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受不同氮沉降影响的两个中欧泥炭地中的微生物群落动态。

Microbial community dynamics in two Central European peatlands affected by different nitrogen depositions.

作者信息

Barta Jiri, Santruckova Hana, Novak Martin, Cejkova Bohuslava, Jackova Ivana, Buzek Frantisek, Stepanova Marketa, Curik Jan, Veselovsky Frantisek, Prechova Eva

机构信息

Department of Ecosystem Biology, University of South Bohemia in České Budejovice, Branisovska 1645a, 370 05 České Budejovice, Czech Republic.

Department of Environmental Geochemistry and Biogeochemistry, Czech Geological Survey, Geologicka 6, 152 00 Prague 5, Czech Republic.

出版信息

FEMS Microbiol Ecol. 2025 Jun 24;101(7). doi: 10.1093/femsec/fiaf056.

Abstract

Changes in organic matter accumulation in wetlands are critical for climate dynamics. Different nitrogen (N) inputs in Sphagnum-dominated peat bogs can lead to varying rates of carbon (C) and N accumulation, influencing greenhouse gas emissions. We investigated how contrasting N deposition shapes microbial communities in two Czech peat bogs, focusing on biological N2 fixation (BNF) as a key N input in pristine wetlands. Higher N deposition resulted in a more active microbial community with increased enzyme activity and C acquisition, potentially accelerating decomposition and reducing C storage. Enhanced denitrification, indicated by active nosZ Clade I genes, suggests that higher N inputs may increase N losses through denitrification. In contrast, the lower N site showed a less active microbial community with slower decomposition, beneficial for C sequestration, though potentially less adaptable to future N increases. Experimental BNF rates were 70 times higher at the high N site, consistent with elevated diazotroph activity indicated by active nifH gene. Phosphorus (P) availability and NH4+/NO3- ratios appeared to drive BNF differences, emphasizing the need for managed N inputs to maintain peatland ecological functions.

摘要

湿地中有机物质积累的变化对气候动态至关重要。在以泥炭藓为主的泥炭沼泽中,不同的氮(N)输入会导致碳(C)和氮积累速率不同,从而影响温室气体排放。我们研究了不同的氮沉降如何塑造捷克两个泥炭沼泽中的微生物群落,重点关注生物固氮(BNF),它是原始湿地中关键的氮输入方式。较高的氮沉降导致微生物群落更活跃,酶活性和碳获取增加,这可能会加速分解并减少碳储存。活跃的I类nosZ基因表明反硝化作用增强,这表明较高的氮输入可能会通过反硝化作用增加氮损失。相比之下,低氮位点的微生物群落活性较低,分解较慢,这有利于碳固存,尽管可能对未来氮增加的适应性较差。高氮位点的实验性生物固氮速率比低氮位点高70倍,这与活跃的nifH基因所表明的固氮菌活性升高一致。磷(P)的有效性和NH4+/NO3-比率似乎驱动了生物固氮的差异,这强调了需要控制氮输入以维持泥炭地生态功能。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e36f/12198764/aa8596bf06d0/fiaf056fig1.jpg

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