24The Arctic Ocean currently receives a large supply of global river discharge and terrestrial 25 dissolved organic matter. Moreover, an increase in freshwater runoff and riverine transport of 26 organic matter to the Arctic Ocean is a predicted consequence of thawing permafrost and 27 increased precipitation. The fate of the terrestrial humic-rich organic material and its impact on 28 the marine carbon cycle are largely unknown. Here, the first metagenomic survey of the Canada 29Basin in the Western Arctic Ocean showed that pelagic Chloroflexi from the Arctic Ocean are 30 replete with aromatic compound degradation genes, acquired in part by lateral transfer from 31 terrestrial bacteria. Our results imply marine Chloroflexi have the capacity to use terrestrial 32 organic matter and that their role in the carbon cycle may increase with the changing 33 hydrological cycle. 34 35 released to the Atlantic, at least in part by microbial processes 10 . As input of tDOM increases, 49 knowledge on its microbial transformation will be critical for understanding changes in Arctic 50 carbon cycling. 51The marine SAR202 is a diverse and uncultivated clade of Chloroflexi bacteria that 52 comprise roughly 10% of planktonic cells in the dark ocean [11][12][13][14][15] . SAR202 is also common in 53 marine sediments and deep lakes [16][17][18] . It has long been speculated that SAR202 may play a 54 role in the degradation of recalcitrant organic matter 12,15 , and the recent analysis of SAR202 55 single-cell amplified genomes (SAGs) lends support to this notion 19 . More generally, 56Chloroflexi, including those in the SAR202 clade, are also present in the upper layers of the 57 Arctic Ocean 20 , leading to the hypothesis that recalcitrant organic compounds present in high 58Arctic tDOM could be utilized by this group. 5960
Results
61In this study, we analyzed Chloroflexi metagenome assembled genomes (MAGs) 62 generated from samples collected from the vertically stratified waters of the Canada Basin in the 63 Western Arctic Ocean (Fig. 1a). A metagenomic co-assembly was generated from samples 64 originating from the surface layer (5 m to 7 m), the subsurface chlorophyll maximum (25 m to 79 65 m) and a layer corresponding to the terrestrially-derived DOM fluorescence (FDOM) maximum 66 previously described within the cold CB halocline comprised of Pacific-origin waters (177 m to 67 213 m) 21 . The Pacific-origin FDOM maximum is due to sea ice formation and interactions with 68 bottom sediments on the Beaufort and Chukchi shelves, which themselves are influenced by 69 coastal erosion and river runoff 21 . Binning based on tetranucleotide frequency and coverage 70 resulted in 360 MAGs from a diversity of marine microbes (Fig. 1b). Six near complete 71Chloroflexi MAGs were identified. Based on 16S rRNA gene phylogeny, these MAGs 72 represented 3 distinct SAR202 subclades (SAR202-II, -VI, -VII), the AncK29 clade and the TK10 73 Chloroflexi bacterium 5419 | Bioreactor (A0A1Q3SS95) Pseudomonas alcaligenes | Experimnetally validated (Q9S3...