GP51A-1307
Genomic Insights into the Biomineralization and Environmental Function of Magnetotactic Bacteria
Friday, 18 December 2015
Poster Hall (Moscone South)
Wei Lin, Institute of Geology and Geophysics, Chinese Academy of Sciences, Paleomagnetism and Geochronology Laboratory, Key Laboratory of Earth and Planetary Physics, Beijing, China and Yongxin Pan, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Abstract:
Microorganisms have populated the Earth for billions of years and their activities are important biologic forces shaping our planetary environments. Microbial biomineralization that selectively take up environmental elements (e.g., C, S, P, Fe) and synthesize minerals either intracellularly or extracellularly is of great interest. One of the most interesting examples of these types of organisms are magnetotactic bacteria (MTB), a polyphyletic group of prokaryotes that uptake iron from aquatic habitats and biomineralize intracellular nano-sized iron minerals of magnetite (Fe3O4) and/or greigite (Fe3S4), known as magnetosomes, and orientate and swim along the Earth’s magnetic field. However, our knowledge on the biomineralization mechanisms of MTB and their environmental function remains very limited because the genomic information of most MTB is still not fully understood. By using metagenomic approaches, we have acquired genomic sequences of environmental MTB communities and discovered several conserved genomic fragments containing gene operons for magnetite or greigite biomineralization from Proteobacteria and Nitrospirae MTB. The comparison of these gene clusters has provided valuable insights into the origin and evolution of magnetosome biomineralization. We further obtained several draft genomes of uncultivated MTB belonging to the phylum Nitrospirae, which reveals a metabolic flexibility of this poorly understood magnetotactic group and indicates their considerable roles in the biogeochemical cycles of iron and sulfur.