对氮和硫循环的影响:陆地含水层中硝化螺藻的系统发育和生态位范围

IF 5.1 Q1 ECOLOGY ISME communications Pub Date : 2024-03-27 DOI:10.1093/ismeco/ycae047
Olivia E. Mosley, Emilie Gios, Kim M. Handley
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引用次数: 0

摘要

越来越多的证据表明,硝螺虫是水生和地下氮和硫循环的重要贡献者。在这里,我们确定了定殖于陆地含水层的硝螺藻的系统发育和生态位关联。利用 16S rRNA 基因测定了 59 口地下水井中的硝螺藻成分。分析表明,硝螺藻的分布受地下水中氧气供应量的影响很大,其特点是好氧(硝螺藻、Leptospirillum)和厌氧(Thermodesulfovibrionia、未分类)菌系之间的权衡。七个硝螺菌元基因组(MAGs)来自一个井的子集,其中三个来自最近指定的 "9FT-COMBO-42-15 "类。其中大多数在缺氧地下水中含量相对较高,转录也相对活跃。这些 MAG 与其他 743 个硝螺虫基因组一起进行了分析。结果表明,某些品系在含水层中占主导地位(例如,非硝化硝螺菌,9FT-COMBO-42-15 类和 UBA9217 类,Thermodesulfovibrionales 家族 UBA1546)。这些菌系的特点是具有硝酸盐还原和硫循环机制,除硝化螺菌外,还具有伍德-荣格达尔途径,与碳限制、低氧和富含硫的含水层条件相一致。9FT-COMBO-42-15 类是 Nitrospiria 的姊妹支系,由两个家族组成,跨越了碳固定方法的转变:f_HDB-SIOIB13 编码 rTCA(如 Nitrospiria),f_9FT-COMBO-42-15 编码 Wood-Ljungdahl CO 脱氢酶(如 Thermodesulfovibrionia 和 UBA9217)。9FT-COMBO-42-15 家族还可通过硫氧化能力(通过 DsrABEFH 和 SoxXAYZB)和将硝酸盐还原为氨的异氨还原能力进一步区分。f_9FT-COMBO-42-15 MAG(nzgw271)的基因转录表明,缺氧地下水中氮、硫循环的耦合十分活跃。研究结果表明,硝螺藻广泛分布于地下水中,氧气的可用性驱动了与氮和硫代谢相关的生态作用截然不同的品系的空间分化。
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Implications for nitrogen and sulfur cycles: phylogeny and niche-range of Nitrospirota in terrestrial aquifers
Increasing evidence suggests Nitrospirota are important contributors to aquatic and subsurface nitrogen and sulfur-cycles. Here we determined the phylogenetic and ecological niche associations of Nitrospirota colonising terrestrial aquifers. Nitrospirota compositions were determined across 59 groundwater wells using 16S rRNA genes. Analyses showed Nitrospirota distributions were strongly influenced by oxygen availability in groundwater, marked by a trade-off between aerobic (Nitrospira, Leptospirillum) and anaerobic (Thermodesulfovibrionia, unclassified) lineages. Seven Nitrospirota metagenome-assembled genomes (MAGs) from a subset of wells included three from the recently designated class '9FT-COMBO-42-15'. Most were relatively more abundant, and transcriptionally active, in dysoxic groundwater. These MAGs were analysed with 743 other Nitrospirota genomes. Results illustrate the predominance of certain lineages in aquifers (e.g., non-nitrifying Nitrospiria, classes 9FT-COMBO-42-15 and UBA9217, Thermodesulfovibrionales family UBA1546). These lineages are characterised by mechanisms for nitrate reduction and sulfur-cycling, and, excluding Nitrospiria, the Wood-Ljungdahl pathway, consistent with carbon-limited, low-oxygen and sulfur-rich aquifer conditions. Class 9FT-COMBO-42-15 is a sister clade of Nitrospiria, and comprises two families spanning a transition in carbon fixation approaches: f_HDB-SIOIB13 encodes rTCA (like Nitrospiria) and f_9FT-COMBO-42-15 encodes Wood-Ljungdahl CO dehydrogenase (like Thermodesulfovibrionia and UBA9217). The 9FT-COMBO-42-15 family is further differentiated by the capacity for sulfur oxidation (via DsrABEFH and SoxXAYZB) and dissimilatory nitrate reduction to ammonium. Gene transcription by a f_9FT-COMBO-42-15 MAG, nzgw271, indicated active coupling of nitrogen and sulfur cycles in dysoxic groundwater. Results indicate that Nitrospirota are widely distributed in groundwater, and that oxygen availability drives the spatial differentiation of lineages with ecologically distinct roles related to nitrogen and sulfur metabolism.
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