摘要
藻类、地衣可以直接殖居在碳酸盐岩表面,通过生物化学、生物物理过程对其基质产生钻孔溶蚀作用,并产生相应特征性的微形态。文中初探了微形态与①岩面的水热条件;②不同地貌部位的微环境;③植被覆盖程度;④不同气候带间存在的相关性。并讨论和展望了生物岩溶微形态研究的前景,开拓生物岩溶研究新思路。
Algae and lichens may directly colonize and live on the surface of carbonate rocks. Through biochemical and physical processes, they bore and corrode the substrate, thus producing distinct biokarst microforms. The development of these microforms, moreover, has close relationship with the mositure and heat on the surface of carbonate rocks, microenvironments of different ge-omorphological positions, the cover-degree of vegetation and even different climate zones. In order to open new ideas about the study of biokarst, the prospects of the study of biokarst microforms are discussed and forecasted.
出处
《地质论评》
CAS
CSCD
北大核心
1998年第6期656-661,共6页
Geological Review
基金
国家自然科学基金(编号49272160和49632100)
地质矿产部岩溶动力学开发研究实验室资助
关键词
藻类
地衣
生物岩溶
溶蚀微形态
内陆环境
岩溶
alga
lichen
biokarst
corrosional microform
terrestrial environment