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土壤微生物群落调节着盐度胁迫对滨海盐沼中土壤有机碳分解的阈值效应。

Soil microbial communities regulate the threshold effect of salinity stress on SOM decomposition in coastal salt marshes.

作者信息

Zhang Guangliang, Bai Junhong, Jia Jia, Wang Wei, Wang Dawei, Zhao Qingqing, Wang Chen, Chen Guozhu

机构信息

State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China.

Advanced Institute of Natural Sciences, Beijing Normal University, Zhuhai 519087, China.

出版信息

Fundam Res. 2023 Mar 20;3(6):868-879. doi: 10.1016/j.fmre.2023.02.024. eCollection 2023 Nov.

Abstract

Salinity stress is one of the critical environmental drivers of soil organic matter (SOM) decomposition in coastal ecosystems. Although the temperature sensitivity (Q) of SOM decomposition has been widely applied in Earth system models to forecast carbon processes, the impact of salinity on SOM decomposition by restructuring microbial communities remains uncovered. Here, we conducted a microcosm experiment with soils collected from the coastal salt marsh in the Yellow River Estuary, which is subjected to strong dynamics of salinity due to both tidal flooding and drainage. By setting a gradient of salt solutions, soil salinity was adjusted to simulate salinity stress and soil carbon emission (CO) rate was measured over the period. Results showed that as salinity increased, the estimated decomposition constants based on first-order kinetics gradually decreased at different temperatures. Below the 20‰ salinity treatments, which doubled the soil salinity, Q increased with increasing salinity; but higher salinity constrained the temperature-related response of SOM decomposition by inhibiting microbial growth and carbon metabolisms. Soil bacteria were more sensitive to salinity stress than fungi, which can be inferred from the response of microbial beta-diversity to changing salinity. Among them, the phylotypes assigned to and showed higher salt tolerance, whereas taxa affiliated with and were more easily inhibited by the salinity stress. Several fungal taxa belonging to had higher adaptability to the stress. As the substrate was consumed with the incubation, bacterial competition intensified, but the fungal co-occurrence pattern changed weakly during decomposition. Collectively, these findings revealed the threshold effect of salinity on SOM decomposition in coastal salt marshes and emphasized that salt stress plays a key role in carbon sequestration by regulating microbial keystone taxa, metabolisms, and interactions.

摘要

盐度胁迫是沿海生态系统中土壤有机质(SOM)分解的关键环境驱动因素之一。尽管SOM分解的温度敏感性(Q)已在地球系统模型中广泛应用于预测碳过程,但盐度通过重组微生物群落对SOM分解的影响仍未被揭示。在此,我们利用从黄河口沿海盐沼采集的土壤进行了一项微观实验,该地区由于潮汐淹没和排水,盐度动态变化强烈。通过设置盐溶液梯度,调节土壤盐度以模拟盐度胁迫,并在此期间测量土壤碳排放(CO)速率。结果表明,随着盐度增加,基于一级动力学估算的分解常数在不同温度下逐渐降低。在盐度处理低于20‰(使土壤盐度加倍)时,Q随盐度增加而增加;但更高的盐度通过抑制微生物生长和碳代谢限制了SOM分解与温度相关的响应。土壤细菌比真菌对盐度胁迫更敏感,这可以从微生物β多样性对盐度变化的响应中推断出来。其中,归属于 和 的系统发育型表现出较高的耐盐性,而隶属于 和 的分类单元更容易受到盐度胁迫的抑制。属于 的几个真菌分类单元对胁迫具有较高的适应性。随着培养过程中底物的消耗,细菌竞争加剧,但分解过程中真菌的共现模式变化较弱。总体而言,这些发现揭示了盐度对沿海盐沼中SOM分解的阈值效应,并强调盐胁迫通过调节微生物关键分类单元、代谢和相互作用在碳固存中起关键作用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cab7/11197625/06171e7278c8/ga1.jpg

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