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      Metagenomic Analysis Suggests Modern Freshwater Microbialites Harbor a Distinct Core Microbial Community

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          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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          Ray Meta: scalable de novo metagenome assembly and profiling

          Voluminous parallel sequencing datasets, especially metagenomic experiments, require distributed computing for de novo assembly and taxonomic profiling. Ray Meta is a massively distributed metagenome assembler that is coupled with Ray Communities, which profiles microbiomes based on uniquely-colored k-mers. It can accurately assemble and profile a three billion read metagenomic experiment representing 1,000 bacterial genomes of uneven proportions in 15 hours with 1,024 processor cores, using only 1.5 GB per core. The software will facilitate the processing of large and complex datasets, and will help in generating biological insights for specific environments. Ray Meta is open source and available at http://denovoassembler.sf.net.
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            Stromatolites in Precambrian carbonates: evolutionary mileposts or environmental dipsticks?

            Stromatolites are attached, lithified sedimentary growth structures, accretionary away from a point or limited surface of initiation. Though the accretion process is commonly regarded to result from the sediment trapping or precipitation-inducing activities of microbial mats, little evidence of this process is preserved in most Precambrian stromatolites. The successful study and interpretation of stromatolites requires a process-based approach, oriented toward deconvolving the replacement textures of ancient stromatolites. The effects of diagenetic recrystallization first must be accounted for, followed by analysis of lamination textures and deduction of possible accretion mechanisms. Accretion hypotheses can be tested using numerical simulations based on modem stromatolite growth processes. Application of this approach has shown that stromatolites were originally formed largely through in situ precipitation of laminae during Archean and older Proterozoic times, but that younger Proterozoic stromatolites grew largely through the accretion of carbonate sediments, most likely through the physical process of microbial trapping and binding. This trend most likely reflects long-term evolution of the earth's environment rather than microbial communities.
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              Microbialites: Organosedimentary Deposits of Benthic Microbial Communities

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                Author and article information

                Contributors
                Journal
                Front Microbiol
                Front Microbiol
                Front. Microbiol.
                Frontiers in Microbiology
                Frontiers Media S.A.
                1664-302X
                28 January 2016
                2015
                : 6
                : 1531
                Affiliations
                [1] 1Department of Microbiology and Immunology, University of British Columbia, Vancouver BC, Canada
                [2] 2Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver BC, Canada
                [3] 3Department of Zoology, University of British Columbia, Vancouver BC, Canada
                [4] 4Department of Botany, University of British Columbia, Vancouver BC, Canada
                [5] 5School of Geography and Earth Sciences, McMaster University, Hamilton ON, Canada
                [6] 6Bay Area Environmental Institute, Petaluma CA, USA
                [7] 7NASA Ames Research Center, Moffett Field CA, USA
                [8] 8Canadian Institute for Advanced Research, Toronto ON, Canada
                Author notes

                Edited by: John J. Kelly, Loyola University Chicago, USA

                Reviewed by: Zhenfeng Liu, University of Southern California, USA; Anas Ghadouani, The University of Western Australia, Australia

                *Correspondence: Curtis A. Suttle, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020-2207 Main Mall, Vancouver, BC V6T 1Z4, Canada, suttle@ 123456science.ubc.ca

                Present address: Richard Allen White III, Fundamental and Computational Sciences, Pacific Northwest National Laboratories, Richland, WA, USA

                This article was submitted to Aquatic Microbiology, a section of the journal Frontiers in Microbiology

                Article
                10.3389/fmicb.2015.01531
                4729913
                26903951
                93cc55bf-8a54-4e75-b9e9-d9d117cc98ae
                Copyright © 2016 White, Chan, Gavelis, Leander, Brady, Slater, Lim and Suttle.

                This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

                History
                : 12 January 2015
                : 21 December 2015
                Page count
                Figures: 5, Tables: 3, Equations: 0, References: 80, Pages: 14, Words: 0
                Funding
                Funded by: Canadian Space Agency 10.13039/501100000016
                Award ID: MARSLIFE Project (9F052-10-0176)
                Funded by: National Aeronautics and Space Administration 10.13039/100000104
                Funded by: Natural Sciences and Engineering Research Council of Canada 10.13039/501100000038
                Categories
                Microbiology
                Original Research

                Microbiology & Virology
                microbialites,pavilion lake,metagenomics,thrombolites,metabolic potential
                Microbiology & Virology
                microbialites, pavilion lake, metagenomics, thrombolites, metabolic potential

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