作者简介:沈有信(1966-),男,云南宜良人,研究员,主要从事喀斯特生态学与植被恢复研究工作.E-mail:yxshen@xtbg.ac.cn
收稿日期: 2017-11-07
修回日期: 2018-03-20
网络出版日期: 2018-05-24
基金资助
*国家重点研发计划项目“断陷盆地山地土壤流失过程与驱动机制”(编号:2016YFC0502503);国家自然科学基金项目“喀斯特生态系统裸露岩体集水径流及其生态水文效应研究”(编号:41671031)资助.
版权
Rock Outcrop and Its Ecological Function in Terrestrial Ecosystem
Received date: 2017-11-07
Revised date: 2018-03-20
Online published: 2018-05-24
Supported by
Project supported by the National Key Research and Development Program of China “Process and driving mechanism of soil and water erosion on karst fault basin”(No.2016YFC0502503);The National Natural Science Foundation of China “Water receiving and runoff of rock outcrops and their eco-hydrology effects at karst ecosystems”(No.41671031).
Copyright
沈有信 , 赵志猛 , 毕胜春 , 赵高卷 , 刘娟 . 陆地系统中的露石及其生态作用[J]. 地球科学进展, 2018 , 33(4) : 343 -349 . DOI: 10.11867/j.issn.1001-8166.2018.04.0343
Rock Outcrop (ROC) is very common in terrestrial ecosystems, typically in karst. ROCs play both positive and negative effects in ecosystems. They may collect precipitation (including throughfall), wet/dry deposition, host bacteria, fungi, muss and lichen, and even vascular plants. Both plants and their growing matrixes on ROCs differ greatly from their nearby soil patches. Water and organic and inorganic materials received and produced on ROCs is easily redistributed to their nearby soil patches, put strong influence on water and elements process in soil patches, and thus, affect the plants growing on soil surface. However, quantitative study on water and materials received and produced is scarce, nor on the eco-hydrology effect, thus, blocking the explanation of karst ecosystem succession, block the strategy formulation on countermeasures of karst desertification.
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