College of Life Sciences, Zhejiang University, Hangzhou, China.
FEMS Microbiol Ecol. 2011 Dec;78(3):565-85. doi: 10.1111/j.1574-6941.2011.01186.x. Epub 2011 Sep 15.
Cobalt-rich crusts are important metallic mineral resources with great economic potential, usually distributed on seamounts located in the Pacific Ocean. Microorganisms are believed to play a role in the formation of crusts as well as in metal cycling. To explore the microbial diversity related to cobalt-rich crusts, 16S ribosomal RNA gene clone libraries were constructed from three consecutive sediment layers. In total, 417 bacterial clones were obtained from three bacterial clone libraries, representing 17 distinct phylogenetic groups. Proteobacteria dominated in the bacterial communities, followed by Acidobacteria and Planctomycetes. Compared with high bacterial diversity, archaea showed a remarkably low diversity, with all 137 clones belonging to marine archaeal group I except one novel euryarchaeotal clone. The microbial communities were potentially involved in sulfur, nitrogen and metal cycling in the area of cobalt-rich crusts. Sulfur oxidation and metal oxidation were potentially major sources of energy for this ecosystem. This is the first reported investigation of microbial diversity in sediments associated with cobalt-rich crusts, and it casts fresh light on the microbial ecology of these important ecosystems.
富含钴结壳是一种具有巨大经济潜力的重要金属矿产资源,通常分布在太平洋的海山。微生物被认为在结壳的形成以及金属循环中发挥作用。为了探索与富含钴结壳相关的微生物多样性,从三个连续的沉积物层中构建了 16S 核糖体 RNA 基因克隆文库。总共从三个细菌克隆文库中获得了 417 个细菌克隆,代表了 17 个不同的系统发育群。变形菌在细菌群落中占主导地位,其次是酸杆菌门和浮霉菌门。与高细菌多样性相比,古菌的多样性明显较低,除了一个新的广古菌克隆外,所有 137 个克隆都属于海洋古菌组 I。微生物群落可能参与了富钴结壳区域的硫、氮和金属循环。硫氧化和金属氧化可能是该生态系统的主要能源来源。这是首次对与富含钴结壳相关的沉积物中的微生物多样性进行的调查,为这些重要生态系统的微生物生态学提供了新的认识。