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参与季风主导和西风主导的西藏冰川之间氮循环的不同基因和微生物群落。

Distinct genes and microbial communities involved in nitrogen cycling between monsoon- and westerlies-dominated Tibetan glaciers.

作者信息

Zhang Zhihao, Liu Yongqin, Zhao Weishu, Liu Keshao, Chen Yuying, Wang Feng, Mao Guannan, Ji Mukan

机构信息

State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China.

Center for the Pan-third Pole Environment, Lanzhou University, Lanzhou, 730000, China.

出版信息

Nat Commun. 2025 Jul 1;16(1):5926. doi: 10.1038/s41467-025-61002-x.

Abstract

The Tibetan Plateau (TP) glaciers are influenced by monsoon and westerlies. They are highly sensitive to climate change, with atmospheric nitrogen deposition significantly impacting microbial communities and functions. However, key uncertainties persist regarding biogeography and drivers of genes and microbial communities involved in nitrogen cycling. Here, we investigate the diversity and transcriptional activity of microbial communities and nitrogen-cycling genes using 85 metagenomes and 28 metatranscriptomes from the ablation zone of 21 TP glaciers. Our results show that over 90% of the glacial taxa possess the potential for nitrogen metabolism, with ~33% exhibiting transcriptional activity. Moreover, monsoon-dominated glaciers present greater microbial diversity and higher prevalence of nitrogen-fixing genes than westerlies-dominated glaciers, linked to higher temperatures. Comparatively, the latter show elevated genomic potential for nitrous oxide emissions, likely due to higher nitrate concentrations. These findings establish temperature-nitrogen co-regulation of microbial nitrogen transformations, critical for predicting climate feedback in the extreme environment.

摘要

青藏高原(TP)的冰川受季风和西风影响。它们对气候变化高度敏感,大气氮沉降对微生物群落和功能有显著影响。然而,在参与氮循环的基因和微生物群落的生物地理学及驱动因素方面,关键的不确定性仍然存在。在此,我们利用来自21条TP冰川消融区的85个宏基因组和28个宏转录组,研究了微生物群落和氮循环基因的多样性及转录活性。我们的结果表明,超过90%的冰川分类群具有氮代谢潜力,约33%表现出转录活性。此外,季风主导的冰川比西风主导的冰川呈现出更大的微生物多样性和更高的固氮基因流行率,这与较高温度有关。相比之下,后者显示出更高的一氧化二氮排放基因组潜力,可能是由于硝酸盐浓度较高。这些发现确立了温度-氮对微生物氮转化的共同调节作用,这对于预测极端环境中的气候反馈至关重要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2b06/12216452/a2ec813253e8/41467_2025_61002_Fig1_HTML.jpg

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