“…δ-Proteobacteria were the most abundant group in cold seeps in the Japan Trench (6200 m) (Li et al, 1999) and ε-Proteobacteria, along with γ-and α-Proteobacteria, composed the majority of sequences from some deep sea hydrothermal vent systems (Moyer et al, 1995(Moyer et al, , 1998Reysenbach et al, 2000). Other relatively abundant taxa include the Cytophaga/Flavobacteria/ Bacteroidetes group (Li et al, 1999;Nercessian et al, 2005;Xu et al, 2005;Zeng et al, 2005;Martín-Cuadrado et al, 2007), Planctomycetes (Nercessian et al, 2005;Zeng et al, 2005;DeLong et al, 2006;Martín-Cuadrado et al, 2007;Jamieson et al, 2013;Wu et al, 2013), Chloroflexi (mainly affiliated with Dehalococcoidetes (Inagaki and Nakagawa, 2008)) (DeLong et al, 2006;Martín-Cuadrado et al, 2007;Pachiadaki et al, 2011), Acidobacteria (Martín-Cuadrado et al, 2007;Wu et al, 2013), Firmicutes (Li et al, 1999;Zeng et al, 2005;Martín-Cuadrado et al, 2007), CFB group (Xu et al, 2005;Zeng et al, 2005), JS1 candidate division (previously joined with the OP9 candidate division) (Inagaki et al, 2003(Inagaki et al, , 2006Inagaki and Nakagawa, 2008) and Actinobacteria (Jamieson et al, 2013;Wu et al, 2013). Functions such as sulfate reduction in hydrothermal vents and cold seeps have been mainly attributed to ε-and δ-Proteobacteria (Desulfococcus and Desulfosarcina) (Longnecker and Reysenbach, 2001;Inagaki et al, 2002;Zeng et al, 2005), sulfur oxidation to γ-and ε-Proteobacteria …”