Abstract

Hadal trench bottom (>6000 m below sea level) sediments harbor higher microbial cell abundance compared with adjacent abyssal plain sediments. This is supported by the accumulation of sedimentary organic matter (OM), facilitated by trench topography. However, the distribution of benthic microbes in different trench systems has not been well explored yet. Here, we carried out small subunit ribosomal RNA gene tag sequencing for 92 sediment subsamples of seven abyssal and seven hadal sediment cores collected from three trench regions in the northwest Pacific Ocean: the Japan, Izu-Ogasawara, and Mariana Trenches. Tag-sequencing analyses showed specific distribution patterns of several phyla associated with oxygen and nitrate. The community structure was distinct between abyssal and hadal sediments, following geographic locations and factors represented by sediment depth. Co-occurrence network revealed six potential prokaryotic consortia that covaried across regions. Our results further support that the OM cycle is driven by hadal currents and/or rapid burial shapes microbial community structures at trench bottom sites, in addition to vertical deposition from the surface ocean. Our trans-trench analysis highlights intra- and inter-trench distributions of microbial assemblages and geochemistry in surface seafloor sediments, providing novel insights into ultradeep-sea microbial ecology, one of the last frontiers on our planet.

Highlights

  • Supplementary information The online version of this article contains supplementary material, which is available to authorized users.The abyssal plain extends from the continental slope to the rim of deep trenches (3000–6000 m below sea level [mbsl])(JAMSTEC), 2–15 Natsushima-cho, Yokosuka 237–0061 Kanagawa, Japan10 Present addressFaculty of Science and Engineering, Toyo University, 2100 Kujirai, Kawagoe 350-8585 Saitama, JapanMicrobial community and geochemical analyses of trans-trench sediments for understanding the roles of. . .and covers 85% of the global seafloor area, while the hadal zone (>6000 mbsl) comprises 1–2% of it [1, 2]

  • Cell abundance and microbial carbon turnover rates are significantly higher at hadal trench bottom compared with abyssal plain sediment below the surface layer, while those in outermost surface layer are sometimes comparable between hadal and abyssal sites [4]

  • Sediment cores were collected over five cruises by Japan Agency for Marine-Earth Science and Technology (JAMSTEC); Research Vessel (R/V) Kairei KR11-11 (December 2011) and KR15-01 (March 2015) cruises and R/V Yokosuka YK11-06 (September 2011) cruise for the IzuOgasawara Trench, R/V Kairei KR12-19 (December 2012) cruise for the Japan Trench, and R/V Kairei KR14-01 cruise (January 2014) for the Mariana Trench (Fig. 1 and Table S1)

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Summary

1234567890();,: 1234567890();,: Introduction

The abyssal plain extends from the continental slope to the rim of deep trenches (3000–6000 m below sea level [mbsl])

10 Present address
Materials and methods
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