Abstract

Hadal trenches, oceanic locations deeper than 6,000 m, are thought to have distinct microbial communities compared to those at shallower depths due to high hydrostatic pressures, topographical funneling of organic matter, and biogeographical isolation. Here we evaluate the hypothesis that hadal trenches contain unique microbial biodiversity through analyses of the communities present in the bottom waters of the Kermadec and Mariana trenches. Estimates of microbial protein production indicate active populations under in situ hydrostatic pressures and increasing adaptation to pressure with depth. Depth, trench of collection, and size fraction are important drivers of microbial community structure. Many putative hadal bathytypes, such as members related to the Marinimicrobia, Rhodobacteraceae, Rhodospirilliceae, and Aquibacter, are similar to members identified in other trenches. Most of the differences between the two trench microbiomes consists of taxa belonging to the Gammaproteobacteria whose distributions extend throughout the water column. Growth and survival estimates of representative isolates of these taxa under deep-sea conditions suggest that some members may descend from shallower depths and exist as a potentially inactive fraction of the hadal zone. We conclude that the distinct pelagic communities residing in these two trenches, and perhaps by extension other trenches, reflect both cosmopolitan hadal bathytypes and ubiquitous genera found throughout the water column.

Highlights

  • The deep sea is one of the largest biomes on Earth, containing over half of the microbial cells in the ocean [1,2]

  • Hadal microbial communities are adapted to high hydrostatic pressure conditions Seawater samples were collected at 38 locations within the Kermadec and Mariana trenches at depths up to 10,004 m and 10,920 m, respectively

  • To assess the activity of microbes collected from the Mariana Trench, the fraction of cells engaged in protein synthesis was evaluated using biorthogonal noncanonical amino acid tagging (BONCAT)

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Summary

Introduction

The deep sea is one of the largest biomes on Earth, containing over half of the microbial cells in the ocean [1,2]. Pelagic deep-ocean microbial communities are distinct from those above them [3,4,5,6] and in many cases display higher activities under in situ hydrostatic pressures and low temperatures when compared to atmospheric pressure conditions [7]. Deep-sea environments contain allochthonous members that descend from above, such as in association with sinking particulate organic matter [8]. These communities can differ from one another, varying by water mass or ocean basin and showing metabolic rates ranging over. Mariana and Kermadec trench hadal communities had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript

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