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苔藓植物岩溶作用研究进展
蒙文萍1,2,戴全厚1,*(),冉景丞3
A review on the process of bryophyte karstification
MENG Wen-Ping1,2,DAI Quan-Hou1,*(),RAN Jing-Cheng3

图3. 苔藓植物岩溶作用与环境、岩石间的三向循环互作机制图。苔藓、环境因子、岩石在岩溶作用过程中三者既相互促进又相互制约。环境因子与岩石通过控制苔藓植物的群落特征、形态、生理过程、基因等影响岩溶过程。反之基岩的岩性、组成、产状, 以及苔藓植物对岩面生境(温度、湿度、光照、土壤肥力、微生物)的改善与岩溶速率密切相关。

Fig. 3. The three-way circulation interaction mechanism among bryophyte karstification, environment and rock. Bryophyte, environmental factors and rock in the karstification process promote and restraint each other. Environmental factors and rock affect karstification process and efficiency by controlling the community characteristics, morphology, physiological processes, genes, etc. of bryophyte. The lithology, composition, occurrence of rock, and the improvement of bryophyte on rock surface habitat (temperature, humidity, light, soil fertility, microbes) are closely related to the rate of karstification.