The paper on palynology and archaeology reveals the living environment of ancestor and the mutual relationship between human activity and environment change by pollen analysis of Qiguoshan Section in Chifeng Area.

This article disclose the environmental variation since 1 000 years of Sichanghu of the South along Guerbantonggute Desert,which is based on the pollen analysis in the deposition of the area and combined with the analysis of rock character and historical materials.

The pollen analysis of the layers of Qiangtang and Sanchahe groups in a saddle of the Kunlun Mountains shows that a dry environment had been come into in the Early Pleistocene in the Qiangtang Plateau.

Based on the sporo-pollen analysis and ~(14)C sample annual dating on the deposits of Huashuwozi section and Xiaoxigou section in the northern piedmonts of Tianshan Mts.

Based on the sporo-pollen analysis and ￣(14)C dating from Balikun Lake Core ZK024, the sporo-pollen assemblages array surbey in Balikun Basin since the late Pleistocene is drawn out, and six comprehensive sporo-pollen zones are divided.

By spore-pollen analysis and palynological data,the strata can be divided and contrasted,and their geological times can also be determined,so as to reconstruct their paleovegetations and paleosurroundings.

With the wide application of computers,many more numerical techniques can be used in the spore-pollen analysis today.

According to sporopollen analysis and study and reconstruction of ancient vegetations, combined with studies of the geochemical behaviors of paleosol of the Guanghan layer of the Shanxingdui site and hydrodynamic conditions of ancient rivers, the ancient environment of the Jinsha cultural site was studied in an attempt to provide the e.

5 spore pollen zones are divided throngh the spore pollen analysis.