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给深海沉积以生命的人——纪念中国黄土研究的挚友Nicholas John Shackleton爵士 被引量:1

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作者 刘东生
出处 《第四纪研究》 CAS CSCD 北大核心 2006年第4期497-498,共2页 Quaternary Sciences
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  • 1丁仲礼.2013.固体地球科学研究中的思维方法浅析--以米兰科维奇理论为例.见:丁仲礼,主编.固体地球科学研究方法.北京:科学出版社.13-34.
  • 2Ding Z L, Yu Z, Rutter N W, Liu T. 1994. Towards an orbital time scale for Chinese loess deposits. Quat Sci Rev, 13:39-70.
  • 3Duplessy J C, Shackleton N J. 1985. Response of global deep-water circulation to the Earth's climatic change 135000-107000 years ago, Natur] I 316:500-507.
  • 4Emiliani C. 1955. Pleistocene temperatures. J Geol, 63:538-578.
  • 5Emiliani C, Shackleton N J. 1974. The Brunhes epoch: Isotopic paleotemperatures and geochronology. Science, 183:511-514.
  • 6Guo Z T, Berger A, Yin Q Z, Qin L. 2009. Strong asymmetry of hemispheric climates during MIS-13 inferred from correlating China loess and Antarctica ice records. Clim Past, 5:21-31.
  • 7Hays J D. 2006. Nick Shackleton. Quat Sci Rev, 25:3090-3091.
  • 8Hays J D, Imbrie J, Shackleton N J. 1976. Variations in the Earth's orbit: Pacemaker of the Ice Ages. Science, 194:1121-1132.
  • 9Imbrie J, Hays J D, Martinson D G, Mclntyre A, Mix A C, Morley J J, Pisias N G, Prell W L, Shackleton N J. 1984. The orbital theory ot Pleistocene climate: Support from a revised chronology of the marine 80 record. In: Berger A, ed. Milankovitch and Climate, Part 1. New York: Springer. 269-305.
  • 10Kennett J P, Shackleton N J. 1976. Oxygen isotopic evidence for the development of the psychrosphere 38 Myr ago. Nature, 260:513-515.

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