32Hadal trench bottom (>6,000 m below sea level) sediments harbor higher microbial cell abundance 33 compared to adjacent abyssal plain sediments. This is supported by the accumulation of sedimentary organic 34 matter (OM), facilitated by trench topography. However, the distribution of benthic microbes in different 35 trench systems has not been explored yet. Here, we carried out small subunit ribosomal RNA gene tag 36 sequencing for 92 sediment subsamples of seven abyssal and seven hadal sediment cores collected from three 37 trench regions in the northwest Pacific Ocean: the Japan, and Mariana Trenches. 38 Tag-sequencing analyses showed specific distribution patterns of several phyla associated with oxygen and 39 nitrate. The community structure was distinct between abyssal and hadal sediments, following geographic 40 locations and factors represented by sediment depth. Co-occurrence network revealed six potential prokaryotic 41 consortiums that covaried across regions. Our results further support that the endogenous OM cycle is driven 42 by hadal currents and/or rapid burial shapes microbial community structures at trench bottom sites, in addition 43 to vertical deposition from the surface ocean. Our trans-trench analysis highlights intra-and inter-trench 44 distributions of microbial assemblages and geochemistry in surface seafloor sediments, providing novel 45 insights into ultra-deep-sea microbial ecology, one of the last frontiers on our planet. 46
48The abyssal plain extends from the continental slope to the rim of deep trenches (3,000-6,000 m 49 below sea level [mbsl]) and covers 85% of the global seafloor area, while the hadal zone (>6,000 mbsl) 50 comprises 1-2% of it [1, 2]. In general, abyssal water and sediments are usually oligotrophic, and physical and 51 chemical conditions (e.g., salinity, temperature, dissolved oxygen, and nutrient concentrations) in hadal water 52 are similar to the overlying abyssal water despite the higher hydrostatic pressure [1-3]. However, cell 53 abundance and microbial carbon turnover rates are significantly higher at hadal compared to abyssal seafloors, 54 especially below the sediment surface, while microbial abundance in surface sediments are sometimes 55 comparable between hadal and abyssal sites [4]. This could be attributed to factors apart from differences in 56 the vertical downward flux of sinking organic matter (OM) from the ocean surface and hydrostatic pressure. 57Hadal zones are generally located in oceanic trenches that are formed along plate boundaries by 58 movement of oceanic plates, and thus experience episodic and/or regular landslides [5, 6]. These landslides 59 cause downward transportation of surface sediments along with relatively fresh OM via the funnel effect of 60 trench geomorphology [7][8][9][10][11]. Moreover, higher sedimentation rates and concentrations of subseafloor 61 organic compounds in trench bottom sediments compared to neighboring abyssal sediments have been 62 reported in multiple trench regions under oligotrophic and eutroph...