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土壤微生物权衡生物地球化学循环以获取应对全年气候变化的胁迫耐受性特征。

Soil Microbes Trade-Off Biogeochemical Cycling for Stress Tolerance Traits in Response to Year-Round Climate Change.

作者信息

Garcia Maria O, Templer Pamela H, Sorensen Patrick O, Sanders-DeMott Rebecca, Groffman Peter M, Bhatnagar Jennifer M

机构信息

Department of Biology, Boston University, Boston, MA, United States.

Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.

出版信息

Front Microbiol. 2020 May 13;11:616. doi: 10.3389/fmicb.2020.00616. eCollection 2020.

Abstract

Winter air temperatures are rising faster than summer air temperatures in high-latitude forests, increasing the frequency of soil freeze/thaw events in winter. To determine how climate warming and soil freeze/thaw cycles affect soil microbial communities and the ecosystem processes they drive, we leveraged the Climate Change across Seasons Experiment (CCASE) at the Hubbard Brook Experimental Forest in the northeastern United States, where replicate field plots receive one of three climate treatments: warming (+5°C above ambient in the growing season), warming in the growing season + winter freeze/thaw cycles (+5°C above ambient +4 freeze/thaw cycles during winter), and no treatment. Soil samples were taken from plots at six time points throughout the growing season and subjected to amplicon (rDNA) and metagenome sequencing. We found that soil fungal and bacterial community composition were affected by changes in soil temperature, where the taxonomic composition of microbial communities shifted more with the combination of growing-season warming and increased frequency of soil freeze/thaw cycles in winter than with warming alone. Warming increased the relative abundance of brown rot fungi and plant pathogens but decreased that of arbuscular mycorrhizal fungi, all of which recovered under combined growing-season warming and soil freeze/thaw cycles in winter. The abundance of animal parasites increased significantly under combined warming and freeze/thaw cycles. We also found that warming and soil freeze/thaw cycles suppressed bacterial taxa with the genetic potential for carbon (i.e., cellulose) decomposition and soil nitrogen cycling, such as N fixation and the final steps of denitrification. These new soil communities had higher genetic capacity for stress tolerance and lower genetic capacity to grow or reproduce, relative to the communities exposed to warming in the growing season alone. Our observations suggest that initial suppression of biogeochemical cycling with year-round climate change may be linked to the emergence of taxa that trade-off growth for stress tolerance traits.

摘要

在高纬度森林中,冬季气温的上升速度比夏季气温更快,这增加了冬季土壤冻融事件的发生频率。为了确定气候变暖和土壤冻融循环如何影响土壤微生物群落及其驱动的生态系统过程,我们利用了美国东北部哈伯德布鲁克实验森林的跨季节气候变化实验(CCASE),在该实验中,重复的田间地块接受三种气候处理之一:变暖(生长季节比环境温度高5°C)、生长季节变暖+冬季冻融循环(生长季节比环境温度高5°C+冬季4次冻融循环),以及不进行处理。在整个生长季节的六个时间点从地块采集土壤样本,并进行扩增子(rDNA)和宏基因组测序。我们发现土壤真菌和细菌群落组成受土壤温度变化的影响,其中微生物群落的分类组成在生长季节变暖和冬季土壤冻融循环频率增加的共同作用下比仅变暖时变化更大。变暖增加了褐腐真菌和植物病原体的相对丰度,但降低了丛枝菌根真菌的相对丰度,而在生长季节变暖和冬季土壤冻融循环的共同作用下,所有这些真菌的丰度都恢复了。在变暖和冻融循环共同作用下,动物寄生虫的丰度显著增加。我们还发现,变暖和土壤冻融循环抑制了具有碳(即纤维素)分解和土壤氮循环遗传潜力的细菌类群,如固氮和反硝化的最后步骤。相对于仅在生长季节暴露于变暖的群落,这些新的土壤群落具有更高的胁迫耐受性遗传能力和更低的生长或繁殖遗传能力。我们的观察结果表明,全年气候变化对生物地球化学循环的初步抑制可能与以生长换取胁迫耐受性特征的类群的出现有关。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9d75/7238748/af777c075fff/fmicb-11-00616-g001.jpg

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