Chin J Plant Ecol ›› 2019, Vol. 43 ›› Issue (5): 396-407.DOI: 10.17521/cjpe.2019.0020
• Reviews • Previous Articles Next Articles
MENG Wen-Ping1,2,DAI Quan-Hou1,*(),RAN Jing-Cheng3
Received:
2019-09-22
Accepted:
2019-05-06
Online:
2019-05-20
Published:
2019-10-18
Contact:
DAI Quan-Hou
Supported by:
MENG Wen-Ping, DAI Quan-Hou, RAN Jing-Cheng. A review on the process of bryophyte karstification[J]. Chin J Plant Ecol, 2019, 43(5): 396-407.
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URL: https://www.plant-ecology.com/EN/10.17521/cjpe.2019.0020
Fig. 1 Bryophytes on rock surface at Puding karst ecological monitoring station in Guizhou. A, mosses of Ptychomitriaceae gardenri and Hyophila acutifolia. B, mosses of Plagiobryum zierii, Bryum anagustirete and Anomodon rugelii.
Fig. 2 A schematic flowchart showing the bryophyte karstification process. The moss on rock surface through physical and biochemical action to destroy and corrosion the rock, change the rock surface morphology and form the karst microtopography. At the same time, the dissolution products are deposited to form the original soil.
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.
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