High-resolution vertical biogeochemical profiles in the hyporheic zone reveal insights into microbial methane cycling

<p>Facing the challenges of climate change, policy making relies on sound greenhouse gas (GHG) budgets. Rivers and streams emit large quantities of the potent GHG methane (CH<span class="inline-formula"><sub>4</sub></span>), but their global impact on atmosphe...

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Bibliographic Details
Main Authors: T. Michaelis, A. Wunderlich, Ö. K. Coskun, W. Orsi, T. Baumann, F. Einsiedl
Format: Article
Language:English
Published: Copernicus Publications 2022-09-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/19/4551/2022/bg-19-4551-2022.pdf
Description
Summary:<p>Facing the challenges of climate change, policy making relies on sound greenhouse gas (GHG) budgets. Rivers and streams emit large quantities of the potent GHG methane (CH<span class="inline-formula"><sub>4</sub></span>), but their global impact on atmospheric CH<span class="inline-formula"><sub>4</sub></span> concentrations is highly uncertain. In situ data from the hyporheic zone (HZ), where most CH<span class="inline-formula"><sub>4</sub></span> is produced and some of it can be oxidized to CO<span class="inline-formula"><sub>2</sub></span>, are lacking for an accurate description of CH<span class="inline-formula"><sub>4</sub></span> production and consumption in streams. To address this, we recorded high-resolution depth-resolved geochemical profiles at five different locations in the stream bed of the river Moosach, southern Germany. Specifically, we measured pore-water concentrations and stable carbon isotopes (<span class="inline-formula"><i>δ</i><sup>13</sup></span>C) of dissolved CH<span class="inline-formula"><sub>4</sub></span> as well as relevant electron acceptors for oxidation with a 1 cm vertical depth resolution. Findings were interpreted with the help of a numerical model, and 16S rRNA gene analyses added information on the microbial community at one of the locations. Our data confirm with pore-water CH<span class="inline-formula"><sub>4</sub></span> concentrations of up to 1000 <span class="inline-formula">µ</span>mol L<span class="inline-formula"><sup>−1</sup></span> that large quantities of CH<span class="inline-formula"><sub>4</sub></span> are produced in the HZ. Stable isotope measurements of CH<span class="inline-formula"><sub>4</sub></span> suggest that hydrogenotrophic methanogenesis represents a dominant pathway for CH<span class="inline-formula"><sub>4</sub></span> production in the HZ of the river Moosach, while a relatively high abundance of a novel group of methanogenic archaea, the <i>Candidatus</i> “Methanomethyliales” (phylum <i>Candidatus</i> “Verstraetearchaeota”), indicate that CH<span class="inline-formula"><sub>4</sub></span> production through H<span class="inline-formula"><sub>2</sub></span>-dependent methylotrophic methanogenesis might also be an important CH<span class="inline-formula"><sub>4</sub></span> source. Combined isotopic and modeling results clearly implied CH<span class="inline-formula"><sub>4</sub></span> oxidation processes at one of the sampled locations, but due to the steep chemical gradients and the close proximity of the oxygen and nitrate reduction zones, no single electron acceptor for this process could be identified. Nevertheless, the numerical modeling results showed potential not only for aerobic CH<span class="inline-formula"><sub>4</sub></span> oxidation but also for anaerobic oxidation of CH<span class="inline-formula"><sub>4</sub></span> coupled to denitrification. In addition, the nitrate–methane transition zone was characterized by an increased relative abundance of microbial groups (<i>Crenothrix</i>, NC10) known to mediate nitrate and nitrite-dependent methane oxidation in the hyporheic zone.</p> <p>This study demonstrates substantial CH<span class="inline-formula"><sub>4</sub></span> production in hyporheic sediments, a potential for aerobic and anaerobic CH<span class="inline-formula"><sub>4</sub></span> oxidation, and underlines the high spatiotemporal variability in this habitat.</p>
ISSN:1726-4170
1726-4189