Seafloor basalts are widely distributed and host diverse prokaryotic communities, but no data exist concerning the metabolic rates of the resident microbial communities. We present here potential extracellular enzyme activities of leucine aminopeptidase (LAP) and alkaline phosphatase (AP) measured on basalt samples from different locations on Loihi Seamount, HI, coupled with analysis of prokaryotic biomass and pyrosequencing of the bacterial 16S rRNA gene. The community maximum potential enzyme activity (V max ) of LAP ranged from 0.47 to 0.90 nmol (g rock) Ű1 h Ű1 ; the V max for AP was 28 to 60 nmol (g rock) Ű1 h Ű1 . The K m of LAP ranged from 26 to 33 M, while the K m for AP was 2 to 7 M. Bacterial communities on Loihi basalts were comprised primarily of Alpha-, Delta-, andGammaproteobacteria, Bacteroidetes, and Planctomycetes. The putative ability to produce LAP is evenly distributed across the most commonly detected bacterial orders, but the ability to produce AP is likely dominated by bacteria in the orders Xanthomonadales, Flavobacteriales, and Planctomycetales. The enzyme activities on Loihi basalts were compared to those of other marine environments that have been studied and were found to be similar in magnitude to those from continental shelf sediments and orders of magnitude higher than any measured in the water column, demonstrating that the potential for exposed basalts to transform organic matter is substantial. We propose that microbial communities on basaltic rock play a significant, quantifiable role in benthic biogeochemical processes.
Exposed seafloor basalts comprise a 600,000-km 2 continuous undersea habitat (1). Endolithic basalt microbes are diverse and abundant (2), and several clades of bacteria appear more likely to be encountered on basalts than elsewhere (3). Bacterial phyla display trends in abundance that reflect rock geochemistry, indicating a strong selection of microbial communities by rock composition (4). Genes diagnostic for methanogenesis, nitrogen fixation, anaerobic ammonium oxidation, denitrification, Fe reduction, and dissimilatory sulfate reduction are present in basalt microbial communities (3), indicating the potential for diverse biogeochemical transformations on basalts. However, no data are currently available for metabolic activity rates of basaltic microbes.The relationship between the presence of prokaryotes and the activity and function of enzymes in extreme environments in general and basalts in particular is underexplored. Hydrolytic extracellular enzymes have been shown to be indicators of metabolically active bacteria, and existing data sets from various marine environments can be used for comparison with information from newly explored areas (5, 6). Additionally, in deep sea environments, organic matter is more refractory in nature, and therefore, extracellular enzyme hydrolases should play an important role in the initiation of organic matter recycling. Indeed, recent work showed that the most abundant group of Archaea in marine sediments produces unique...