Microbial hydrogen oxidation potential in seasonally hypoxic Baltic Sea sediments

The majority of the organic matter (OM) degradation on the seafloor occurs in coastal regions. Since oxygen (O<sub>2</sub>) becomes quickly depleted in the top sediments, most of the OM decomposition is driven by microbial sulfate reduction (SR) and fermentation, the latter generating molecular hydrogen (H<sub>2</sub>). If the H<sub>2</sub> is not consumed by hydrogenotrophic microorganisms and accumulates in the sedimentary porewaters, OM degradation is hindered. Despite the importance of H<sub>2</sub> scavenging microorganisms for OM mineralization, the knowledge on H<sub>2</sub> oxidizers and their constraints in coastal marine sediments is still quite limited. Here we investigated the role of H<sub>2</sub> oxidizers in top (2 to 5 cm, suboxic-sulfidic) and bottom (18 to 22 cm, sulfidic) coastal sediments from a location exposed to seasonal hypoxia in the SW Baltic Sea. We used sediments from April, May and August, representative of different seasons. We spiked respective sediment slurries with H<sub>2</sub> and incubated them for up to 4 weeks under O<sub>2</sub>-free conditions. H<sub>2</sub> consumption potential, methane production and shifts in bacterial and archaeal 16S rRNA gene amplicons (generated from RNA) were assessed over time. The seasonal variations in sedimentary community compositions and pore water geochemistry already gave distinct starting conditions for the H<sub>2</sub> enrichments. Sediments exposed to near anoxic bottom water conditions favored a microbial starter community exhibiting the highest H<sub>2</sub> oxidation potential. Most of the observed H<sub>2</sub> oxidation potential appeared associated with hydrogenotrophic sulfate reducers. The putative involvement of massively enriched ANME in H<sub>2</sub> cycling in May 18 to 22 cm sediment horizons is conspicuous. While the differences in the observed H<sub>2</sub> oxidation potentials in the studied sediment slurries are likely related to the (season-depending) overall redox state of the sediments and interstitial waters, the influence of microbial interconnections could not be fully resolved and evaluated, demonstrating the need for further consumption- and community-based studies.

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Journal
Frontiers in Microbiology
Published
2025-04-04
DOI
https://doi.org/10.3389/fmicb.2025.1565157
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
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article

Microbial hydrogen oxidation potential in seasonally hypoxic Baltic Sea sediments

Christian Deusner, Mark Schmidt, Mirjam Perner, Nicole Adam-Beyer
Frontiers in Microbiology
Methane Hydrates and Related Phenomena
article

Microbial hydrogen oxidation potential in seasonally hypoxic Baltic Sea sediments

Christian Deusner, Mark Schmidt, Mirjam Perner, Nicole Adam-Beyer
article en

Abstract

The majority of the organic matter (OM) degradation on the seafloor occurs in coastal regions. Since oxygen (O<sub>2</sub>) becomes quickly depleted in the top sediments, most of the OM decomposition is driven by microbial sulfate reduction (SR) and fermentation, the latter generating molecular hydrogen (H<sub>2</sub>). If the H<sub>2</sub> is not consumed by hydrogenotrophic microorganisms and accumulates in the sedimentary porewaters, OM degradation is hindered. Despite the importance of H<sub>2</sub> scavenging microorganisms for OM mineralization, the knowledge on H<sub>2</sub> oxidizers and their constraints in coastal marine sediments is still quite limited. Here we investigated the role of H<sub>2</sub> oxidizers in top (2 to 5 cm, suboxic-sulfidic) and bottom (18 to 22 cm, sulfidic) coastal sediments from a location exposed to seasonal hypoxia in the SW Baltic Sea. We used sediments from April, May and August, representative of different seasons. We spiked respective sediment slurries with H<sub>2</sub> and incubated them for up to 4 weeks under O<sub>2</sub>-free conditions. H<sub>2</sub> consumption potential, methane production and shifts in bacterial and archaeal 16S rRNA gene amplicons (generated from RNA) were assessed over time. The seasonal variations in sedimentary community compositions and pore water geochemistry already gave distinct starting conditions for the H<sub>2</sub> enrichments. Sediments exposed to near anoxic bottom water conditions favored a microbial starter community exhibiting the highest H<sub>2</sub> oxidation potential. Most of the observed H<sub>2</sub> oxidation potential appeared associated with hydrogenotrophic sulfate reducers. The putative involvement of massively enriched ANME in H<sub>2</sub> cycling in May 18 to 22 cm sediment horizons is conspicuous. While the differences in the observed H<sub>2</sub> oxidation potentials in the studied sediment slurries are likely related to the (season-depending) overall redox state of the sediments and interstitial waters, the influence of microbial interconnections could not be fully resolved and evaluated, demonstrating the need for further consumption- and community-based studies.

Frontiers in MicrobiologyVol. 16
GEOMAR Helmholtz Centre for Ocean Research Kiel (DE)
Life below water
Openalex Percentile: Top 93%
Methane Hydrates and Related Phenomena
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