The Active Sulfate-Reducing Microbial Community in Littoral Sediment of Oligotrophic Lake Constance
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fmicb-10-00247 February 11, 2019 Time: 18:14 # 1 Erschienen in: Frontiers in Microbiology ; 10 (2019). - 247 http://dx.doi.org/10.3389/fmicb.2019.00247 ORIGINAL RESEARCH published: 13 February 2019 doi: 10.3389/fmicb.2019.00247 The Active Sulfate-Reducing Microbial Community in Littoral Sediment of Oligotrophic Lake Constance Susanne Wörner1,2 and Michael Pester1,2,3* 1 Department of Biology, University of Konstanz, Konstanz, Germany, 2 Leibniz Institute DSMZ – German Collection of Microorganisms and Cell cultures, Braunschweig, Germany, 3 Institute for Microbiology, Technical University of Braunschweig, Braunschweig, Germany Active sulfate-reducing microorganisms (SRM) in freshwater sediments are under- examined, despite the well-documented cryptic sulfur cycle occurring in these low- Edited by: sulfate habitats. In Lake Constance sediment, sulfate reduction rates of up to 1,800 nmol Kenneth Wasmund, cm−3 day−1 were previously measured. To characterize its SRM community, we used University of Vienna, Austria a tripartite amplicon sequencing approach based on 16S rRNA genes, 16S rRNA, Reviewed by: Paula Dalcin Martins, and dsrB transcripts (encoding the beta subunit of dissimilatory sulfite reductase). Radboud University Nijmegen, We followed the respective amplicon dynamics in four anoxic microcosm setups Netherlands supplemented either with (i) chitin and sulfate, (ii) sulfate only, (iii) chitin only, or Christina Pavloudi, Hellenic Centre for Marine Research (iv) no amendment. Chitin was used as a general substrate for the whole carbon (HCMR), Greece degradation chain. Sulfate turnover in sulfate-supplemented microcosms ranged from Jesse G. Dillon, −1 −1 California State University, Long 38 to 955 nmol day (g sediment f. wt.) and was paralleled by a decrease of Beach, United States 90–100% in methanogenesis as compared to the respective methanogenic controls. *Correspondence: In the initial sediment, relative abundances of recognized SRM lineages accounted for Michael Pester 3.1 and 4.4% of all bacterial 16S rRNA gene and 16S rRNA sequences, respectively. [email protected] When normalized against the 1.4 × 108 total prokaryotic 16S rRNA gene copies as Specialty section: determined by qPCR and taking multiple rrn operons per genome into account, this This article was submitted to 5 6 −1 Aquatic Microbiology, resulted in approximately 10 –10 SRM cells (g sediment f. wt.) . The three amplicon a section of the journal approaches jointly identified Desulfobacteraceae and Syntrophobacteraceae as the Frontiers in Microbiology numerically dominant and transcriptionally most active SRM in the initial sediment. Received: 09 November 2018 This was corroborated in the time course analyses of sulfate-consuming sediment Accepted: 30 January 2019 Published: 13 February 2019 microcosms irrespective of chitin amendment. Uncultured dsrAB family-level lineages Citation: constituted in sum only 1.9% of all dsrB transcripts, with uncultured lineage 5 and 6 Wörner S and Pester M (2019) being transcriptionally most active. Our study is the first holistic molecular approach to The Active Sulfate-Reducing Microbial Community in Littoral Sediment quantify and characterize active SRM including uncultured dsrAB lineages not only in of Oligotrophic Lake Constance. Lake Constance but for lake sediments in general. Front. Microbiol. 10:247. doi: 10.3389/fmicb.2019.00247 Keywords: lake sediment, next-generation amplicon sequencing, chitin, sulfate reduction, dsrB transcripts Frontiers in Microbiology| www.frontiersin.org 1 February 2019| Volume 10| Article 247 Konstanzer Online-Publikations-System (KOPS) URL: http://nbn-resolving.de/urn:nbn:de:bsz:352-2-dtsrg0xr6hqj6 fmicb-10-00247 February 11, 2019 Time: 18:14 # 2 Wörner and Pester Active Sulfate Reducers in Lake Sediments INTRODUCTION so far not associated with this metabolic trait (Anantharaman et al., 2018; Hausmann et al., 2018; Zecchin et al., 2018). These Lake Constance is a typical pre-alpine lake that has currently included among others the Acidobacteria, Planctomycetes, an oligotrophic status and is oxygenated down to the sediment Verrucomicrobia, and Armatimonadetes. In specific, 8 of these (Güde and Straile, 2016). Within the first millimeters of its 13 newly identified SRM groups are candidate phyla without sediment, oxygen is completely depleted (Gerhardt et al., 2005) isolated representatives (Anantharaman et al., 2018). In parallel, leaving room for anaerobic degradation of organic matter either microbial diversity assays based on the functional marker genes by fermenters that share their degradation products (acetate dsrAB, which encode the dissimilatory sulfite reductase and and H2) with methanogenic archaea (Rothfuss and Conrad, 1993; are commonly used as diagnostic markers in detecting SRM, Thebrath et al., 1993) or by nitrate- (Hauck et al., 2001), Fe (III)- indicate an even larger phylogenetic diversity with at least 13 (Gerhardt et al., 2005), humic acid- (Kappler et al., 2004), and uncultured family-level dsrAB lineages (Pester et al., 2012; Müller sulfate-reducing microorganisms (Bak and Pfennig, 1991a,b). et al., 2015). So far, the latter only partially overlap with the A major component of organic matter entering the sediment metagenome-discovered putative SRM, e.g., uncultured dsrAB is chitin as an abundant biopolymer in aquatic environments lineage 8 is represented by Acidobacteria (Hausmann et al., (Gooday, 1990; Cauchie, 2002). It consists of linked amino-sugar 2018) and uncultured dsrAB lineage 13 is closely related to subunits with ß-1,4-N-acetyl-D-glucosamine as the monomeric mesophilic Nitrospirae (Zecchin et al., 2018). Extending upon structure and serves as structural element in the exoskeleton of the phylogenetic framework for dsrAB genes that was proposed arthropods (e.g., zooplankton) and the cell wall of fungi and by Müller et al.(2015), a recent dsrB amplicon survey of 200 certain algae and protozoa (Gooday, 1990). The estimated annual environmental samples including various freshwater habitats production of 28 × 106 tons by crustaceans and insects in increased the number of known species-level operational freshwater ecosystems and its efficient turnover in freshwater taxonomic units (OTUs) related to potential SRM from ca. 800 sediments (50–75%, Beier and Bertilsson, 2013) indicate chitin as (Müller et al., 2015) to more than 150,000 (Vigneron et al., 2018). an important carbon and nitrogen source for microorganisms in Considering the ca. 240 cultivated sulfate-reducing microbial these habitats (Gooday, 1990; Cauchie, 2002). species (Rabus et al., 2013), this result uncovered that less than In Lake Constance, sulfate concentrations of 50–300 mM can 0.2% of all potential SRM are available in pure culture. The same be measured in the upper layers of the littoral sediments. Here, study revealed that among uncultured SRM those belonging to maximum sulfate reduction rates (SRR) as determined using uncultured dsrAB lineage 5 are quite prevalent in freshwater 35 2− −3 S-SO4 as a radiotracer reached values of 1,800 nmol cm habitats (Vigneron et al., 2018). day−1 at 1–2 cm sediment depth (Bak and Pfennig, 1991a). This Despite the importance of sulfate reduction for the sediment surpasses typical SRR in sulfate-rich marine surface sediments biogeochemistry of Lake Constance as a typical freshwater lake, by one order of magnitude, where sulfate reduction is one of its SRM community is so far very poorly characterized. The the major anaerobic carbon degradation pathways (Jørgensen, only attempt was based on enrichment cultures grown on H2, 1982; Bowles et al., 2014). The high SRR at concomitant low lactate, acetate, propionate or long chain fatty acids, with isolates sulfate concentrations in Lake Constance are explained by a fast being affiliated to the genera Desulfovibrio, Desulfobulbus, and and effective cycling of sulfur species between their oxidized and Desulfotomaculum (Bak and Pfennig, 1991b). Therefore, we reduced states, which is controlled by a cryptic sulfur cycle as attempted to systematically analyze and quantify the littoral is typical for freshwater sediments and wetlands (Pester et al., SRM community of Lake Constance using a tripartite, high 2012). In particular, sulfide as the end product of sulfate reduction throughput amplicon sequencing approach based on 16S rRNA does not accumulate beyond 80 mM in littoral sediments of Lake genes, 16S rRNA, and dsrB transcripts. To delineate active Constance (Gerhardt, 2004), but is likely rapidly re-oxidized back SRM, sediment was incubated in the presence of chitin as to sulfate at oxic-anoxic interfaces or under completely anoxic a general substrate for the complete anaerobic degradation conditions using nitrate, Fe (III), or humic acids as electron network in the presence and absence of externally supplied acceptor (Pester et al., 2012). SRR in Lake Constance sediments pulses of sulfate. This was compared to sediment incubated are saturated at 60 mM sulfate, reaching maximum values of with sulfate pulses only or without any external additions. Our 3,000 nmol cm−3 day−1 in sediment slurries (Bak and Pfennig, results show that SRM constitute about 3% of the total bacterial 1991a). This shows that SRR are not limited by the prevailing sediment community with their major representatives being sulfate concentrations in Lake Constance (Bak and Pfennig, affiliated to the deltaproteobacterial families Desulfobacteraceae 1991a; Güde and Straile, 2016), which is also true for many other and Syntrophobacteraceae. freshwater lakes