A large number of mycolate actinomycetes have been recovered from deep-sea
sediments in the NW Pacific Ocean using selective isolation methods. The is
olates were putatively assigned to the genus Rhodococcus on the basis of co
lony characteristics and mycolic acid profiles. The diversity among these i
solates and their relationship to type strains of Rhodococcus and other myc
olate taxa were assessed by Curie point pyrolysis mass spectrometry (PyMS).
Three major (A, C, D) and two minor (B, E) groups were defined by PyMS. Cl
uster A was a large group of isolates recovered from sediment in the Izu Bo
nin Trench (2679 m); Cluster C comprised isolates from both the Izu Bonin T
rench (6390 and 6499 m) and from the Japan Trench (4418, 6048 and 6455 m).
These Cluster C isolates showed close similarity to Dietzia maris and this
was subsequently confirmed using molecular methods. Cluster D contained iso
lates recovered from a sediment taken from a depth of 1168m in Sagami Bay a
nd were identified as members of the terrestrial species Rhodococcus luteus
. Clusters B and E had close affinities with members of the genera Gordonia
and Mycobacterium. The presence of Thermoactinomyces in certain of the dee
p-sea sediments studied was indicative of the movement of terrestrial mater
ial into the ocean depths.
16S ribosomal RNA gene sequence analyses produced excellent definition of m
ost genera of the mycolata, and indicated that the among the deep sea isola
tes (1) were novel species of Corynebacterium, Gordonia and Mycobacterium,
and (2) a Sea of Japan isolate the phylogenetic depth of which suggests the
possibility of a new genus. Polyphasic taxonomic analysis revealed conside
rable diversity among the deep sea rhodococci and evidence for recently div
erged species or DNA groups.