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在研究喀斯特洞穴有光及黑暗环境中的洞穴叠层石及其沉积作用的基础上，总结出喀斯特洞穴叠层石的沉积模式，进一步确立了喀斯特洞穴石灰华沉积物的生物成因观点。
Based on the study of the cavestone and its deposition in the light and dark environment of karst caves, the sedimentary model of the karst cave laminated stone was summarized, and the biological genesis of the travertine sediments in karst cave was further established.