Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, PR China; University of Chinese Academy of Sciences, Beijing 100049, PR China; Faculty of Life Science and Technology, Central South University of Forestry & Technology, Changsha 410004, PR China; National Engineering Laboratory for Applied Technology of Forestry & Ecology in South China, Changsha 410004, PR China.
Faculty of Resources and Environmental Engineering, Anshun University, Anshun 561000, China.
Sci Total Environ. 2024 Jun 1;927:172171. doi: 10.1016/j.scitotenv.2024.172171. Epub 2024 Apr 3.
Rocky desertification is one of the most ecological problems in the karst context. Although extensive research has been conducted to explore how to restore and protect, the responses of soil fungi and archaea to rocky desertification succession remain limited. Here, four grades of rocky desertification in a karst ecosystem were selected, amplicon sequencing analysis was conducted to investigate fungal and archaeal community adaptation in response to rocky desertification succession. Our findings revealed that the diversity and community structure of fungi and archaea in soils declined with the aggravation of rocky desertification. As the rocky desertification succession intensified, microbial interactions shifted from cooperation to competition. Microbial survival strategies were K-strategist and r-strategist dominated in the early and late stages of succession, respectively. Additionally, the driving factors affecting microorganisms have shifted from vegetation diversity to soil properties as the intensification of rocky desertification. Collectively, our study highlighted that plant diversity and soil properties play important roles on soil microbiomes in fragile karst ecosystems and that environmental factors induced by human activities might still be the dominant factor exacerbating rocky desertification, which could significantly enrich our understanding of microbial ecology within karst ecosystems.
石漠化是喀斯特地区最主要的生态问题之一。尽管已经开展了广泛的研究来探索如何恢复和保护,但土壤真菌和古菌对石漠化演替的响应仍十分有限。本研究选取了喀斯特生态系统中的四个不同等级的石漠化程度,通过扩增子测序分析来研究真菌和古菌群落对石漠化演替的适应。结果表明,土壤中真菌和古菌的多样性和群落结构随石漠化的加剧而降低。随着石漠化演替的加剧,微生物间的相互作用由合作转向竞争。在演替的早期和晚期,微生物的生存策略分别以 K 策略者和 r 策略者为主。此外,随着石漠化的加剧,影响微生物的驱动因素已经从植被多样性转变为土壤性质。总的来说,本研究强调了植物多样性和土壤性质对脆弱喀斯特生态系统土壤微生物组的重要作用,并且人类活动引起的环境因素可能仍然是加剧石漠化的主导因素,这可以极大地丰富我们对喀斯特生态系统中微生物生态学的理解。