The water column of the Yamal tundra lakes as a microbial filter preventing methane emission

A. Savvichev, I. Rusanov, Y. Dvornikov, V. Kadnikov, A. Kallistová, E. Veslopolova, A. Chetverova, M. Leibman, P. Sigalevich, N. Pimenov, N. Ravin, A. Khomutov
{"title":"The water column of the Yamal tundra lakes as a microbial filter preventing methane emission","authors":"A. Savvichev, I. Rusanov, Y. Dvornikov, V. Kadnikov, A. Kallistová, E. Veslopolova, A. Chetverova, M. Leibman, P. Sigalevich, N. Pimenov, N. Ravin, A. Khomutov","doi":"10.5194/BG-18-2791-2021","DOIUrl":null,"url":null,"abstract":"Abstract. Microbiological, molecular ecological, biogeochemical, and isotope geochemical research was carried out in four lakes of the central part of the Yamal Peninsula in the area of continuous permafrost. Two of them were large (73.6 and 118.6 ha) and deep (up to 10.6 and 12.3 m) mature lakes embedded into all geomorphological levels of the peninsula, and two others were smaller (3.2 and 4.2 ha) shallow (up to 2.3 and 1.8 m) lakes which appeared as a result of thermokarst on constitutional (segregated) ground ice. We collected samples in August 2019. The Yamal tundra lakes exhibited high phytoplankton production (340–1200 mg C m−2 day−1) during the short summer season. Allochthonous and autochthonous, both particulate and dissolved organic matter was deposited to the bottom sediments, where methane production occurred due to anaerobic degradation (90–1000 µmol СН4 dm−3). The rates of hydrogenotrophic methanogenesis appeared to be higher in the sediments of deep lakes than in those of the shallow ones. In the sediments of all lakes, Methanoregula and Methanosaeta were predominant components of the archaeal methanogenic community. Methane oxidation (1.4–9.9 µmol dm−3 day−1) occurred in the upper sediment layers simultaneously with methanogenesis. Methylobacter tundripaludum (family Methylococcaceae) predominated in the methanotrophic community of the sediments and the water column. The activity of methanotrophic bacteria in deep mature lakes resulted in a decrease of the dissolved methane concentration in lake water from 0.8–4.1 µmol CH4 L−1 to 0.4 µmol CH4 L−1, while in shallow thermokarst lakes the geochemical effect of methanotrophs was much less pronounced. Thus, only small shallow Yamal lakes may contribute significantly to the overall diffusive methane emissions from the water surface during the warm summer season. The water column of large deep lakes on Yamal acts, however, as a microbial filter preventing methane emission into the atmosphere.","PeriodicalId":89897,"journal":{"name":"Biogeosciences discussions : (BGD)","volume":"18 1","pages":"2791-2807"},"PeriodicalIF":0.0000,"publicationDate":"2021-05-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Biogeosciences discussions : (BGD)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/BG-18-2791-2021","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 7

Abstract

Abstract. Microbiological, molecular ecological, biogeochemical, and isotope geochemical research was carried out in four lakes of the central part of the Yamal Peninsula in the area of continuous permafrost. Two of them were large (73.6 and 118.6 ha) and deep (up to 10.6 and 12.3 m) mature lakes embedded into all geomorphological levels of the peninsula, and two others were smaller (3.2 and 4.2 ha) shallow (up to 2.3 and 1.8 m) lakes which appeared as a result of thermokarst on constitutional (segregated) ground ice. We collected samples in August 2019. The Yamal tundra lakes exhibited high phytoplankton production (340–1200 mg C m−2 day−1) during the short summer season. Allochthonous and autochthonous, both particulate and dissolved organic matter was deposited to the bottom sediments, where methane production occurred due to anaerobic degradation (90–1000 µmol СН4 dm−3). The rates of hydrogenotrophic methanogenesis appeared to be higher in the sediments of deep lakes than in those of the shallow ones. In the sediments of all lakes, Methanoregula and Methanosaeta were predominant components of the archaeal methanogenic community. Methane oxidation (1.4–9.9 µmol dm−3 day−1) occurred in the upper sediment layers simultaneously with methanogenesis. Methylobacter tundripaludum (family Methylococcaceae) predominated in the methanotrophic community of the sediments and the water column. The activity of methanotrophic bacteria in deep mature lakes resulted in a decrease of the dissolved methane concentration in lake water from 0.8–4.1 µmol CH4 L−1 to 0.4 µmol CH4 L−1, while in shallow thermokarst lakes the geochemical effect of methanotrophs was much less pronounced. Thus, only small shallow Yamal lakes may contribute significantly to the overall diffusive methane emissions from the water surface during the warm summer season. The water column of large deep lakes on Yamal acts, however, as a microbial filter preventing methane emission into the atmosphere.
亚马尔苔原湖的水柱作为防止甲烷排放的微生物过滤器
摘要对亚马尔半岛中部连续多年冻土区的四个湖泊进行了微生物学、分子生态学、生物地球化学和同位素地球化学研究。其中两个较大(73.6和118.6 ha)和深(高达10.6和12.3 m) 成熟的湖泊嵌入半岛的所有地貌层次,另外两个较小(3.2和4.2 ha)浅层(高达2.3和1.8 m) 由于构成的(分离的)地面冰上的热岩溶而出现的湖泊。我们在2019年8月采集了样本。亚马尔苔原湖的浮游植物产量很高(340–1200 毫克 C m−2 第−1天)。外来和本地的颗粒和溶解有机物都沉积在底部沉积物中,由于厌氧降解,甲烷在那里产生(90-1000 µmol СН4 dm−3)。深湖沉积物中的氢营养甲烷生成率似乎高于浅湖沉积物。在所有湖泊的沉积物中,甲烷菌和甲烷菌是古菌产甲烷群落的主要组成部分。甲烷氧化(1.4–9.9 µmol dm−3 第−1天)与甲烷生成同时发生在上层沉积物层。苔原甲杆菌(甲基球菌科)在沉积物和水柱的甲烷营养群落中占主导地位。甲烷营养细菌在深度成熟湖泊中的活性导致湖水中溶解的甲烷浓度从0.8–4.1下降 µmol CH4 L−1至0.4 µmol CH4 L−1,而在浅层热岩溶湖泊中,甲烷营养物的地球化学效应则不那么明显。因此,在温暖的夏季,只有小而浅的亚马尔湖可能对水面的整体扩散性甲烷排放有很大贡献。然而,亚马尔岛上大型深湖的水柱起着微生物过滤器的作用,防止甲烷排放到大气中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信
小红书