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作 者:LIAN Bin YUAN DaoXian LIU ZaiHua
机构地区:[1]State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China [2] Institute of Karst Geology, Chinese Academy of Geological Sciences, Karst Dynamic Laboratory, Ministry of Land and Resources, Guilin 541004, China
出 处:《Chinese Science Bulletin》2011年第35期3743-3747,共5页
基 金:supported by the Ministry of Science and Technology of China (2006CB403200);the National Natural Science Foundation of China (40773069);the National Science Fund for Creative Research Groups (40721002 and 41021062)
摘 要:The role of microbes in the karstification process was determined based on the karst dynamics,CO2 capture,and carbonate deposition.A close relationship was found among microbial activity,karst dynamics and stability,and the carbon cycle in a karst ecosystem.More in-depth studies were needed to investigate the impact of microbes on karst dynamics within different eco-envi-ronments under natural conditions to determine the response of biological organisms to a changing environment,as well as the relationship between microbial organisms and the karstification process.The role of microbes in the karstification process was determined based on the karst dynamics, CO2 capture, and carbonate deposition. A close relationship was found among microbial activity, karst dynamics and stability, and the carbon cycle in a karst ecosystem. More in-depth studies were needed to investigate the impact of microbes on karst dynamics within different eco-environments under natural conditions to determine the response of biological organisms to a changing environment, as well as the relationship between microbial organisms and the karstification process.
关 键 词:岩溶生态系统 微生物 岩溶动力学 生态环境 碳酸盐沉积 发育过程 二氧化碳 岩溶作用
分 类 号:P642.25[天文地球—工程地质学]
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