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海洋冷泉沉积物中以 ANME-1 为主导的群落的综合宏基因组和宏蛋白质组分析。

Integrated metagenomic and metaproteomic analyses of an ANME-1-dominated community in marine cold seep sediments.

机构信息

Department of Biology, Centre for Geobiology Department of Earth Science, University of Bergen, Bergen, Norway.

出版信息

Environ Microbiol. 2012 May;14(5):1333-46. doi: 10.1111/j.1462-2920.2012.02716.x. Epub 2012 Mar 9.

Abstract

Sulfate-reducing methanotrophy by anaerobic methanotrophic archaea (ANME) and sulfate-reducing bacteria (SRB) is a major biological sink of methane in anoxic methane-enriched marine sediments. The physiology of a microbial community dominated by free-living ANME-1 at 14-16 cm below the seafloor in the G11 pockmark at Nyegga was investigated by integrated metagenomic and metaproteomic approaches. Total DNA was subjected to 454-pyrosequencing (829 527 reads), and 16.6 Mbp of sequence information was assembled into 27352 contigs. Taxonomic analysis supported a high abundance of Euryarchaea (70%) with 66% of the assembled metagenome belonging to ANME-1. Extracted sediment proteins were separated in two dimensions and subjected to mass spectrometry (LTQ-Orbitrap XL). Of 356 identified proteins, 245 were expressed by ANME-1. These included proteins for cold-adaptation and production of gas vesicles, reflecting both the adaptation of the ANME-1 community to a permanently cold environment and its potential for positioning in specific sediment depths respectively. In addition, key metabolic enzymes including the enzymes in the reverse methanogenesis pathway (except N(5) ,N(10) -methylene-tetrahydromethanopterin reductase), heterodisulfide reductases and the F(420) H(2) :quinone oxidoreductase (Fqo) complex were identified. A complete dissimilatory sulfate reduction pathway was expressed by sulfate-reducing Deltaproteobacteria. Interestingly, an APS-reductase comprising Gram-positive SRB and related sequences were identified in the proteome. Overall, the results demonstrated that our approach was effective in assessing in situ metabolic processes in cold seep sediments.

摘要

硫酸盐还原产甲烷作用由厌氧甲烷营养古菌 (ANME) 和硫酸盐还原菌 (SRB) 驱动,是缺氧富甲烷海洋沉积物中甲烷的主要生物汇。通过整合宏基因组学和宏蛋白质组学方法,研究了尼格加 G11 麻坑 14-16 厘米深处以自由生活的 ANME-1 为主导的微生物群落的生理学。对总 DNA 进行了 454 焦磷酸测序(829527 个读数),并将 16.6 Mbp 的序列信息组装成 27352 个连续序列。分类分析支持古菌(70%)的丰度很高,组装的宏基因组中有 66%属于 ANME-1。提取的沉积物蛋白进行二维分离,并进行质谱分析(LTQ-Orbitrap XL)。在鉴定的 356 种蛋白质中,有 245 种由 ANME-1 表达。这些蛋白质包括冷适应和气泡囊的产生蛋白,分别反映了 ANME-1 群落对永久低温环境的适应及其在特定沉积物深度定位的潜力。此外,还鉴定了关键代谢酶,包括反向产甲烷途径中的酶(除 N(5) 、N(10) -亚甲基四氢叶酸还原酶)、异源二硫化物还原酶和 F(420) H(2) :醌氧化还原酶(Fqo)复合物。硫酸盐还原 δ 变形菌表达了完整的异化硫酸盐还原途径。有趣的是,在蛋白质组中鉴定到了包含革兰氏阳性 SRB 和相关序列的 APS 还原酶。总的来说,结果表明我们的方法有效地评估了冷渗沉积物中的原位代谢过程。

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