The role of lichens in inhibiting erosion of a soluble rock

被引:40
作者
Mottershead, D
Lucas, G
机构
[1] Liverpool John Moores Univ, Sch Educ Community & Social Sci, Liverpool L3 2ET, Merseyside, England
[2] Edge Hill Coll Higher Educ, Ormskirk L39 4QP, Lancs, England
关键词
D O I
10.1006/lich.2000.0300
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Soluble rocks undergo erosion by solution when rain falls on an unprotected rock surface. Lichens may act to protect the surface from such erosion, and the protected area may subsequently emerge from the surrounding lowering surface to form an area of higher relief. Specimens of Aspicilia calcarea and Diploschistes diacapsis act in this way on a gypsum surface, creating conical or rounded mounds up to 15 mm in height. In the case of Aspicilia, the lichen centre decays, re-exposing to surface solution the central area, which then corrodes to create a cratered gypsum cone. The gradient of the cone side-slopes is a function of the relative rates of lichen radial growth and rock surface lowering. (C) 2000 The British Lichen Society.
引用
收藏
页码:601 / 609
页数:9
相关论文
共 10 条
[1]  
CALAFORRA JM, 1998, KARSTOLOGIA VESOS
[2]  
Fiol L, 1996, EARTH SURF PROCESSES, V21, P447, DOI 10.1002/(SICI)1096-9837(199605)21:5&lt
[3]  
447::AID-ESP607&gt
[4]  
3.0.CO
[5]  
2-X
[6]  
GEIKE A, 1893, TXB GEOLOGY
[7]  
HAIGH MJ, 1981, BRIT GEOMORPHOLOGICA, V29, P31
[8]  
Mottershead D. N., 1981, APPL GEOGR, V1, P297
[9]  
MOTTERSHEAD DN, 1980, TIMESCALES GEOMORPHO, P95
[10]  
VILES H, 1994, BRIT GEOMOR, P99