab, Merritt Island, Florida
| | - Jennifer M. Mobberley
- Department of Microbiology and Cell Science, University of Florida, Space Life Sciences Lab, Merritt Island, Florida
| | - Brooke E. Vitek
- Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida
| | - Pieter T. Visscher
- Department of Marine Sciences, University of Connecticut, Groton, Connecticut
| | - Paul D. Hagan
- Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida
| | - R. Pamela Reid
- Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida
| | - Reinhard Kozdon
- Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York
- Department of Geoscience, University of Wisconsin, Madison, Wisconsin
| | - Ian J. Orland
- Department of Geoscience, University of Wisconsin, Madison, Wisconsin
| | - John W. Valley
- Department of Geoscience, University of Wisconsin, Madison, Wisconsin
| | - Noah J. Planavsky
- Department of Geology and Geophysics, Yale University, New Haven, Connecticut
| | - Giorgio Casaburi
- Department of Microbiology and Cell Science, University of Florida, Space Life Sciences Lab, Merritt Island, Florida
| | - Jamie S. Foster
- Department of Microbiology and Cell Science, University of Florida, Space Life Sciences Lab, Merritt Island, Florida
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15
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Hays LE, Graham HV, Des Marais DJ, Hausrath EM, Horgan B, McCollom TM, Parenteau MN, Potter-McIntyre SL, Williams AJ, Lynch KL. Biosignature Preservation and Detection in Mars Analog Environments. ASTROBIOLOGY 2017; 17:363-400. [PMID: 28177270 PMCID: PMC5478115 DOI: 10.1089/ast.2016.1627] [Citation(s) in RCA: 73] [Impact Index Per Article: 10.4] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
This review of material relevant to the Conference on Biosignature Preservation and Detection in Mars Analog Environments summarizes the meeting materials and discussions and is further expanded upon by detailed references to the published literature. From this diverse source material, there is a detailed discussion on the habitability and biosignature preservation potential of five primary analog environments: hydrothermal spring systems, subaqueous environments, subaerial environments, subsurface environments, and iron-rich systems. Within the context of exploring past habitable environments on Mars, challenges common to all of these key environments are laid out, followed by a focused discussion for each environment regarding challenges to orbital and ground-based observations and sample selection. This leads into a short section on how these challenges could influence our strategies and priorities for the astrobiological exploration of Mars. Finally, a listing of urgent needs and future research highlights key elements such as development of instrumentation as well as continued exploration into how Mars may have evolved differently from Earth and what that might mean for biosignature preservation and detection. Key Words: Biosignature preservation-Biosignature detection-Mars analog environments-Conference report-Astrobiological exploration. Astrobiology 17, 363-400.
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Affiliation(s)
- Lindsay E. Hays
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California
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16
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Saghaï A, Zivanovic Y, Moreira D, Benzerara K, Bertolino P, Ragon M, Tavera R, López-Archilla AI, López-García P. Comparative metagenomics unveils functions and genome features of microbialite-associated communities along a depth gradient. Environ Microbiol 2016; 18:4990-5004. [PMID: 27422734 PMCID: PMC5477898 DOI: 10.1111/1462-2920.13456] [Citation(s) in RCA: 16] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/02/2016] [Accepted: 07/13/2016] [Indexed: 12/15/2022]
Abstract
Modern microbialites are often used as analogs of Precambrian stromatolites; therefore, studying the metabolic interplay within their associated microbial communities can help formulating hypotheses on their formation and long-term preservation within the fossil record. We performed a comparative metagenomic analysis of microbialite samples collected at two sites and along a depth gradient in Lake Alchichica (Mexico). The community structure inferred from single-copy gene family identification and long-contig (>10 kb) assignation, consistently with previous rRNA gene surveys, showed a wide prokaryotic diversity dominated by Alphaproteobacteria, Gammaproteobacteria, Cyanobacteria, and Bacteroidetes, while eukaryotes were largely dominated by green algae or diatoms. Functional analyses based on RefSeq, COG and SEED assignations revealed the importance of housekeeping functions, with an overrepresentation of genes involved in carbohydrate metabolism, as compared with other metabolic capacities. The search for genes diagnostic of specific metabolic functions revealed the important involvement of Alphaproteobacteria in anoxygenic photosynthesis and sulfide oxidation, and Cyanobacteria in oxygenic photosynthesis and nitrogen fixation. Surprisingly, sulfate reduction appeared negligible. Comparative analyses suggested functional similarities among various microbial mat and microbialite metagenomes as compared with soil or oceans, but showed differences in microbial processes among microbialite types linked to local environmental conditions.
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Affiliation(s)
- Aurélien Saghaï
- Ecologie Systématique Evolution, CNRS, Université Paris-Sud, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Yvan Zivanovic
- Institut de Biologie Intégrative de la Cellule, CNRS, Université Paris-Sud Orsay, Université Paris-Saclay, France
| | - David Moreira
- Ecologie Systématique Evolution, CNRS, Université Paris-Sud, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Karim Benzerara
- Institut de Minéralogie et de Physique des Matériaux et de Cosmochimie, CNRS, Muséum National d'Histoire Naturelle, Université Pierre et Marie Curie, Sorbonne Universités, Paris, France
| | - Paola Bertolino
- Ecologie Systématique Evolution, CNRS, Université Paris-Sud, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Marie Ragon
- Ecologie Systématique Evolution, CNRS, Université Paris-Sud, Université Paris-Saclay, AgroParisTech, Orsay, France
| | - Rosaluz Tavera
- Departamento de Ecología y Recursos Naturales, Universidad Nacional Autónoma de México, DF Mexico, Mexico
| | | | - Purificación López-García
- Ecologie Systématique Evolution, CNRS, Université Paris-Sud, Université Paris-Saclay, AgroParisTech, Orsay, France
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17
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White RA, Chan AM, Gavelis GS, Leander BS, Brady AL, Slater GF, Lim DSS, Suttle CA. Metagenomic Analysis Suggests Modern Freshwater Microbialites Harbor a Distinct Core Microbial Community. Front Microbiol 2016; 6:1531. [PMID: 26903951 PMCID: PMC4729913 DOI: 10.3389/fmicb.2015.01531] [Citation(s) in RCA: 41] [Impact Index Per Article: 5.1] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/12/2015] [Accepted: 12/21/2015] [Indexed: 11/13/2022] Open
Abstract
Modern microbialites are complex microbial communities that interface with abiotic factors to form carbonate-rich organosedimentary structures whose ancestors provide the earliest evidence of life. Past studies primarily on marine microbialites have inventoried diverse taxa and metabolic pathways, but it is unclear which of these are members of the microbialite community and which are introduced from adjacent environments. Here we control for these factors by sampling the surrounding water and nearby sediment, in addition to the microbialites and use a metagenomics approach to interrogate the microbial community. Our findings suggest that the Pavilion Lake microbialite community profile, metabolic potential and pathway distributions are distinct from those in the neighboring sediments and water. Based on RefSeq classification, members of the Proteobacteria (e.g., alpha and delta classes) were the dominant taxa in the microbialites, and possessed novel functional guilds associated with the metabolism of heavy metals, antibiotic resistance, primary alcohol biosynthesis and urea metabolism; the latter may help drive biomineralization. Urea metabolism within Pavilion Lake microbialites is a feature not previously associated in other microbialites. The microbialite communities were also significantly enriched for cyanobacteria and acidobacteria, which likely play an important role in biomineralization. Additional findings suggest that Pavilion Lake microbialites are under viral selection as genes associated with viral infection (e.g CRISPR-Cas, phage shock and phage excision) are abundant within the microbialite metagenomes. The morphology of Pavilion Lake microbialites changes dramatically with depth; yet, metagenomic data did not vary significantly by morphology or depth, indicating that microbialite morphology is altered by other factors, perhaps transcriptional differences or abiotic conditions. This work provides a comprehensive metagenomic perspective of the interactions and differences between microbialites and their surrounding environment, and reveals the distinct nature of these complex communities.
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Affiliation(s)
- Richard Allen White
- Department of Microbiology and Immunology, University of British Columbia, Vancouver BC, Canada
| | - Amy M Chan
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver BC, Canada
| | - Gregory S Gavelis
- Department of Zoology, University of British Columbia, Vancouver BC, Canada
| | - Brian S Leander
- Department of Zoology, University of British Columbia, VancouverBC, Canada; Department of Botany, University of British Columbia, VancouverBC, Canada
| | - Allyson L Brady
- School of Geography and Earth Sciences, McMaster University, Hamilton ON, Canada
| | - Gregory F Slater
- School of Geography and Earth Sciences, McMaster University, Hamilton ON, Canada
| | - Darlene S S Lim
- Bay Area Environmental Institute, PetalumaCA, USA; NASA Ames Research Center, Moffett FieldCA, USA
| | - Curtis A Suttle
- Department of Microbiology and Immunology, University of British Columbia, VancouverBC, Canada; Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, VancouverBC, Canada; Department of Botany, University of British Columbia, VancouverBC, Canada; Canadian Institute for Advanced Research, TorontoON, Canada
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18
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Tomescu AMF, Klymiuk AA, Matsunaga KKS, Bippus AC, Shelton GWK. Microbes and the Fossil Record: Selected Topics in Paleomicrobiology. THEIR WORLD: A DIVERSITY OF MICROBIAL ENVIRONMENTS 2016. [DOI: 10.1007/978-3-319-28071-4_3] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/12/2022]
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19
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Casaburi G, Duscher AA, Reid RP, Foster JS. Characterization of the stromatolite microbiome from Little Darby Island, The Bahamas using predictive and whole shotgun metagenomic analysis. Environ Microbiol 2015; 18:1452-69. [PMID: 26471001 DOI: 10.1111/1462-2920.13094] [Citation(s) in RCA: 27] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/16/2015] [Revised: 10/13/2015] [Accepted: 10/13/2015] [Indexed: 02/01/2023]
Abstract
Modern stromatolites represent ideal ecosystems to understand the biological processes required for the precipitation of carbonate due to their long evolutionary history and occurrence in a wide range of habitats. However, most of the prior molecular work on stromatolites has focused on understanding the taxonomic complexity and not fully elucidating the functional capabilities of these systems. Here, we begin to characterize the microbiome associated with stromatolites of Little Darby Island, The Bahamas using predictive metagenomics of the 16S rRNA gene coupled with direct whole shotgun sequencing. The metagenomic analysis of the Little Darby stromatolites revealed many shared taxa and core pathways associated with biologically induced carbonate precipitation, suggesting functional convergence within Bahamian stromatolites. A comparison of the Little Darby stromatolites with other lithifying microbial ecosystems also revealed that although factors, such as geographic location and salinity, do drive some differences within the population, there are extensive similarities within the microbial populations. These results suggest that for stromatolite formation, 'who' is in the community is not as critical as metabolic activities and environmental interactions. Together, these analyses help improve our understanding of the similarities among lithifying ecosystems and provide an important first step in characterizing the shared microbiome of modern stromatolites.
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Affiliation(s)
- Giorgio Casaburi
- Department of Microbiology and Cell Science, University of Florida, Space Life Science Lab, Merritt Island, FL, USA
| | - Alexandrea A Duscher
- Department of Microbiology and Cell Science, University of Florida, Space Life Science Lab, Merritt Island, FL, USA
| | - R Pamela Reid
- Rosenstiel School of Marine Sciences, University of Miami, Miami, FL, USA
| | - Jamie S Foster
- Department of Microbiology and Cell Science, University of Florida, Space Life Science Lab, Merritt Island, FL, USA
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20
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White RA, Power IM, Dipple GM, Southam G, Suttle CA. Metagenomic analysis reveals that modern microbialites and polar microbial mats have similar taxonomic and functional potential. Front Microbiol 2015; 6:966. [PMID: 26441900 PMCID: PMC4585152 DOI: 10.3389/fmicb.2015.00966] [Citation(s) in RCA: 36] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/12/2015] [Accepted: 08/31/2015] [Indexed: 12/15/2022] Open
Abstract
Within the subarctic climate of Clinton Creek, Yukon, Canada, lies an abandoned and flooded open-pit asbestos mine that harbors rapidly growing microbialites. To understand their formation we completed a metagenomic community profile of the microbialites and their surrounding sediments. Assembled metagenomic data revealed that bacteria within the phylum Proteobacteria numerically dominated this system, although the relative abundances of taxa within the phylum varied among environments. Bacteria belonging to Alphaproteobacteria and Gammaproteobacteria were dominant in the microbialites and sediments, respectively. The microbialites were also home to many other groups associated with microbialite formation including filamentous cyanobacteria and dissimilatory sulfate-reducing Deltaproteobacteria, consistent with the idea of a shared global microbialite microbiome. Other members were present that are typically not associated with microbialites including Gemmatimonadetes and iron-oxidizing Betaproteobacteria, which participate in carbon metabolism and iron cycling. Compared to the sediments, the microbialite microbiome has significantly more genes associated with photosynthetic processes (e.g., photosystem II reaction centers, carotenoid, and chlorophyll biosynthesis) and carbon fixation (e.g., CO dehydrogenase). The Clinton Creek microbialite communities had strikingly similar functional potentials to non-lithifying microbial mats from the Canadian High Arctic and Antarctica, but are functionally distinct, from non-lithifying mats or biofilms from Yellowstone. Clinton Creek microbialites also share metabolic genes (R2 < 0.750) with freshwater microbial mats from Cuatro Ciénegas, Mexico, but are more similar to polar Arctic mats (R2 > 0.900). These metagenomic profiles from an anthropogenic microbialite-forming ecosystem provide context to microbialite formation on a human-relevant timescale.
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Affiliation(s)
- Richard Allen White
- Department of Microbiology and Immunology, University of British Columbia Vancouver, BC, Canada
| | - Ian M Power
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia Vancouver, BC, Canada
| | - Gregory M Dipple
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia Vancouver, BC, Canada
| | - Gordon Southam
- School of Earth Sciences, University of Queensland Brisbane, QLD, Australia
| | - Curtis A Suttle
- Department of Microbiology and Immunology, University of British Columbia Vancouver, BC, Canada ; Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia Vancouver, BC, Canada ; Department of Botany, University of British Columbia Vancouver, BC, Canada ; Canadian Institute for Advanced Research Toronto, ON, Canada
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21
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Theisen CH, Sumner DY, Mackey TJ, Lim DSS, Brady AL, Slater GF. Carbonate fabrics in the modern microbialites of Pavilion Lake: two suites of microfabrics that reflect variation in microbial community morphology, growth habit, and lithification. GEOBIOLOGY 2015; 13:357-372. [PMID: 25809931 DOI: 10.1111/gbi.12134] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/11/2014] [Accepted: 02/23/2015] [Indexed: 06/04/2023]
Abstract
Modern microbialites in Pavilion Lake, BC, provide an analog for ancient non-stromatolitic microbialites that formed from in situ mineralization. Because Pavilion microbialites are mineralizing under the influence of microbial communities, they provide insights into how biological processes influence microbialite microfabrics and mesostructures. Hemispherical nodules and micrite-microbial crusts are two mesostructures within Pavilion microbialites that are directly associated with photosynthetic communities. Both filamentous cyanobacteria in hemispherical nodules and branching filamentous green algae in micrite-microbial crusts were associated with calcite precipitation at microbialite surfaces and with characteristic microfabrics in the lithified microbialite. Hemispherical nodules formed at microbialite surfaces when calcite precipitated around filamentous cyanobacteria with a radial growth habit. The radial filament pattern was preserved within the microbialite to varying degrees. Some subsurface nodules contained well-defined filaments, whereas others contained only dispersed organic inclusions. Variation in filament preservation is interpreted to reflect differences in timing and amount of carbonate precipitation relative to heterotrophic decay, with more defined filaments reflecting greater lithification prior to degradation than more diffuse filaments. Micrite-microbial crusts produce the second suite of microfabrics and form in association with filamentous green algae oriented perpendicular to the microbialite surface. Some crusts include calcified filaments, whereas others contained voids that reflect the filamentous community in shape, size, and distribution. Pavilion microbialites demonstrate that microfabric variation can reflect differences in lithification processes and microbial metabolisms as well as microbial community morphology and organization. Even when the morphology of individual filaments or cells is not well preserved, the microbial growth habit can be captured in mesoscale microbialite structures. These results suggest that when petrographic preservation is extremely good, ancient microbialite growth structures and microfabrics can be interpreted in the context of variation in community organization, community composition, and lithification history. Even in the absence of distinct microbial microfabrics, mesostructures can capture microbial community morphology.
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Affiliation(s)
- C Harwood Theisen
- Department of Earth and Planetary Sciences, University of California, Davis, CA, USA
| | - D Y Sumner
- Department of Earth and Planetary Sciences, University of California, Davis, CA, USA
| | - T J Mackey
- Department of Earth and Planetary Sciences, University of California, Davis, CA, USA
| | - D S S Lim
- Bay Area Environmental Research Institute, Petaluma, CA, USA
- NASA Ames Research Center, Moffett Field, CA, USA
| | - A L Brady
- School of Geography and Earth Sciences, McMaster University, Hamilton, ON, Canada
| | - G F Slater
- School of Geography and Earth Sciences, McMaster University, Hamilton, ON, Canada
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22
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Petryshyn VA, Lim D, Laval BL, Brady A, Slater G, Tripati AK. Reconstruction of limnology and microbialite formation conditions from carbonate clumped isotope thermometry. GEOBIOLOGY 2015; 13:53-67. [PMID: 25515686 DOI: 10.1111/gbi.12121] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/18/2014] [Accepted: 09/17/2014] [Indexed: 06/04/2023]
Abstract
Quantitative tools for deciphering the environment of microbialite formation are relatively limited. For example, the oxygen isotope carbonate-water geothermometer requires assumptions about the isotopic composition of the water of formation. We explored the utility of using 'clumped' isotope thermometry as a tool to study the temperatures of microbialite formation. We studied microbialites recovered from water depths of 10-55 m in Pavilion Lake, and 10-25 m in Kelly Lake, spanning the thermocline in both lakes. We determined the temperature of carbonate growth and the (18)O/(16)O ratio of the waters that microbialites grew in. Results were then compared to current limnological data from the lakes to reconstruct the history of microbialite formation. Modern microbialites collected at shallow depths (11.7 m) in both lakes yield clumped isotope-based temperatures of formation that are within error of summer water temperatures, suggesting that clumped isotope analyses may be used to reconstruct past climates and to probe the environments in which microbialites formed. The deepest microbialites (21.7-55 m) were recovered from below the present-day thermoclines in both lakes and yield radioisotope ages indicating they primarily formed earlier in the Holocene. During this time, pollen data and our reconstructed water (18)O/(16)O ratios indicate a period of aridity, with lower lake levels. At present, there is a close association between both photosynthetic and heterotrophic communities, and carbonate precipitation/microbialite formation, with biosignatures of photosynthetic influences on carbonate detected in microbialites from the photic zone and above the thermocline (i.e., depths of generally <20 m). Given the deeper microbialites are receiving <1% of photosynthetically active radiation (PAR), it is likely these microbialites primarily formed when lower lake levels resulted in microbialites being located higher in the photic zone, in warm surface waters.
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Affiliation(s)
- V A Petryshyn
- Department of Earth, Planetary and Space Sciences, University of California, Los Angeles, CA, USA
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