Friis-Christensen E,Lassen K,1991.Length of the solar cycle:an indicator of solar activity closely associated w ith climate.Science,254:698~700
[15]
Tsukada M, 1983.Vegetation and Climate during the Last Glacial Maximum in Japan.Quaternary Research, 19:212~235
[16]
Huang Maohuan, Li Jun, Xie Zichu et al, 1990 Studies on the BHQ ice core from the Law Dome, Antarctica Artarctica Research, 2(1):20~26
[17]
Chen Haowen, Zhu Mingyuan, Yuan Junfeng,1998. Estimation of concentration of heterotrophic bacteria in surface water of Great Wall Bay and its adjacent waters,Antarctica and preliminary analysis of some relevant factors (this Volume)
[18]
Wang Pinxian, Sun Xiangjun, 1994.Last Glacial Maximum in China: Comparison between Land and Sea.Catena 23(1994)341~353
Campo E V, Gasse F, 1993.Pollen-and Diatom-inferred Climatic and hydrological Changes in Sumxi Co basin(Western Tibet)since 13 000 Yr B.P.Quaternary Research, 39:300~313
[28]
姚檀栋, J R Petit, 1992.南极冰盖边缘- 冰芯冰晶测量及其气候意义 冰川冻土, 14(1):11~18
[29]
Chen Haowen,Zhu Mingyuan, Hong Xuguang et al.,1998. Primary analysis on concentration and distribution of chlorophylla in surface water of Great Wall Bay and its adjacent area during austral summer 1993/1994 Cthis Volume)
[30]
Jarvis D I, 1993.Pollen evidence of changing Holocene monsoon climate is Sichuan Province, China.Quaternary Research, 39:325~337
[31]
Ehhalt D H,Roh rer F,Wah ner A,1992.Sources and distribution of NOxin the upper troposphere at northern mid-latitudes.Journal of Geophysical Research,97(D4):3 725~3 738
[32]
Tsukada M, 1980.The History of Japanese Cedar:The Last 15 000 years.Kagaku(Science), Iwanami Sboten, Tokyo 50:538~546
[33]
Drewry D J, 1982 Measured properties of the Antarctic ice sheet:Surface configuration, ice thickness, volume and bedrock characteristics Annual of Glaciology, 3:83~91
