北极土壤C和N循环与干旱期间微生物的适应有关。

IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Theis Thomsen, Morten Dencker Schostag, Anders Priemé, Jonathan Donhauser
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引用次数: 0

摘要

气候变化增加了干旱事件的频率和强度,但干旱条件下微生物介导的土壤碳(C)和氮(N)循环机制尚不清楚。我们对格陵兰岛的土壤进行了一个微观实验,该土壤遭受了五个级别的干旱,在3周的时间内将含水量从180%减少到15%,然后再湿润,模拟自然干旱事件。我们将与胁迫反应和碳氮循环相关的微生物基因表达变化与温室气体(GHG)排放、胞外酶活性和土壤碳氮状态联系起来。基因表达的最大变化发生在中等干旱水平(80%含水量),其特征是微生物生理对干旱条件的适应,包括渗透物的产生以及细胞壁和膜的修饰。这种基因表达变化的高峰标志着一个临界点,与更强烈干旱条件下微生物呼吸和细胞外酶活性的显著下降有关。有趣的是,c -循环基因表达与土壤溶解有机氮(DON)、NH4 +、NO3 -和PO4 -含量相关。此外,氮循环基因的表达与po43 -含量和漆酶活性相关。这些发现强调了干旱条件下微生物碳、氮和磷循环之间的联系,因为化学计量学的限制。再润湿24小时后,我们发现微生物C利用基因的表达转向更不稳定的化合物,合成代谢活性和信号相关基因的表达增加,但没有胁迫响应的特征,这表明微生物群落已经克服了再润湿诱导的渗透压变化,并将代谢活性分配给生长。综上所述,与C:N:P化学计量学相关的微生物生理干旱响应和微生物资源利用是北极土壤在干燥和再湿润条件下C和N循环的关键机制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Arctic Soil C and N Cycling Are Linked With Microbial Adaptations During Drought

Arctic Soil C and N Cycling Are Linked With Microbial Adaptations During Drought

Arctic Soil C and N Cycling Are Linked With Microbial Adaptations During Drought

Climate change increases the frequency and intensity of drought events, yet the mechanisms of microbe-mediated soil carbon (C) and nitrogen (N) cycling under drought are poorly understood. We conducted a microcosm experiment with a Greenlandic soil subjected to five levels of drought, reducing water content from 180% to 15% over the course of 3 weeks followed by rewetting, mimicking a natural drought event. We linked changes in microbial gene expression related to stress response as well as C and N cycling with greenhouse gas (GHG) emissions, extracellular enzyme activities, and soil C and N status. Maximum changes in gene expression occurred at intermediate levels of drought (80% water content), characterized by acclimation of microbial physiology to drought conditions, including production of osmolytes as well as cell wall and membrane modifications. This peak in gene expression changes marked a tipping point associated with a pronounced decline in microbial respiration as well as extracellular enzyme activities under more intense drought conditions. Interestingly, C-cycling gene expression correlated with soil dissolved organic nitrogen (DON), NH4+, NO3 and PO43− contents. Moreover, N-cycling gene expression correlated with PO43− contents and with the activity of laccases. These findings highlight linkages between microbial C, N, and P cycling because of stoichiometric constraints under drought. 24 h after rewetting, we found a shift in microbial expression of C usage genes towards more labile compounds, and an increase in genes related to anabolic activity and signaling, but no signatures of stress responses, suggesting that the microbial community had overcome rewetting-induced changes in osmotic pressure and allocated metabolic activity to growth. Overall, we show that microbial physiological drought responses and microbial resource usage related to C:N:P stoichiometry are key mechanisms of C and N cycling in the Arctic soil under drying and rewetting.

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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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