Martinson D G;Pisias N G;Hays J D;Imbrie J, Moore T C, Shackleton N J,Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy,Quaternary Research,1987.
[2]
Stuiver, M;P M Grootes;T F Braziunas,The GISP2 18O climate record of the past 16,500 years and the role of the sun, ocean and volcanoes,Quaternary Research,1995.
[3]
Bond G;Heinrich H;Broecker W,Evidence for massive discharges of icebergs into the south Atlantic ocean during the last galcial period,Nature,1992.
[4]
LI Bin ；YUAN Daoxian ；QIN Jiaming,Oxygen and carbon isotopic characteristics of rainwater, drip water and present speleothems in a cave in Guilin area, and their environmental meanings,Science in China. Series D, Earth sciences？,2000, 43(3).
[5]
Li B;Yuan DX,The Younger Dryas Event and Holocene climate Fluctuations recorded in a stalagmite from Panlong Cave of Guilin, China,Acta Geologica Sinica,1998(04).
[6]
Linsley B K;Thunell R C,The record of Deglaciation in the Sulu sea: Evidence for the Younger Dryas event in the tropical western Pacific,Paleoceanography,1990.
Meese D A;R B Alley;R J Fiacco;M S Germani, A J Gow, P M Grootes, M Illing, P A Mayewski, M C Morrison, M Ram, K C Taylor, Q Yang G A Zielinski,Preliminary depth-agescale of the GISP2 ice core,Special CRREL Report,1994.
[9]
LINSLEY B K,Oxygen-isotope record of sea level and climate variations in Sulu sea over past 150 000 years,Nature？ ,1996, 380.
