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Updated: May 19, 2026

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Acetoclastic methanogenesis associated with arsenic methylation in a reducing aquifer: Pathway-specific patterns and
Yamin Deng1, Xiaofang Yuan2, Yuxiao Xu1
1MOE Key Laboratory of Groundwater Quality and Health & School of Environmental Studies, China University of Geosciences, Wuhan 430078, China.
Abstract:
The distribution of methylated arsenic (MeAs) in reducing groundwater systems remains incompletely understood, in part due to uncertainties regarding how specific methanogenic pathways may influence arsenic biomethylation, a critical issue in arsenic biogeochemistry and risk assessment. To explore this question, we integrated hydrogeochemical characterization, carbon isotopic tracing, metagenomic analysis, and pathway-specific enrichment experiments, focusing on MeAs-rich alluvial-lacustrine aquifers in the central Yangtze River Basin. A strong positive correlation between arsM and mcrA abundances (r = 0.84, p < 0.001) points to a co-occurrence of genetic potential for arsenic methylation and methanogenesis in the studied aquifer. Metagenome-assembled genome (MAG) analysis showed a pathway-specific distribution of arsM gene, a higher proportion of acetoclastic methanogen MAGs harbored complete arsM genes (14.29 %), compared to methylotrophic (9.09 %) and hydrogenotrophic (0.00 %) methanogens. In pathway-specific enrichment assays under controlled laboratory conditions, acetoclastic cultures exhibited the highest capacity for stepwise arsenic methylation (MMA and DMA production), with methylation efficiency reaching approximately 10.2 %, whereas methylotrophic cultures produced only transient MMA and hydrogenotrophic cultures showed minimal methylation. These observations provide insights into pathway-dependent differences in methanogen-associated arsenic methylation, highlighting a possible biogeochemical link between methanogenesis and arsenic cycling in the studied aquifer. These findings contribute to understanding potential controls on MeAs occurrence in reducing groundwater and provide a basis for further investigations in comparable hydrogeological settings.
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