The interim of Late Pleistocene and Holocene is a very important epoch,but the research of the climate change in this period is not well reported.

Characteristics of Palynological Assemblage of Late Stage of Late Pleistocene in Changjiang River Delta Area and Paleoenvironment;

The Sporopollen Assemblages and Their Paleoenvironment Significance of the Qianhu Bay,Zhangpu,Fujian since Late Pleistocene;

The distribution of elephant fossils and the physiognomy characters of late Pleistocene in Jixian County of Tianjin;

Syn-depositional Deformation Structures by Earthquake Related to Volcanic Activity of the Late Pleistocene in Weizhou Island, Beihai City, Guangxi;

Deposit Characteristic and Developed Law of Debris Flow During the Late Pleistocene in Xiaojiang Valley;

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.

Late Pleistocene epoch lake facies sedimentary characteristics, paleoplant-cover and definition of climate transformation since 17.4 ka B.P.Tanggula area, Qinghai;

late Pleistocene Epoch, early-middle Holocene Epoch and late Holocene Epoch.

It is considers that the activitie caused by tensile force at those faults such as Guangzhou-Conghua,Qingquanjie,Shougouling and Wenchong since Late Pleistocene Epoch,but the activity is weak relatively and without serious harms to engineering.