“…MCG are present in terrestrial hot springs , deep oceanic subsurface sediments (Parkes et al, 2005), deep terrestrial subsurface (Inagaki et al, 2003), continental shelf sediments (Vetriani et al, 1998), ancient marine sapropels (Coolen et al, 2002), petroleum-contaminated soil (Kasai et al, 2005), termite guts (Friedrich et al, 2001), mud volcanoes (Heijs et al, 2007), methane hydrate-containing marine sediments (Inagaki et al, 2006), landfill leachate (Huang et al, 2003), anaerobic wastewater reactors (Collins et al, 2005), sulfidic springs (Elshahed et al, 2003), brackish lakes (Hershberger et al, 1996) and coastal salt marshes (Castro et al, 2004). Only 28 out of 4720 MCG sequences were retrieved from potentially oxic habitats (for example, database releases EU370096 and FJ560325).…”