Shrubification of herbaceous peatlands modulates root exudates, increasing rhizosphere soil CO2 emissions while decreasing CH4 emissions

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Catena Pub Date : 2024-08-09 DOI:10.1016/j.catena.2024.108282
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Abstract

As shrubs continue to expand in peatlands due to climate change, it is critical to examine the mechanisms underlying carbon dioxide (CO2) and methane (CH4) emissions. While the decrease in water levels during shrub encroachment into peatlands is known to increase soil carbon emissions, the role of the genetic potential of microbial metabolic processes mediated by root exudates in affecting rhizosphere soil carbon emissions is less well understood. Here, we conducted in situ field monitoring of shrub and herb peatlands, combined with laboratory incubation experiments involving the addition of root exudates. Using metagenomics and metabolomics technologies, we aimed to elucidate the microbiological mechanisms behind changes in carbon emissions. This study found that the rhizosphere soil under shrubs had a higher CO2 emission rate with greater genetic potential for CO2 production (19.36%), but exhibited a lower CH4 emission rate conferring a lower genetic potential for CH4 production (52.30%) than that under herbs. These differences were attributed to the distinct ways in which the root exudates of shrubs and herbs influence the structure and function of the microbial community, thereby favoring CO2 and CH4 emissions differently. Specifically, the relatively higher amounts of sugars and amino acids in shrub root exudates stimulate the genetic potential for cellulose and hemicellulose decomposition, leading to a 13.23% increase in CO2 emissions. In contrast, the relatively higher amounts of lipids in herb root exudates promote the genetic potential for the acetic acid-type methanogenic process, resulting in a 33.50% increase in CH4 emissions. Shrubification increased the genetic potential for labile carbon decomposition while decreasing the genetic potential for chitin and lignin decomposition, possibly promoting recalcitrant carbon conservation in the rhizosphere soil. Altogether, shrubification of herbaceous peatlands increases rhizosphere soil carbon emissions by regulating root exudates. It is recommended that appropriate ecosystem management measures be implemented to control shrub expansion, thereby optimizing carbon emissions from peatlands.

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草本泥炭地的灌木化改变了根部渗出物,增加了根瘤土壤的二氧化碳排放量,同时减少了甲烷排放量
由于气候变化,灌木在泥炭地中不断扩展,因此研究二氧化碳(CO)和甲烷(CH)排放的内在机制至关重要。众所周知,灌木侵占泥炭地过程中水位下降会增加土壤碳排放,但人们对由根部渗出物介导的微生物代谢过程的遗传潜力在影响根圈土壤碳排放方面的作用却不甚了解。在这里,我们对灌木和草本泥炭地进行了现场实地监测,并结合实验室培养实验,添加了根系渗出物。利用元基因组学和代谢组学技术,我们旨在阐明碳排放变化背后的微生物机制。研究发现,与草本植物相比,灌木根圈土壤的二氧化碳排放率较高,产生二氧化碳的遗传潜力较大(19.36%),但二氧化碳排放率较低,产生二氧化碳的遗传潜力较小(52.30%)。这些差异归因于灌木和草本植物根部渗出物影响微生物群落结构和功能的不同方式,从而有利于不同的 CO 和 CH 排放。具体来说,灌木根部渗出物中相对较多的糖和氨基酸会刺激纤维素和半纤维素分解的遗传潜力,从而导致二氧化碳排放量增加 13.23%。相比之下,草本植物根系渗出液中相对较多的脂质促进了乙酸型甲烷生成过程的遗传潜力,导致 CH 排放量增加 33.50%。灌木化增加了可溶性碳分解的遗传潜力,同时降低了甲壳素和木质素分解的遗传潜力,这可能促进了根圈土壤中难降解碳的保存。总之,草本泥炭地的灌木化通过调节根部渗出物增加了根圈土壤的碳排放。建议实施适当的生态系统管理措施,控制灌木扩展,从而优化泥炭地的碳排放。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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