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1 inct pathways for arginine breakdown in each halophile.
2  are considerably larger, on average, in the halophile.
3 than for the corresponding proteins from non-halophiles.
4 e in the domain Archaea are obligate extreme halophiles.
5 spects of theories for understanding extreme halophiles.
6 halophile Haloarcula marismortui and the non-halophile anabaena.
7 an unusual peptide that is unique to several halophile archaeal cysteinyl-tRNA synthetases (CysRS), w
8 at approximately 67% ribosomal proteins from halophiles are negatively charged, whereas only up to ap
9 ne knockouts and replacements, indicate this halophile can serve as an excellent model system among t
10  acids do comprise a foldable set within the halophile environment.
11   This result indicates that the capacity of halophiles for aerobic respiration may have been acquire
12                              Archaebacterial halophiles (Haloarchaea) are oxygen-respiring heterotrop
13 the stability of 2Fe-2S ferredoxins from the halophile Haloarcula marismortui and the non-halophile a
14 mologs in the genomic sequences of two other halophiles, Haloarcula marismortui and Haloferax volcani
15                  In the CysRS of the extreme halophile Halobacterium species NRC-1, deletion of the p
16 m the chromosome of an archaeon, the extreme halophile Halobacterium strain NRC-1.
17 ross archaeal lineages: a photoheterotrophic halophile (Halobacterium salinarum NRC-1), a hydrogenotr
18 e report the complete sequence of an extreme halophile, Halobacterium sp. NRC-1, harboring a dynamic
19 V) prepared from the polar lipids of extreme halophiles, Halobacterium halobium and Halobacterium sal
20              Using the genetically tractable halophile Haloferax volcanii as a model system, we descr
21 nucleosome occupancy map, as observed in the halophile Haloferax volcanii.
22 ification enzymes in the mesophilic moderate halophile Haloferax volcanii.
23  acidophile, Sulfolobus sofataricus (Sso); a halophile, Haloferax volcanii (Hvo); and a hyperthermoph
24              In anaerobic batch culture, the halophile Halomonas halodenitrificans is shown to be abl
25 omal proteins from all organisms, especially halophiles, has distinct positive and negative regions a
26                   The archaeon TBP, from the halophile/hyperthermophile organism Pyrococcus woesei, i
27 ehaviors of Halobacterium NRC-1, an archaeal halophile, in sublethal levels of Mn(II), Fe(II), Co(II)
28 types: they were either methanogens, extreme halophiles, or ('sulphur-dependent') extreme thermophile
29 sly described Thermococcus kodakaraensis and halophile proteins.
30 oximately 15% of ribosomal proteins from non-halophiles share this property.
31 and the hvDHFRs by a common mechanism, not a halophile-specific mechanism, such as the binding of hyd
32                       The functions of these halophile-specific peptides are largely unknown.
33 c techniques are available--the methanogens, halophiles, Sulfolobales, and Thermococcales--with the a
34     Many archaeal sequences (methanogens and halophiles) tend to align best with the Gram-positive se
35 ends to be lower for ribosomal proteins from halophiles than for the corresponding proteins from non-
36                 Vibrio parahaemolyticus is a halophile that inhabits brackish waters and a wide range
37 is may result from the specific lifestyle of halophiles that require high intracellular salt concentr
38 encing projects are under way, including two halophiles, two Thermoplasma, and a methanogen.
39 ns show the definite archaeal nature of this halophile with additional similarities to the Gram-posit

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