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陆地输入塑造了北极高纬度峡湾(斯瓦尔巴群岛伊士峡湾)中的沿海细菌和古菌群落。

Terrestrial Inputs Shape Coastal Bacterial and Archaeal Communities in a High Arctic Fjord (Isfjorden, Svalbard).

作者信息

Delpech Lisa-Marie, Vonnahme Tobias R, McGovern Maeve, Gradinger Rolf, Præbel Kim, Poste Amanda E

机构信息

Department of Biology, École Normale Supérieure de Lyon, Université de Lyon, Lyon, France.

Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway.

出版信息

Front Microbiol. 2021 Feb 26;12:614634. doi: 10.3389/fmicb.2021.614634. eCollection 2021.

Abstract

The Arctic is experiencing dramatic changes including increases in precipitation, glacial melt, and permafrost thaw, resulting in increasing freshwater runoff to coastal waters. During the melt season, terrestrial runoff delivers carbon- and nutrient-rich freshwater to Arctic coastal waters, with unknown consequences for the microbial communities that play a key role in determining the cycling and fate of terrestrial matter at the land-ocean interface. To determine the impacts of runoff on coastal microbial (bacteria and archaea) communities, we investigated changes in pelagic microbial community structure between the early (June) and late (August) melt season in 2018 in the Isfjorden system (Svalbard). Amplicon sequences of the 16S rRNA gene were generated from water column, river and sediment samples collected in Isfjorden along fjord transects from shallow river estuaries and glacier fronts to the outer fjord. Community shifts were investigated in relation to environmental gradients, and compared to river and marine sediment microbial communities. We identified strong temporal and spatial reorganizations in the structure and composition of microbial communities during the summer months in relation to environmental conditions. Microbial diversity patterns highlighted a reorganization from rich communities in June toward more even and less rich communities in August. In June, waters enriched in dissolved organic carbon (DOC) provided a niche for copiotrophic taxa including and . In August, lower DOC concentrations and Atlantic water inflow coincided with a shift toward more cosmopolitan taxa usually associated with summer stratified periods (e.g., SAR11 Clade Ia), and prevalent oligotrophic marine clades (OM60, SAR92). Higher riverine inputs of dissolved inorganic nutrients and suspended particulate matter also contributed to spatial reorganizations of communities in August. Sentinel taxa of this late summer fjord environment included taxa from the class Verrucomicrobiae (, ), potentially indicative of a higher fraction of particle-attached bacteria. This study highlights the ecological relevance of terrestrial runoff for Arctic coastal microbial communities and how its impacts on biogeochemical conditions may make these communities susceptible to climate change.

摘要

北极正在经历巨大变化,包括降水量增加、冰川融化和永久冻土解冻,导致流入沿海水域的淡水径流增加。在融化季节,陆地径流将富含碳和养分的淡水输送到北极沿海水域,这对在陆地-海洋界面决定陆地物质循环和归宿方面起关键作用的微生物群落产生了未知影响。为了确定径流对沿海微生物(细菌和古菌)群落的影响,我们调查了2018年伊士峡湾系统(斯瓦尔巴群岛)融化季节早期(6月)和晚期(8月)浮游微生物群落结构的变化。16S rRNA基因的扩增子序列是从伊士峡湾沿峡湾断面采集的水柱、河流和沉积物样本中生成的,这些断面从浅河河口和冰川前沿延伸至外峡湾。研究了群落变化与环境梯度的关系,并与河流和海洋沉积物微生物群落进行了比较。我们发现,在夏季,微生物群落的结构和组成与环境条件相关,发生了强烈的时空重组。微生物多样性模式突出显示,从6月丰富的群落向8月更均匀、丰富度更低的群落进行了重组。6月,富含溶解有机碳(DOC)的水域为包括 和 在内的富营养类群提供了生态位。8月,较低的DOC浓度和大西洋水流入与向通常与夏季分层期相关的更多世界性类群(如SAR11进化枝Ia)以及普遍存在的贫营养海洋类群(OM60、SAR92)的转变同时发生。8月,河流中溶解无机养分和悬浮颗粒物的输入增加也导致了群落的空间重组。这个夏末峡湾环境的哨兵类群包括疣微菌纲( 、 )的类群,这可能表明附着在颗粒上的细菌比例更高。这项研究突出了陆地径流对北极沿海微生物群落的生态相关性,以及其对生物地球化学条件的影响如何使这些群落易受气候变化的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9c23/7952621/5d36507b9eb7/fmicb-12-614634-g001.jpg

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