Structure and Spatial Heterogeneity of Chemosynthesis-Based Deep-Sea Archaeal and Bacterial Communities in Western South Atlantic.

Cold seeps are widespread deep-sea ecosystems sustained by methane-rich fluid seepage and host dense chemosynthesis-based biological communities. In 2016, a methane-driven chemosynthetic system was discovered on the Rio Grande Cone, in the Western South Atlantic Ocean, but the structure and drivers of its prokaryotic communities remained poorly understood. Here, we investigated archaeal and bacterial communities associated with deep-sea sediments across three geographic areas (A, C, and E) and a vertical gradient of up to 18 m below the seafloor, encompassing sediment layers within and below the sulfate-methane transition zone (SMTZ). Community composition was assessed using high-throughput sequencing of the 16S rRNA gene (V3-V4 region), processed into amplicon sequence variants (ASVs), and related to local geochemical gradients using multivariate analyses. To disentangle the ecological responses of methane-cycling taxa from the broader microbiome, the prokaryotic community was analyzed by contrasting the ANME-SRB consortium with the remaining archaeal and bacterial taxa. Both groups exhibited significant spatial structuring across areas and sediment layers. Methane concentration and depth were the dominant drivers shaping both ANME-SRB and the remaining prokaryotic community, with conductivity further influencing the latter. Core microbiome analysis revealed a small number of widespread taxa accounting for a large proportion of total community abundance, including an atypical dominance of the archaeal genus