Institute of Earth, Ocean and Atmospheric Sciences, Rutgers University, New Brunswick, United States; Institute of Marine Science, National Research Council of Italy, Ancona, Italy; Program in Interdisciplinary Studies, Institute for Advanced Studies, Princeton, United States; Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo, Japan
Stefan M Sievert
Biology Department, Woods Hole Oceanographic Institution, Woods Hole, United States
Institute of Earth, Ocean and Atmospheric Sciences, Rutgers University, New Brunswick, United States; Department of Biochemistry and Microbiology, Rutgers University, New Brunswick, United States
Anaerobic thermophiles inhabit relic environments that resemble the early Earth. However, the lineage of these modern organisms co-evolved with our planet. Hence, these organisms carry both ancestral and acquired genes and serve as models to reconstruct early metabolism. Based on comparative genomic and proteomic analyses, we identified two distinct groups of genes in Thermovibrio ammonificans: the first codes for enzymes that do not require oxygen and use substrates of geothermal origin; the second appears to be a more recent acquisition, and may reflect adaptations to cope with the rise of oxygen on Earth. We propose that the ancestor of the Aquificae was originally a hydrogen oxidizing, sulfur reducing bacterium that used a hybrid pathway for CO2 fixation. With the gradual rise of oxygen in the atmosphere, more efficient terminal electron acceptors became available and this lineage acquired genes that increased its metabolic flexibility while retaining ancestral metabolic traits.