Microbial communities have been thriving in hydrothermal vents for

Range >3.3 billion years
Organism Biosphere
Reference Schönheit P, Buckel W, Martin WF. On the Origin of Heterotrophy. Trends Microbiol. 2016 Jan24(1):12-25. doi: 10.1016/j.tim.2015.10.003. p.13 top paragraphPubMed ID26578093
Primary Source [29] Westall, F. et al. (2015) Archean (3.33 Ga) microbe-sediment systems were diverse and flourished in a hydrothermal context. Geology 43, 615–618 doi: 10.1130/G36646.1 link
Comments p.13 top paragraph:"The core pathway of carbon and energy metabolism in anaerobic autotrophs that inhabit such hydrothermal and deep crust environments [refs 22–24] is the acetyl-coenzyme A (CoA) pathway, the most ancient of the six pathways of CO2 fixation known and the only one present in archaea and bacteria [refs 2,25]. Spontaneous exergonic organic syntheses from H2 and CO2 occur today at hydrothermal vents, for example formate synthesis [refs 18,26] and methane synthesis [refs 19,20,27], that are similar, if not homologous [ref 28], to core energy-releasing reactions of carbon and energy metabolism in methanogens and acetogens, which live by the reduction of CO2 by H2. Microbial communities have been thriving in hydrothermal vents for over 3.3 billion years [primary source]."
Entered by Uri M
ID 112445