Changbai Mountain, Northeast China is a very sensitive area to global climate change, and the information of its peat land is significant to reconstruct the middle and late Holocene climatic change. Phytolith provides an effective way to research environmental change in Quaternary, because many plants have high production of phytoliths in same time and phytolith is not easily moved. This paper focused on the phytolith character of the Hushan peat profile and discussed the environmental implications of its phytolith assemblages. The result showed that the phytolith and pollen information has obvious consistency, this illustrated that phytolith information is as useful as pollen and phytolith is an effective proxy index to reconstruct the paleoenvironment.