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琉球石灰岩含水层中微生物群落及其氮代谢基因相关网络的宏基因组分析。

Metagenomic analysis of the microbial communities and associated network of nitrogen metabolism genes in the Ryukyu limestone aquifer.

机构信息

Kitasato University School of Marine Biosciences, 1-15-1 Kitasato, Minami, Sagamihara, Kanagawa, 252-0373, Japan.

National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba Central 7, 1-1-1 Higashi, Tsukuba, Ibaraki, 305-8567, Japan.

出版信息

Sci Rep. 2024 Feb 22;14(1):4356. doi: 10.1038/s41598-024-54614-8.

Abstract

While microbial biogeochemical activities such as those involving denitrification and sulfate reduction have been considered to play important roles in material cycling in various aquatic ecosystems, our current understanding of the microbial community in groundwater ecosystems is remarkably insufficient. To assess the groundwater in the Ryukyu limestone aquifer of Okinawa Island, which is located in the southernmost region of Japan, we performed metagenomic analysis on the microbial communities at the three sites and screened for functional genes associated with nitrogen metabolism. 16S rRNA amplicon analysis showed that bacteria accounted for 94-98% of the microbial communities, which included archaea at all three sites. The bacterial communities associated with nitrogen metabolism shifted by month at each site, indicating that this metabolism was accomplished by the bacterial community as a whole. Interestingly, site 3 contained much higher levels of the denitrification genes such as narG and napA than the other two sites. This site was thought to have undergone denitrification that was driven by high quantities of dissolved organic carbon (DOC). In contrast, site 2 was characterized by a high nitrate-nitrogen (NO-N) content and a low amount of DOC, and this site yielded a moderate amount of denitrification genes. Site 1 showed markedly low amounts of all nitrogen metabolism genes. Overall, nitrogen metabolism in the Ryukyu limestone aquifer was found to change based on environmental factors.

摘要

虽然微生物生物地球化学活性(如反硝化和硫酸盐还原)被认为在各种水生生态系统的物质循环中发挥着重要作用,但我们目前对地下水生态系统中微生物群落的了解还远远不够。为了评估位于日本最南端冲绳岛的琉球石灰岩含水层中的地下水,我们对三个地点的微生物群落进行了宏基因组分析,并筛选了与氮代谢相关的功能基因。16S rRNA 扩增子分析表明,细菌在所有三个地点都占微生物群落的 94-98%,其中包括古菌。与氮代谢相关的细菌群落随月份在每个地点发生变化,表明这种代谢是由整个细菌群落完成的。有趣的是,地点 3 含有比其他两个地点高得多的反硝化基因,如 narG 和 napA。该地点被认为发生了由大量溶解有机碳 (DOC) 驱动的反硝化作用。相比之下,地点 2 的硝酸盐氮 (NO-N) 含量较高,DOC 含量较低,且该地点产生了中等数量的反硝化基因。地点 1 显示出所有氮代谢基因的含量明显较低。总体而言,琉球石灰岩含水层中的氮代谢是根据环境因素而变化的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f121/10883930/8437c2eb39d6/41598_2024_54614_Fig1_HTML.jpg

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