The deep biosphere contains a large portion of the total microbial communities on Earth, but little is known about the carbon sources that support deep life. In this study, we used Stable Isotope Probing (SIP) and high throughput amplicon sequencing to identify the acetate assimilating microbial communities at 2260 m depth in the bedrock of Outokumpu, Finland. The long-term and short-term effects of acetate on the microbial communities were assessed by DNA-targeted SIP and RNA targeted cell activation. The microbial communities reacted within hours to the amended acetate. Archaeal taxa representing the rare biosphere at 2260 m depth were identified and linked to the cycling of acetate, and were shown to have an impact on the functions and activity of the microbial communities in general through small key carbon compounds. The major archaeal lineages identified to assimilate acetate and metabolites derived from the labelled acetate were Methanosarcina spp., Methanococcus spp., Methanolobus spp., and unclassified Methanosarcinaceae. These archaea have previously been detected in the Outokumpu deep subsurface as minor groups. Nevertheless, their involvement in the assimilation of acetate and secretion of metabolites derived from acetate indicated an important role in the supporting of the whole community in the deep subsurface, where carbon sources are limited.Geosciences 2018, 8, 418 2 of 20 utilizing soluble gases, such as crustal methane or hydrogen from radiolytic decomposition of water, have been made since [5][6][7][8]. More specifically, the metabolic capabilities of deep terrestrial subsurface microbial communities include the pathways covering, e.g., methanogenesis [9][10][11], anaerobic methane oxidation [12], acetogenesis [4,13], sulfate reduction [14-16], oxidation of sulfur by denitrification [17], and reduction of iron [14].The Outokumpu deep scientific drill hole, located in Eastern Finland, hosts a unique environment piercing through crystalline Precambrian bedrock and its numerous saline fluid filled fracture zones. The composition of the microbial communities and the geochemical characteristics of the Outokumpu deep subsurface have been studied in detail [11,[18][19][20][21][22][23][24][25][26][27]. The metabolic strategies of the microbial communities at different depths in Outokumpu have been estimated through functional gene analysis and metagenomes [11,21]. Purkamo et al. [21,22] suggested that microbial communities commonly employ heterotrophic carbon assimilation in the Outokumpu deep subsurface, and that the communities have the capacity of both sulphate and nitrate reduction. At greater depths, genetic potential for autotrophic acetogenesis and hydrogenotrophic methanogenesis has been detected from Outokumpu metagenomes together with H 2 oxidation and CO 2 fixation coupling hydrogenases [11].The terrestrial deep subsurface represents an oligotrophic, nutrient-poor, and isolated habitat. The fact that heterotrophy appears to be common in the Outokumpu deep biosphere means that the carbon sub...