Colquhoun J A, Mexson J, Goodfellow M, Ward A C, Horikoshi K, Bull A T
Department of Biosciences, University of Kent, Canterbury, UK.
Antonie Van Leeuwenhoek. 1998 Jul-Oct;74(1-3):27-40. doi: 10.1023/a:1001743625912.
A large number of mycolate actinomycetes have been recovered from deep-sea sediments in the NW Pacific Ocean using selective isolation methods. The isolates were putatively assigned to the genus Rhodococcus on the basis of colony characteristics and mycolic acid profiles. The diversity among these isolates and their relationship to type strains of Rhodococcus and other mycolate 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. Cluster A was a large group of isolates recovered from sediment in the Izu Bonin Trench (2679 m); Cluster C comprised isolates from both the Izu Bonin Trench (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 isolates recovered from a sediment taken from a depth of 1168 m in Sagami Bay and 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 deep-sea sediments studied was indicative of the movement of terrestrial material into the ocean depths. 16S ribosomal RNA gene sequence analyses produced excellent definition of most genera of the mycolata, and indicated that the among the deep sea isolates (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 considerable diversity among the deep sea rhodococci and evidence for recently diverged species or DNA groups.
利用选择性分离方法,已从西北太平洋的深海沉积物中分离出大量含分枝菌酸的放线菌。根据菌落特征和分枝菌酸谱,这些分离菌株被初步归为红球菌属。通过居里点热解质谱法(PyMS)评估了这些分离菌株之间的多样性及其与红球菌属模式菌株和其他含分枝菌酸分类单元的关系。PyMS确定了三个主要组(A、C、D)和两个次要组(B、E)。A组是从伊豆-小笠原海沟(2679米)沉积物中分离出的一大组菌株;C组包括来自伊豆-小笠原海沟(6390米和6499米)以及日本海沟(4418米、6048米和6455米)的分离菌株。这些C组分离菌株与海氏迪茨氏菌表现出密切相似性,随后通过分子方法得以证实。D组包含从相模湾1168米深处沉积物中分离出的菌株,被鉴定为陆地物种藤黄红球菌的成员。B组和E组与戈登氏菌属和分枝杆菌属的成员有密切亲缘关系。在所研究的某些深海沉积物中存在嗜热放线菌,这表明陆地物质已进入海洋深处。16S核糖体RNA基因序列分析对大多数含分枝菌酸菌属进行了很好的界定,并表明在深海分离菌株中,(1)存在棒状杆菌属、戈登氏菌属和分枝杆菌属的新物种,(2)在日本海分离出的一个菌株,其系统发育深度表明可能存在一个新属。多相分类分析揭示了深海红球菌之间存在相当大的多样性,以及近期分化出的物种或DNA组的证据。