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Lacustrine Nostoc (Nostocales) and associated microbiome generate a new type of modern clotted microbialite
Authors:Linda E. Graham  Jennifer J. Knack  Michael J. Piotrowski  Lee W. Wilcox  Martha E. Cook  Charles H. Wellman  Wilson Taylor  Louise A. Lewis  Patricia Arancibia‐Avila
Affiliation:1. Department of Botany, University of Wisconsin‐Madison, , Madison, Wisconsin, 53606 USA;2. School of Biological Sciences, Illinois State University, , Normal, Illinois, 61790 USA;3. Department of Animal and Plant Sciences, University of Sheffield, , Sheffield, S10 2TN UK;4. Department of Biology, University of Wisconsin‐Eau Claire, , Eau Claire, Wisconsin, 54702 USA;5. Department of Ecology and Evolutionary Biology, University of Connecticut, , Storrs, Connecticut, 06269 USA;6. Department of Basic Sciences, University of Bio‐Bio, , Chillan, Chile
Abstract:Microbialites are mineral formations formed by microbial communities that are often dominated by cyanobacteria. Carbonate microbialites, known from Proterozoic times through the present, are recognized for sequestering globally significant amounts of inorganic carbon. Recent ecological work has focused on microbial communities dominated by cyanobacteria that produce microbial mats and laminate microbialites (stromatolites). However, the taxonomic composition and functions of microbial communities that generate distinctive clotted microbialites (thrombolites) are less well understood. Here, microscopy and deep shotgun sequencing were used to characterize the microbiome (microbial taxa and their genomes) associated with a single cyanobacterial host linked by 16S sequences to Nostoc commune Vaucher ex Bornet & Flahault, which dominates abundant littoral clotted microbialites in shallow, subpolar, freshwater Laguna Larga in southern Chile. Microscopy and energy‐dispersive X‐ray spectroscopy suggested the hypothesis that adherent hollow carbonate spheres typical of the clotted microbialite begin development on the rigid curved outer surfaces of the Nostoc balls. A surface biofilm included >50 nonoxygenic bacterial genera (taxa other than Nostoc) that indicate diverse ecological functions. The Laguna Larga Nostoc microbiome included the sulfate reducers Desulfomicrobium and Sulfospirillum and genes encoding all known proteins specific to sulfate reduction, a process known to facilitate carbonate deposition by increasing pH. Sequences indicating presence of nostocalean and other types of nifH, nostocalean sulfide:ferredoxin oxidoreductase (indicating anoxygenic photosynthesis), and biosynthetic pathways for the secondary products scytonemin, mycosporine, and microviridin toxin were identified. These results allow comparisons with microbiota and microbiomes of other algae and illuminate biogeochemical roles of ancient microbialites.
Keywords:microbialite  microbiome  Nostoc  sulfate reduction  X‐ray spectroscopy
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