Phylogenetic analysis of psychrophilic bacteria isolated from the Japan Trench, including a description of the deep-sea species Psychrobacter pacificensis sp nov.
A. Maruyama et al., Phylogenetic analysis of psychrophilic bacteria isolated from the Japan Trench, including a description of the deep-sea species Psychrobacter pacificensis sp nov., INT J SY EV, 50, 2000, pp. 835-846
Citations number
46
Categorie Soggetti
Microbiology
Journal title
INTERNATIONAL JOURNAL OF SYSTEMATIC AND EVOLUTIONARY MICROBIOLOGY
Phylogenetic positions of psychrophilic bacteria isolated from the Japan Tr
ench were determined by sequencing analysis of PCR-amplified bacterial smal
l subunit (16S) rRNA genes. Between surface and deep-sea psychrophiles. dis
tinct positions clearly differed within the gamma-Proteobacteria, In phylog
enetic analysis using neighbour-joining, maximum-parsimony and maximum-like
lihood, strains from surface seawater were inferred to be located in the Ha
lomonas aquamarina-meridiana clade within the family Halomonadaceae, Strain
s from deep seawater (5000-6000 m), however, formed a novel monophyletic cl
ade within the Moraxella-Psychrobacter branch in the family Moraxellaceae,
showing separation from terrestrial and Antarctic relatives. These deep-sea
strains were also discriminated from other known Psychrobacter species in
phenotype, e.g. limited growth in the absence of NaCl (optimum at about 3%
NaCl), positive urease activity, acid production from xylose and arabinose,
and the presence of multiple fimbriae, DNA relatedness values among six de
ep-sea strains were >85% in DNA-DNA hybridization experiments and greater t
han or equal to 98% in aligned 165 rDNA sequences. From this evidence, a ne
w species, Psychrobacter pacificensis, is proposed for these deep-sea psych
rophiles; the type strain of Psychrobacter pacificensis is strain NIBH P2K6
(T) (= IFO 16270(T)), Occurrence of psychrobacters in cold Japan Trench dee
p seawater and at the Antarctic sea surface suggests that deep-sea bacteria
l habitation and evolution have been mediated by global deep-ocean circulat
ion linked to the sinking of cooled seawater in polar regions.