Middle Jurassic Sporopollen Assemblage from the Yan an Formation in Binxian County, Shaanxi Province and Its Significance;

Discovery of Paleogene sporopollen in the Shexing Formation in Doilungdêgên County, northern Lhasa, and its geological significance;

Late Quaternary sporopollen records ad rapid climatic fluctuation events in the Yinchuan basin;

This study focuses on the palynology and sequence stratigraphy of the Paleogene successions in the Jiyang Depression.

The paleoclimatic change since the last glaciation in the north of Okinawa Trough based on the spore-pollen records;

The abrupt changes in spore-pollen species and in the content of reduction sulfur are sensitive to water depth, and can be used as indicators for sequence boundaries and system tracts.

he 19 principal species of spore-pollen taken from peat section of Nianbaoyeze in Heng Duan Mountain are analysed and a cluster analysis is made with 25 samples by using corresponding analysis and selecting 5 principal factors.

Records for pollen and charcoal from Qujialing archaeological site of Hubei and ancient civilization development

Holocene palaeoenvironment changes recorded by pollen of Baahar Nuur Lake

Biomisation, an effective method of quantitatively reconstructing palaeovegetation, can trans-late pollen records into biome assignments based on defining biome types in terms of characteristic plant functional types and using a standard numerical method to calculate the affinity scores of pollen spectra.

Studies on the relationship between sporo-pollen of submarine surface sediments and vegetation around Hainan island;

Research Advances of Quaternary Sporo-pollen in Tibet

According to the composite analysis of mass susceptibility,sporo-pollen in the XH1 core in northern Jiangsu basin and dating result of14C,the paleomagnetism suggests that paleoclimate changes can be distinguished into five stages distinctly: in depth of 25-16.