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Methane diffusion affects characteristics of benthic communities in and around microbial mat-covered sediments in the northeastern Japan sea.

Authors :
Ota, Yuki
Iguchi, Akira
Nishijima, Miyuki
Mukai, Ryo
Suzumura, Masahiro
Yoshioka, Hideyoshi
Suzuki, Atsushi
Tsukasaki, Ayumi
Aoyagi, Tomo
Hori, Tomoyuki
Source :
Chemosphere. Feb2024, Vol. 349, pN.PAG-N.PAG. 1p.
Publication Year :
2024

Abstract

We investigated relationships between features of benthic macrofaunal communities and geochemical parameters in and around microbial mat-covered sediments associated with a methane seepage on Sakata Knoll in the eastern Japan Sea. A depression on top of the knoll corresponds to a gas-hydrate-bearing area with seepage of methane-rich fluid, and microbial mats cover the seafloor sediments. Sediment cores were collected at three sites for this study: one within a microbial mat, a second a few meters outside of the microbial mat, and a third from a reference site outside the gas-hydrate-bearing areas. Morphological analysis showed that the site inside the microbial mat had higher macrofaunal density and biomass compared with the other sites. 18S rRNA gene analysis showed that annelids were dominant in the surface sediment inside the microbial mat with the possible occurrence of microbial anaerobic oxidation of methane (AOM), whereas in the surface sediments outside the microbial mat and at the reference site the predominant species belonged to phylum Cercozoa. Morphological analysis also showed that the surface sediment inside the microbial mat noticeably favored annelids, with dorvilleid Ophryotrocha sp. and ampharetid Neosabellides sp. identified as major constituents. Statistical analysis showed that sulfidic sediment conditions with concentrations of H 2 S up to 121 μM resulting from AOM likely resulted in the predominance of annelids with tolerance to sulfide. Both the 18S rRNA genes and macrofaunal characteristics showed that benthic biodiversity among the three sites was greatest outside the microbial mat. The site outside the microbial mat may represent geochemical transition conditions, including a lower rate of upward methane gas-flow compared with the site inside the microbial mat. The high biodiversity there might result from the presence of species specifically suited to the transition zone as well as species also found in photosynthesis-based communities of the background environment. [Display omitted] • Microbial mats overlie methane seepage sediments on Sakata Knoll in the Japan Sea. • Methane diffusion affects redox conditions and organic matter supply in the sediments. • Benthic communities dominated by annelids are related to sulfidic sediments. • The environment outside the microbial mats has higher biodiversity than inside. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00456535
Volume :
349
Database :
Academic Search Index
Journal :
Chemosphere
Publication Type :
Academic Journal
Accession number :
174605768
Full Text :
https://doi.org/10.1016/j.chemosphere.2023.140964