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Amsterdam urban canals contain novel niches for methane-cycling microorganisms
Authors:Koen A J Pelsma  Michiel H in 't Zandt  Huub J M Op den Camp  Mike S M Jetten  Joshua F Dean  Cornelia U Welte
Institution:1. Department of Microbiology, Radboud Institute for Biological and Environmental Sciences, Heyendaalseweg 135, Nijmegen, 6525 AJ The Netherlands;2. Department of Microbiology, Radboud Institute for Biological and Environmental Sciences, Heyendaalseweg 135, Nijmegen, 6525 AJ The Netherlands

Netherlands Earth System Science Centre, Utrecht University, Heidelberglaan 2, Utrecht, 3584 CS The Netherlands;3. Department of Microbiology, Radboud Institute for Biological and Environmental Sciences, Heyendaalseweg 135, Nijmegen, 6525 AJ The Netherlands

Netherlands Earth System Science Centre, Utrecht University, Heidelberglaan 2, Utrecht, 3584 CS The Netherlands

Soehngen Institute of Anaerobic Microbiology, Radboud University, Heyendaalseweg 135, Nijmegen, 6525 AJ The Netherlands;4. School of Environmental Sciences, University of Liverpool, Liverpool, L69 3GP UK

Abstract:Urbanised environments have been identified as hotspots of anthropogenic methane emissions. Especially urban aquatic ecosystems are increasingly recognised as important sources of methane. However, the microbiology behind these emissions remains unexplored. Here, we applied microcosm incubations and molecular analyses to investigate the methane-cycling community of the Amsterdam canal system in the Netherlands. The sediment methanogenic communities were dominated by Methanoregulaceae and Methanosaetaceae, with co-occurring methanotrophic Methanoperedenaceae and Methylomirabilaceae indicating the potential for anaerobic methane oxidation. Methane was readily produced after substrate amendment, suggesting an active but substrate-limited methanogenic community. Bacterial 16S rRNA gene amplicon sequencing of the sediment revealed a high relative abundance of Thermodesulfovibrionia. Canal wall biofilms showed the highest initial methanotrophic potential under oxic conditions compared to the sediment. During prolonged incubations the maximum methanotrophic rate increased to 8.08 mmol gDW?1 d?1 that was concomitant with an enrichment of Methylomonadaceae bacteria. Metagenomic analysis of the canal wall biofilm lead to the recovery of a single methanotroph metagenome-assembled genome. Taxonomic analysis showed that this methanotroph belongs to the genus Methyloglobulus. Our results underline the importance of previously unidentified and specialised environmental niches at the nexus of the natural and human-impacted carbon cycle.
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