“…For example, genera Thermoanaerobacter or Thermoanaerobacterium were detected in deep terrestrial environments such as terrestrial deep crusts (Szewzyk et al, 1994;Liu et al, 1997;Roh et al, 2003;Zhang et al, 2006), deep oil reservoirs (e.g., L'Haridon et al, 1995;Slobodkin et al, 1999;Birkeland, 2004;Fardeau et al, 2004), and terrestrial hot springs that serve as channels between the deep, hot biosphere and the surface biosphere (Cook et al, 1996;Slobodkin et al, 1999;Bao et al, 2002;Wagner and Wiegel, 2008;Bonch-Osmolovskaya, 2010). However, despite quite a few other types of thermophilic metal-reducing bacteria detected (e.g., Slobodkin, 2005), genera Thermoanaerobacter and Thermoanaerobacterium have rarely been reported from deep-sea hydrothermal vents where diverse thermophilic microorganisms thrive (e.g., Parkes et al, 1994;Reysenbach et al, 2000;Sokolova et al, 2001;Holden and Adams, 2003;Huber et al, 2007;Nakagawa and Takai, 2008;Wagner and Wiegel, 2008;Tsai et al, 2011). All these geological and microbial ecological observations suggest that Fe(III) respiration is the key component of the deep, hot biosphere (Gold, 1992;Kashefi and Lovley, 2003).…”