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冰川融水和季节性变化影响北极沿海和开阔水域固氮生物的群落组成。

Glacial meltwater and seasonality influence community composition of diazotrophs in Arctic coastal and open waters.

机构信息

Department of Biology, University of Copenhagen, Strandpromenaden 5, DK-3000 Helsingør, Denmark.

Department of Biology, Aarhus University, Ny Munkegade 114-116, DK-8000 Aarhus, Denmark.

出版信息

FEMS Microbiol Ecol. 2023 Jul 21;99(8). doi: 10.1093/femsec/fiad067.

Abstract

The Arctic Ocean is particularly affected by climate change with unknown consequences for primary productivity. Diazotrophs-prokaryotes capable of converting atmospheric nitrogen to ammonia-have been detected in the often nitrogen-limited Arctic Ocean but distribution and community composition dynamics are largely unknown. We performed amplicon sequencing of the diazotroph marker gene nifH from glacial rivers, coastal, and open ocean regions and identified regionally distinct Arctic communities. Proteobacterial diazotrophs dominated all seasons, epi- to mesopelagic depths and rivers to open waters and, surprisingly, Cyanobacteria were only sporadically identified in coastal and freshwaters. The upstream environment of glacial rivers influenced diazotroph diversity, and in marine samples putative anaerobic sulphate-reducers showed seasonal succession with highest prevalence in summer to polar night. Betaproteobacteria (Burkholderiales, Nitrosomonadales, and Rhodocyclales) were typically found in rivers and freshwater-influenced waters, and Delta- (Desulfuromonadales, Desulfobacterales, and Desulfovibrionales) and Gammaproteobacteria in marine waters. The identified community composition dynamics, likely driven by runoff, inorganic nutrients, particulate organic carbon, and seasonality, imply diazotrophy a phenotype of ecological relevance with expected responsiveness to ongoing climate change. Our study largely expands baseline knowledge of Arctic diazotrophs-a prerequisite to understand underpinning of nitrogen fixation-and supports nitrogen fixation as a contributor of new nitrogen in the rapidly changing Arctic Ocean.

摘要

北极海洋特别容易受到气候变化的影响,其对初级生产力的影响尚不清楚。固氮生物——能够将大气中的氮转化为氨的原核生物——已经在通常氮限制的北极海洋中被检测到,但它们的分布和群落组成动态在很大程度上是未知的。我们从冰川河流、沿海和开阔海域中进行了固氮生物标志物基因 nifH 的扩增子测序,并鉴定出了具有区域特色的北极群落。变形菌固氮生物在所有季节、从表到中层水深度以及从河流到开阔海域都占据主导地位,令人惊讶的是,蓝细菌仅在沿海和淡水水域中偶有发现。冰川河流的上游环境影响了固氮生物的多样性,在海洋样本中,疑似厌氧硫酸盐还原菌表现出季节性演替,在夏季到极夜期间最为普遍。β变形菌(伯克霍尔德氏菌目、亚硝化单胞菌目和红环菌目)通常在河流和淡水影响的水域中被发现,而δ变形菌(脱硫单胞菌目、脱硫杆菌目和脱硫弧菌目)和γ变形菌在海洋水域中被发现。所鉴定的群落组成动态,可能是由径流、无机养分、颗粒有机碳和季节性驱动的,这意味着固氮作用是一种具有生态相关性的表型,预计对正在发生的气候变化具有响应能力。我们的研究在很大程度上扩展了对北极固氮生物的基线知识——这是理解氮固定基础的前提,并支持固氮作用作为快速变化的北极海洋中新增氮的贡献者。

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