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 <i>Sulfophobococcus</i>. Functional predictions indicated a predominance of sulfur- and nitrogen-related metabolisms, with no clear depth-structured metabolic profiles across the SMTZ. Overall, our results highlight how local geochemical gradients shape both methane-cycling and non-methane-cycling prokaryotic assemblages in a poorly explored South Atlantic cold seep, providing a baseline for future genome-resolved investigations of microbial functioning in this system.

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Publication Details

Journal
Ecology and Evolution
Published
2026-02-01
DOI
https://doi.org/10.1002/ece3.72973
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
0.00

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article

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

Eric W. Triplett, Eduardo Eizirik, Adolpho Herbert Augustin, Luiz Frederico Rodrigues et al.
Ecology and Evolution
Methane Hydrates and Related Phenomena
article

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

Eric W. Triplett, Eduardo Eizirik, Adolpho Herbert Augustin, Luiz Frederico Rodrigues, Adriano R. Viana, Dennis Miller, J.M. Ketzer, Renata Medina‐Silva, Karine A. Felix Ribeiro, Taiz L. Lopes Simão, Raquel Dias, Adriana Giongo
article en

Abstract

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 <i>Sulfophobococcus</i>. Functional predictions indicated a predominance of sulfur- and nitrogen-related metabolisms, with no clear depth-structured metabolic profiles across the SMTZ. Overall, our results highlight how local geochemical gradients shape both methane-cycling and non-methane-cycling prokaryotic assemblages in a poorly explored South Atlantic cold seep, providing a baseline for future genome-resolved investigations of microbial functioning in this system.

Ecology and EvolutionVol. 16(2)
Petrobras (Brazil) (BR), University of Florida (US), Pontifícia Universidade Católica do Rio Grande do Sul (BR)
Conselho Nacional de Desenvolvimento Científico e Tecnológico, Petrobras
Life below water
Openalex Percentile: Top 57%
Methane Hydrates and Related Phenomena
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