The chemolithotrophic Zetaproteobacteria represent a novel class of Proteobacteria which oxidize Fe(II) to Fe(III) and are the dominant bacterial population in iron-rich microbial mats. Zetaproteobacteria were first discovered at Lo 'ihi Seamount, located 35 km southeast off the big island of Hawai'i, which is characterized by low-temperature diffuse hydrothermal venting. Novel nondegenerate quantitative PCR (qPCR) assays for genes associated with microbial nitrogen fixation, denitrification, arsenic detoxification, Calvin-Benson-Bassham (CBB), and reductive tricarboxylic acid (rTCA) cycles were developed using selected microbial mat community-derived metagenomes. Nitrogen fixation genes were not detected, but all other functional genes were present. This suggests that arsenic detoxification and denitrification processes are likely cooccurring in addition to two modes of carbon fixation. Two groups of microbial mat community types were identified by terminal restriction fragment length polymorphism (T-RFLP) and were further described based on qPCR data for zetaproteobacterial abundance and carbon fixation mode preference. qPCR variance was associated with mat morphology but not with temperature or sample site. Geochemistry data were significantly associated with sample site and mat morphology. Together, these qPCR assays constitute a functional gene signature for iron microbial mat communities across a broad array of temperatures, mat types, chemistries, and sampling sites at Lo 'ihi Seamount.
Deep-sea hydrothermal vents are dynamic and extremely productive biological ecosystems supported by chemosynthetic microbial primary production. In the absence of photosynthesis, microorganisms derive energy via the oxidation of reduced chemicals [e.g., H 2 , H 2 S, Fe(II), and CH 4 ] emitted in hydrothermal fluids (1). In contrast to other strategies for microbial chemosynthesis at hydrothermal vents, iron oxidation has only more recently been studied (2). By weight, iron is the most abundant element in the earth, and it has vast potential as an energy source for microbes via chemolithoautotrophy coupled to Fe(II) oxidation (3). However, iron's ability to act as an electron donor for the biotic fixation of CO 2 in neutrophilic environments is limited by the rapid abiotic oxidation of Fe(II) to Fe(III) in the presence of oxygen (4, 5). Despite the ephemeral nature of iron as an energy source, iron-oxidizing bacteria (FeOB) have been identified in a wide array of freshwater and marine habitats and can flourish at circumneutral deep-sea vents with sharp redox gradients and hydrothermal fluids high in CO 2 and reduced iron (6-9). The recently described Zetaproteobacteria represent a novel class of marine Proteobacteria that are diverse and abundant contributors to deep-sea FeOB communities (10).Zetaproteobacteria were first discovered at iron-rich, low-temperature hydrothermal vents at Lo 'ihi Seamount, HI (2, 11), and have been demonstrated to be significant microbial colonizers of seamounts (10, 12). Lo 'ihi Seamount is a s...