van Grinsven Sigrid, Sinninghe Damsté Jaap S, Harrison John, Villanueva Laura
Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, Utrecht University, Utrecht, Netherlands.
Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands.
Front Microbiol. 2020 May 14;11:715. doi: 10.3389/fmicb.2020.00715. eCollection 2020.
Methanotrophs are of major importance in limiting methane emissions from lakes. They are known to preferably inhabit the oxycline of stratified water columns, often assumed due to an intolerance to atmospheric oxygen concentrations, but little is known on the response of methanotrophs to different oxygen concentrations as well as their preference for different electron acceptors. In this study, we enriched a methanotroph of the genus from the oxycline and the anoxic water column of a stratified lake, which was also present in the oxic water column in the winter. We tested the response of this -dominated enrichment culture to different electron acceptors, i.e., oxygen, nitrate, sulfate, and humic substances, and found that, in contrast to earlier results with water column incubations, oxygen was the preferred electron acceptor, leading to methane oxidation rates of 45-72 pmol cell day. Despite the general assumption of methanotrophs preferring microaerobic conditions, methane oxidation was most efficient under high oxygen concentrations (>600 μM). Low (<30 μM) oxygen concentrations still supported methane oxidation, but no methane oxidation was observed with trace oxygen concentrations (<9 μM) or under anoxic conditions. Remarkably, the presence of nitrate stimulated methane oxidation rates under oxic conditions, raising the methane oxidation rates by 50% when compared to oxic incubations with ammonium. Under anoxic conditions, no net methane consumption was observed; however, methanotroph abundances were two to three times higher in incubations with nitrate and sulfate compared to anoxic incubations with ammonium as the nitrogen source. Metagenomic sequencing revealed the absence of a complete denitrification pathway in the dominant methanotroph , but the most abundant methylotroph seemed capable of denitrification, which can possibly play a role in the enhanced methane oxidation rates under nitrate-rich conditions.
甲烷氧化菌对于限制湖泊甲烷排放至关重要。已知它们通常栖息于分层水柱的氧化还原界面,这通常被认为是由于它们不耐受大气中的氧气浓度,但关于甲烷氧化菌对不同氧气浓度的响应以及它们对不同电子受体的偏好知之甚少。在本研究中,我们从一个分层湖泊的氧化还原界面和缺氧水柱中富集了一种 属的甲烷氧化菌,该菌在冬季的含氧水柱中也有存在。我们测试了这种以 为主的富集培养物对不同电子受体(即氧气、硝酸盐、硫酸盐和腐殖质)的响应,发现与早期水柱培养的结果相反,氧气是首选的电子受体,导致甲烷氧化速率为45 - 72皮摩尔/细胞·天。尽管通常认为甲烷氧化菌更喜欢微需氧条件,但在高氧气浓度(>600 μM)下甲烷氧化最为有效。低(<30 μM)氧气浓度仍能支持甲烷氧化,但在微量氧气浓度(<9 μM)或缺氧条件下未观察到甲烷氧化。值得注意的是,硝酸盐的存在刺激了有氧条件下的甲烷氧化速率,与用铵进行的有氧培养相比,甲烷氧化速率提高了50%。在缺氧条件下,未观察到净甲烷消耗;然而,与以铵作为氮源的缺氧培养相比,在添加硝酸盐和硫酸盐的培养中,甲烷氧化菌的丰度高出两到三倍。宏基因组测序显示优势甲烷氧化菌中不存在完整的反硝化途径,但最丰富的甲基营养菌似乎能够进行反硝化,这可能在富含硝酸盐条件下提高甲烷氧化速率中发挥作用。