[1] |
钱建兴编著,1990,氧同位素地质学及其原理,海洋出版社,117---120,北京。 |
[2] |
Altenbach,A. V. and Sarnthein,M.1989,Productirity rocord in benthic foraminifera, Productivity of the:present and past (eds. Berger, W. H., Smetacek, V. S. and Wefer, G.),John Wiley&Sons Limited.S.Bernhard, Dahlem Konferenzen,255~269. |
[3] |
Imbrie, J.,Hays, J. D. et al, 1989, The orbital theory of Pleistocene climate; support from a revised chronology of the marine b'00 record,"MilanKovitch and Climate",Part 1(Berger,A. L.,et al eds.),Reidel .The Netherlands,269~305. |
[4] |
Ramsay, A. T. S.,1977.Oceance Miaopalaeontology, Vol. 1,academic press, London, New York, San Francisco, 808. |
[5] |
‘Shackleton, N. J.,M.^.Hall. et al . 1983. Carbca isotope data in core V 19一30 confirm reduced carbon dioxide concentration in the ice age atmosphere, Nature.306,319一322. |
[6] |
Thompson, P. R.,A. W. H. Be等,1976, Disappearence of Pink一pigmented Gldigerimcides rder at 120, 000 Yr BP in the Indian and Pacific Oceans. Nature 280.559~558. |
[7] |
Wang Chung一Ho, Chen Min一pen et al, 1986, Stable isotope records of late Pleislocene sediments from the South China Sea,Bulletin of the Institute of Earth Science, Academia Sinica. 6,185~195. |
[8] |
Wang Chung一Ho and Chen Min一Pen, 1990.Upper Pleistocence oxygen and carbon isotopic changes of core SCS一15B at the South China Sea. Journal of Southeast Asian Earth Science, 9(3),243~246. |
[9] |
Williams,D. F.,1985,Carbon isotope variations in surface waters of Gulf of Mexico on time scale of 10.000.30, 000,150.000 and 2 million years. In:The Carbon Cycle and Atmospheric C02: Natural Variations Archean to Present, Amer. Geophy. Union Geophy. Monograph, 32.329一391. |