CIP 109650T
Halobacillus kuroshimensis
JCM 14155;DSM 18393
CIP
Bacteria
yes
Japan
Carbonate rocks authentically formed in a methane seep of the Kuroshima Knoll, located at 642 m depth (Fujikuraet al., 2003; Inagakiet al., 2004), were collected with the remotely operated vehicle Dolphin 3K, operated by the Japan Agency for Marine Earth Science and Technology (JAMSTEC).
30 °C
Aerobic
Int. J. Syst. Evol. Microbiol, 2007, 57, 1243, doi:10.1099/ijs.0.64817-0; Int. J. Syst. Evol. Microbiol, 2007, 57, 1935, doi:10.1099/ijs.0.65395-0; Int. J. Syst. Evol. Microbiol, 2007, 57, 2021, doi:10.1099/ijs.0.65188-0; Int. J. Syst. Evol. Microbiol, 2007, 57, 2727, doi:10.1099/ijs.0.65660-0
2007, JCM <- T. Naganuma, Hiroshima Univ., Hiroshima, Japan: strain IS-Hb7
Deep sea carbonate rock
B
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