|
汪品先、阂秋宝、卞云华等,十三万年来南海北部陆坡的浮游有孔虫及其古海洋学意义,地质学报,60 (1986),3:215-225.
|
|
杨怀仁、徐馨,中国东部第四纪自然环境的演变,南京大学学报(自然科学版),1980, 1:121-144.
|
|
杨达源,晚更新世冰期最盛时长江中下游地区的古环境,地理学报,41 (1986),4:302-310.
|
|
业治铮、张明书等,西沙石岛风成石灰岩和化石土壤的发现及其意义,海洋地质与第四纪地质,(1984)1:1-10.
|
|
Shackleton. N.J. and N.D. Opdyke, Oxygen isotope and palaeomagnetic stratigraphy of Equatorial pacific core V28-239, Late Pliocene to Latest Pleistocene, Mem.Geol. Soc. Am.,145(1976),449-464.
|
|
Emiliani, C.,Palaeotemperature analysis of Caribbean cores P6304-8 and P6304-9 and a generalized temperature curve for the 425000 years, Tournal of Geology,74 (1366),109-124.
|
|
Reiss, Z, et al.,Late Q uaternary palaenceanography of the Gulf of Aqaba (Elat) Red Sea, Quaternary Res.,11 (1980),294-308.
|
|
Thompson, P.R.,A.W.A.Be, et al.,Disappearance of pink-pig mented Globigerinodes ruber at 120000 yr,B.P, in the Indian and Pacific Oceans, Nature, 280 (1979),554-558.
|
|
Kukla. G. T.,Pleistocene land-sea correlations. 1. Europe. Earth-Science Renews, 13 (1977),307-374.
|
|
Hays, J. D.,J.Imbrie and N.J,Shackleton, Variations is the earth's orbit; Paemaker of the Ice Ages, Science, 194 (1976),1121-1132.
|
|
Wright, H. E. Jr.,Sensitivity and pesponse time of natural systems to climatic change in the Quatenary, Quater, Science Revives, 3 (1984),91-131.
|
|
Ruddiman, W. F. and A. McIntyre, Oceanic mechanisms for amplification of the 23 000-year ice-volume cycle, Science, 212 (1981),617-627.
|
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