Compostion of Carbon Isotopes in Soil Carbonates and Paleoclimate Recoreds of The Late Holocene in the West of Jilin,China;

Evolutional characteristics and their paleoclimate significance of elements in the Qianjiang formation, Qianjiang depression;

Numerical modeling in paleoclimate study:Progress and problems;

We have researched the forming condition of gas hydrate in the South China Sea according to the physical oceanography,palaeo-climate,sedimentary environment,and tectonic environment.

Distribution patterns of phytolith percentage,warmth index and grass cover index demonstrate that there occur 3 assemblage zones in response to palaeo-vegetation and palaeo-climate changes in mid-late Pleistocene,respectively.

Effect of palaeoclimate change at the late Cretaceous period on lithologic sequences in Songliao basin;

Palynological Assemblages of Pleistocence from Shanghai Region and Its Palaeovegetation and Palaeoclimate;

A δ~(13)C record of the organic matter in lacustrine sediments of the core ZHJfrom Lake Caohai and its palaeoclimate implications;

Predicting Paleo-climate Since 140 Ma B.P. by Experiment of Carbon Isotope in Loess;

Using the function, paleo-climate parameters of Yunshu peat profile were calculated and the paleo-climate evolution is then divided into 7 stages: warm-cold-warm-clod-warm-cold-warm.

The authors introduce and summarize some important progress made in paleo-vegetation and paleo-climate researches,especially the recognition of biological origin,reconstruction of paleo-vegetation, paleo-temperature and climatic change.

Ancient climate characteristics in different periods have been reconstructed by means of forest ecology environment reflected by these changes.

By means of the comprehensive study of the petrified wood,other plant fossils and rock groups,some principal characteristics of the ancient climate in SE China are .

there is important information of ancient climate and geography environment in prehistoric myth.