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土壤微生物组对高强度野火的生态和基因组响应:将群落组装与功能潜力联系起来。

Ecological and genomic responses of soil microbiomes to high-severity wildfire: linking community assembly to functional potential.

机构信息

Environmental Systems Graduate Group, University of California, Merced, CA, USA.

Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, USA.

出版信息

ISME J. 2022 Jul;16(7):1853-1863. doi: 10.1038/s41396-022-01232-9. Epub 2022 Apr 16.

DOI:10.1038/s41396-022-01232-9
PMID:35430593
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9213548/
Abstract

Increasing wildfire severity, which is common throughout the western United States, can have deleterious effects on plant regeneration and large impacts on carbon (C) and nitrogen (N) cycling rates. Soil microbes are pivotal in facilitating these elemental cycles, so understanding the impact of increasing fire severity on soil microbial communities is critical. Here, we assess the long-term impact of high-severity fires on the soil microbiome. We find that high-severity wildfires result in a multi-decadal (>25 y) recovery of the soil microbiome mediated by concomitant differences in aboveground vegetation, soil chemistry, and microbial assembly processes. Our results depict a distinct taxonomic and functional successional pattern of increasing selection in post-fire soil microbial communities. Changes in microbiome composition corresponded with changes in microbial functional potential, specifically altered C metabolism and enhanced N cycling potential, which related to rates of potential decomposition and inorganic N availability, respectively. Based on metagenome-assembled genomes, we show that bacterial genomes enriched in our earliest site (4 y since fire) harbor distinct traits such as a robust stress response and a high potential to degrade pyrogenic, polyaromatic C that allow them to thrive in post-fire environments. Taken together, these results provide a biological basis for previously reported process rate measurements and explain the temporal dynamics of post-fire biogeochemistry, which ultimately constrains ecosystem recovery.

摘要

野火严重程度的增加在美国西部很常见,这会对植物再生产生有害影响,并对碳(C)和氮(N)循环速率产生重大影响。土壤微生物在促进这些元素循环中起着关键作用,因此了解增加火灾严重程度对土壤微生物群落的影响至关重要。在这里,我们评估了高强度火灾对土壤微生物组的长期影响。我们发现,高强度野火会导致土壤微生物组在几十年(>25 年)的时间里得到恢复,这是由地上植被、土壤化学和微生物组装过程的同时差异所介导的。我们的结果描绘了一个独特的分类和功能演替模式,即在火后土壤微生物群落中选择的增加。微生物群落组成的变化与微生物功能潜力的变化相对应,特别是改变了 C 代谢和增强了 N 循环潜力,这与潜在分解速率和无机 N 可用性分别相关。基于宏基因组组装基因组,我们表明,在我们最早的地点(火灾后 4 年)富集的细菌基因组具有独特的特征,例如强大的应激反应和高降解热解、多环芳烃 C 的潜力,这使它们能够在火后环境中茁壮成长。总之,这些结果为先前报道的过程速率测量提供了生物学基础,并解释了火后生物地球化学的时间动态,这最终限制了生态系统的恢复。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/46945836698c/41396_2022_1232_Fig7_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/720044002b96/41396_2022_1232_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/9fa872e8ed42/41396_2022_1232_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/46945836698c/41396_2022_1232_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/e22d54f04d17/41396_2022_1232_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/6a7fcf956a03/41396_2022_1232_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/66d2a5c0c327/41396_2022_1232_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/8f1923399a84/41396_2022_1232_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/720044002b96/41396_2022_1232_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/9fa872e8ed42/41396_2022_1232_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c70c/9213548/46945836698c/41396_2022_1232_Fig7_HTML.jpg

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