研究论文

走向地球系统科学的必由之路

  • 汪品先
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  • 同济大学海洋地质教育部重点实验室,上海 200092
汪品先(1936-),男,江苏苏州人,教授,中国科学院院士,主要从事海洋微体古生物及古环境研究.E-mail:pxwang@online.sh.cn

收稿日期: 2003-06-23

  网络出版日期: 2003-10-01

本文引用格式

汪品先 . 走向地球系统科学的必由之路[J]. 地球科学进展, 2003 , 18(5) : 795 -796 . DOI: 10.11867/j.issn.1001-8166.2003.05.0795

参考文献

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[2] Dickens G R, O'Neil J R, Rea D K, et al. Dissociation on oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene[J]. Paleoceanography, 1995, 10:965-971. 

[3] Thorseth I H, Torsvik T, Torsvik V, et al. Diversity of life in ocean floor basalt [J]. Earth and Planetary Science Letters, 2001,194:31-37.

[4] Stanley S M, Hardie L A. Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1998, 144: 3-19.

[5] Hart M B, Hylton M D, Oxford M J, et al. The search for the origin of the planktic foraminifera [J]. Journal of the Geological Society, London, 2003, 160:341-343.

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