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Karst rocky desertification refers to the process of land degradation caused by various factors such as climate change and human activities including deforestation and agriculture on a fragile karst substrate. Nutrient limitation is common in karst areas. Moss crust grows widely in karst areas. The microorganisms associated with bryophytes are vital to maintaining ecological functions, including climate regulation and nutrient circulation. The synergistic effect of moss crusts and microorganisms may hold great potential for restoring degraded karst ecosystems. However, our understanding of the responses of microbial communities, especially abundant and rare taxa, to nutrient limitations and acquisition in the presence of moss crusts is limited. Different moss habitats exhibit varying patterns of nutrient availability, which also affect microbial diversity and composition. Therefore, in this study, we investigated three habitats of mosses: autochthonal bryophytes under forest, lithophytic bryophytes under forest and on cliff rock. We measured soil physicochemical properties and enzymatic activities. We conducted high-throughput sequencing and analysis of soil microorganisms. Our finding revealed that autochthonal moss crusts under forest had higher nutrient availability and a higher proportion of copiotrophic microbial communities compared to lithophytic moss crusts under forest or on cliff rock. However, enzyme activities were lower in autochthonal moss crusts under forest. Additionally, rare taxa exhibited distinct structures in all three habitats. Analysis of co-occurrence network showed that rare taxa had a relatively high proportion in the main modules. Furthermore, we found that both abundant and rare taxa were primarily assembled by stochastic processes. Soil properties significantly affected the community assembly of the rare taxa, indirectly affecting microbial diversity and complexity and finally nutrient acquisition. These findings highlight the importance of rare taxa under moss crusts for nutrient acquisition. Addressing this knowledge gap is essential for guiding ongoing ecological restoration projects in karst rocky desertification regions.
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http://dx.doi.org/10.3389/fmicb.2024.1384367 | DOI Listing |
Glob Chang Biol
August 2025
College of Geography and Resources, Sichuan Normal University, Chengdu, China.
The rapid accumulation of bioavailable phosphorus (Bio-P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio-P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier foreland on Gongga Mountain as a natural laboratory, microbial community assembly, co-occurrence networks, and phosphorus cycling genes (PCGs) were examined across four successional stages, from bare land to moss crust.
View Article and Find Full Text PDFYing Yong Sheng Tai Xue Bao
June 2025
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, Shaanxi, China.
The restoration of moss crust (moss-dominated biological soil crust) through artificial cultivation is of great significance for preventing soil wind erosion and desertification in arid and semi-arid regions. However, the tiny size of moss plant and associated observational challenge hindered the establishment of scientifically validated and standardized indicators for assessing the growth and development of artificial moss crusts. We measured moss crust development indicators, including plant density, coverage, and height every five days during a 60-day cultivation experiment, as well as the dry weight and thickness of moss crust after the cultivation.
View Article and Find Full Text PDFLife (Basel)
May 2025
Programa de Pós-Graduação em Biologia Vegetal, Instituto de Ciências Biológicas, Universidade Federal de Minas Gerais, Av. Antônio Carlos, 6627, Pampulha, Belo Horizonte 31270-901, MG, Brazil.
Rocky outcrops are harsh habitats that support specialized organisms and communities, including biocrusts, which play roles in soil stabilization, water retention, and nutrient cycling. Despite their importance, tropical biocrusts, particularly in granite-gneiss formations, remain underexplored. This study examines biocrust composition in a granite-gneiss outcrop in a rural landscape in Southeastern Brazil, identifying microhabitats and analyzing co-occurrence patterns and community structure.
View Article and Find Full Text PDFBiology (Basel)
May 2025
College of Geographical Sciences, Qinghai Normal University, Xining 810008, China.
Desertification, which may lead to land degradation, is a significant global ecological issue. Biological soil crusts (BSCs) can play a role in sand fixation, carbon sequestration, and the improvement in soil functions in the ecological restoration of sandy soil. Therefore, elucidating the responses of BSCs to afforestation measures in alpine sandy areas is necessary to guide vegetation configuration in sandy ecosystems and enhance the effectiveness of sand fixation measures to prevent desertification.
View Article and Find Full Text PDFYing Yong Sheng Tai Xue Bao
January 2025
College of Land Science and Technology, China Agricultural University/Key Laboratory of Arable Land Conservation in North China, Ministry of Agriculture and Rural Affairs, Beijing 100193, China.
The intensification of global climate change may increase temperature and precipitation in drylands. Biocrust is one of the important surface covers in drylands. The responses of soil organic carbon (SOC) fractions and their stability in biocrusts-covered soil to climate warming and wetting remain unclear.
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