bioRxiv Science⌕ Search

Biology subjects

Mayr, M. J.

Publications and source records attributed to Mayr, M. J..

2 recordsLinked to original sources

Distinct Microbial Communities Within and On Seep Carbonates Support Long-term Anaerobic Oxidation of Methane and Novel pMMO Diversity

At methane seeps worldwide, syntrophic anaerobic methane-oxidizing archaea and sulfate-reducing bacteria (ANME-SRB) promote carbonate precipitation and rock formation, acting as methane and carbon sink. While maintenance of active anaerobic oxidation of methane (AOM) within seep carbonates has been documented, the ANME-SRB reactivity to methane exposure remains uncertain. Surface-associated microbes may metabolize AOM-derived sulfide, maintain carbonate anoxia, and contribute to carbonate dissolution and higher trophic levels; however, these microbial communities are poorly described thus far. Here we provide new insights into microbial diversity, metabolic potential, activity, and resiliency within and on Southern Californian methane seep carbonates, by combining 16S rRNA and metagenomic sequencing, laboratory incubations, and BONCAT-FISH. Ca. Methanophaga (ANME-1) dominated the carbonate interiors across different seepage activities, based on sequencing, while the dominant SRB was Ca. Desulfaltia, potentially a new ANME partner. BONCAT-FISH revealed differences in ANME-1 cell activity, suggesting cell dormancy or DNA preservation at less active seep sites. Carbonate incubations from low activity seeps ([≥]24 months) showed an exponential AOM reactivation (44-day doubling time), suggesting seep carbonates remain potential methane sinks over dynamic seepage conditions. The surface-associated communities were distinct from the carbonate interior and other seep habitats, and highly heterogeneous. Surface ANME-SRB biofilms and sulfide-oxidizing bacterial mats were associated with high and intermediate AOM carbonates, potentially influencing carbonate precipitation/dissolution. Carbonate surfaces shared diverse aerobic methanotrophs with invertebrates, potentially serving as pool for animal epibionts. Besides particulate methane monooxygenases from aerobic methanotrophs, we found divergent forms including within a Methylophagaceae (GCA-002733105) MAG suggesting a new function within Methylophagaceae.

ecology↗

Growth and rapid succession of methanotrophs effectively limit methane release during lake overturn

Lakes and reservoirs contribute substantially to atmospheric concentrations of the potent greenhouse gas methane. Lacustrine sediments produce large amounts of methane, which accumulate in oxygen-depleted hypolimnia of stratified lakes. Due to climate change and progressing eutrophication, the number of lakes with hypolimnetic methane storage may increase in the future. However, whether stored methane eventually reaches the atmosphere during lake overturn is a matter of controversy and depends critically on the response of the methanotroph assemblage. We show that the methanotroph assemblage in a mixing lake underwent both a substantial bloom and ecological succession. As a result, the methane oxidation capacity of the mixed layer kept pace with the methane supplied from the hypolimnion and most of the stored methane was oxidized. This previously unknown aspect of freshwater methanotroph ecology represents an effective mechanism limiting methane transfer from lakes to the atmosphere.

microbiology↗