Hiraoka Satoshi, Machiyama Asako, Ijichi Minoru, Inoue Kentaro, Oshima Kenshiro, Hattori Masahira, Yoshizawa Susumu, Kogure Kazuhiro, Iwasaki Wataru
Department of Computational Biology and Medical Sciences, Graduate School of Frontier Sciences, the University of Tokyo, Chiba, 277-8568, Japan.
Department of Biological Sciences, Graduate School of Science, the University of Tokyo, Tokyo, 113-0032, Japan.
BMC Genomics. 2016 Jan 14;17:53. doi: 10.1186/s12864-016-2380-4.
The Great East Japan Earthquake of 2011 triggered large tsunami waves, which flooded broad areas of land along the Pacific coast of eastern Japan and changed the soil environment drastically. However, the microbial characteristics of tsunami-affected soil at the genomic level remain largely unknown. In this study, we isolated microbes from a soil sample using general low-nutrient and seawater-based media to investigate microbial characteristics in tsunami-affected soil.
As expected, a greater proportion of strains isolated from the tsunami-affected soil than the unaffected soil grew in the seawater-based medium. Cultivable strains in both the general low-nutrient and seawater-based media were distributed in the genus Arthrobacter. Most importantly, whole-genome sequencing of four of the isolated Arthrobacter strains revealed independent losses of siderophore-synthesis genes from their genomes. Siderophores are low-molecular-weight, iron-chelating compounds that are secreted for iron uptake; thus, the loss of siderophore-synthesis genes indicates that these strains have adapted to environments with high-iron concentrations. Indeed, chemical analysis confirmed the investigated soil samples to be rich in iron, and culture experiments confirmed weak cultivability of some of these strains in iron-limited media. Furthermore, metagenomic analyses demonstrated over-representation of denitrification-related genes in the tsunami-affected soil sample, as well as the presence of pathogenic and marine-living genera and genes related to salt-tolerance.
Collectively, the present results would provide an example of microbial characteristics of soil disturbed by the tsunami, which may give an insight into microbial adaptation to drastic environmental changes. Further analyses on microbial ecology after a tsunami are envisioned to develop a deeper understanding of the recovery processes of terrestrial microbial ecosystems.
2011年东日本大地震引发了巨大的海啸,淹没了日本东部太平洋沿岸的大片土地,土壤环境发生了巨大变化。然而,在基因组水平上,受海啸影响土壤的微生物特征仍 largely unknown。在本研究中,我们使用普通低营养和海水培养基从土壤样本中分离微生物,以研究受海啸影响土壤的微生物特征。
正如预期的那样,从受海啸影响土壤中分离出的菌株比未受影响土壤中分离出的菌株在海水培养基中生长的比例更高。普通低营养和海水培养基中的可培养菌株均分布在节杆菌属。最重要的是,对四株分离出的节杆菌菌株进行全基因组测序发现,它们的基因组中独立缺失了铁载体合成基因。铁载体是分泌用于摄取铁的低分子量铁螯合化合物;因此,铁载体合成基因的缺失表明这些菌株已经适应了高铁浓度的环境。事实上,化学分析证实所研究的土壤样本富含铁,培养实验证实其中一些菌株在铁限制培养基中的可培养性较弱。此外,宏基因组分析表明,在受海啸影响的土壤样本中,与反硝化相关的基因过度表达,并且存在致病属和海洋生物属以及与耐盐性相关的基因。
总的来说,目前的结果将提供一个受海啸干扰土壤的微生物特征的例子,这可能有助于深入了解微生物对剧烈环境变化的适应。预计对海啸后微生物生态学的进一步分析将有助于更深入地了解陆地微生物生态系统的恢复过程。