Environmental Engineering Reference
In-Depth Information
[21]
Inagaki F., Takai K., Nealson K. H. and Horikoshi K.
Sulfurovum lithotrophicum
gen. nov.,
sp. nov., a novel sulfur-oxidizing chemolithoautotroph within the epsilon-Proteobacteria
isolated from the Okinawa Trough hydrothermal sediments. Int J Syst Evol Microbiol
2004a; 54:1477-88.
[22]
Inagaki F., Tsunogai U., Suzuki M., Kosaka A., Machiyama H., Takai K., Nunoura
T., Nealson, K. H. and Horikoshi K. Characterization of C1-metabolizing prokaryotic
communities in methane seep habitats at the Kuroshima Knoll, the southern Ryukyu arc,
by analyzing
pmoA, mmoX, mxaF, mcrA, and
16S rRNA genes. Appl Environ Microbiol
2004b; 70:7445-55.
[23]
Jan R. L., Wu J., Chaw S. M., Tsal C. W. and Tsen S. D. A novel species of ther-
moacidophilic archaeon,
Sulfolobus yanmingensis
sp. nov. Int J. Syst Bacteriol 1999;
49:1809-16.
[24]
Kamekura M. Diversity of extremely halophilic bacteria. Extremophiles 1998; 2:289-96.
[25]
Karner N. B., DeLong E. F. and Karl D. M. Archaeal dominance in the mesopelagic zone
of the Pacific Ocean. Nature 2001; 409:507-10.
[26]
Kieft T. L., Fredrickson J. K., Onstott T. C., Gorby Y. A., Kostandarithes H. M., Bailey T.
J., Kennedy D. W., Li S. W., Plymale A. E., Spadoni C. M. and Gray M. S. Dissimilatory
reduction of Fe(III) and other electron acceptors by a
Thermus
isolate. Appl Environ
Microbiol 1999; 65:1214-21.
[27]
Kminek G., Bada J. L., Pogliano K. and Ward J. F. Radiation-dependent limit for the
viability of bacterial spores in halite fluid inclusions and on Mars. Radiation Res 2003;
159:722-29.
[28]
Kormas K. A., Smith D. C., Edgcomb V. and Teske A. Molecular analysis of deep
subsurface microbial communities in Nankai Trough sediments (ODP Leg 190, Site
1176). FEMS Microbiol Ecol 2003; 45:115-25.
[29]
Kuwano T., Ogawa Y., Koizumi I. and Oba T. Calcite-cemented Miocene to Pliocene
breccia at the Sanriku Escarpment, Northern Japan Trench. JAMSTEC J Deep Sea Res
1997; 13:573-89. (in Japanese with English abstract)
[30]
Kuypers M. M. M., Blokker P., Hopmans E. C., Kinkel H., Pancost R. D., Schouten S. and
Damste J. S. S. Archaeal remains dominate marine organic matter from the early Albian
oceanic anoxic event 1b. Palaeograph Palaeoclimatol Palaeoecol 2002; 185:211-34.
[31]
Lindahl T. Instability and decay of the primary structure of DNA. Nature 1993; 362:709-
15.
[32]
Larson R. L. latest pulse of Earth: Evidence for a mid-Cretaceous superplume. Geology
1991; 19:547-50.
[33]
Matsushima Y. and Aoki M. Temperature and oxygen isotope variations during formation
of the Hishikari epithermal gold-silver veins, southern Kyushu, Japan. Ecol Geol 1994;
89:1608-13.
[34]
McArthur J. V. D., Kovacic D. A. and Smith M. H. Genetic diversity in natural populations
of a soil bacterium across a landscape gradient. Proc Natl Acad Sci USA 1988; 85:9621-
24.
[35]
McGenity T. J., Gemmell R. T., Grant W. D. and Stan-Lotter H. Origins of halophilic
microorganisms in ancient salt deposits. Environ Microbiol 2000; 2:243-50.
[36]
Mikucki J. A., Liu Y., Delwiche M., Colwell F. S. and Boone D. R. Isolation of a
methanogen from deep marine sediments that contain methane hydrates, and description
of
Methanoculleus submarines
sp. nov. Appl Environ Microbiol 2003; 69:3311-16.
