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Connecting biodiversity and potential functional role in modern euxinic environments by microbial metagenomics

机译:通过微生物宏基因组学联系生物多样性和现代优氧环境中的潜在功能角色

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摘要

Stratified sulfurous lakes are appropriate environments for studying the links between composition and functionality in microbial communities and are potentially modern analogs of anoxic conditions prevailing in the ancient ocean. We explored these aspects in the Lake Banyoles karstic area (NE Spain) through metagenomics and in silico reconstruction of carbon, nitrogen and sulfur metabolic pathways that were tightly coupled through a few bacterial groups. The potential for nitrogen fixation and denitrification was detected in both autotrophs and heterotrophs, with a major role for nitrogen and carbon fixations in Chlorobiaceae. Campylobacterales accounted for a large percentage of denitrification genes, while Gallionellales were putatively involved in denitrification, iron oxidation and carbon fixation and may have a major role in the biogeochemistry of the iron cycle. Bacteroidales were also abundant and showed potential for dissimilatory nitrate reduction to ammonium. The very low abundance of genes for nitrification, the minor presence of anammox genes, the high potential for nitrogen fixation and mineralization and the potential for chemotrophic CO2 fixation and CO oxidation all provide potential clues on the anoxic zones functioning. We observed higher gene abundance of ammonia-oxidizing bacteria than ammonia-oxidizing archaea that may have a geochemical and evolutionary link related to the dominance of Fe in these environments. Overall, these results offer a more detailed perspective on the microbial ecology of anoxic environments and may help to develop new geochemical proxies to infer biology and chemistry interactions in ancient ecosystems.
机译:分层的含硫湖泊是研究微生物群落组成与功能之间联系的合适环境,并且可能是古代海洋中普遍存在的缺氧条件的现代类似物。我们通过宏基因组学和计算机重建碳,氮和硫代谢途径(通过几个细菌群紧密耦合),探索了班约莱斯湖喀斯特地区(西班牙北部)的这些方面。在自养生物和异养生物中都检测到了固氮和反硝化的潜力,这对于绿藻科中的固氮和固碳起着重要作用。弯曲杆菌占反硝化基因的很大比例,而Gallionellales可能参与了反硝化,铁氧化和碳固定,可能在铁循环的生物地球化学中起主要作用。拟杆菌也很丰富,显示出硝酸盐异化还原为铵的潜力。硝化基因的丰度非常低,厌氧氨氧化酶基因的少量存在,固氮和矿化的高潜力以及化学营养性CO2固定和CO氧化的潜力,都为缺氧区域的功能提供了线索。我们观察到氨氧化细菌的基因丰度比氨氧化古细菌更高,后者在这些环境中可能具有与Fe的优势有关的地球化学和进化联系。总体而言,这些结果为缺氧环境的微生物生态学提供了更详细的观点,并可能有助于开发新的地球化学代理来推断古代生态系统中的生物学和化学相互作用。

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