地球科学进展 ›› 1995, Vol. 10 ›› Issue (2): 136 -142. doi: 10.11867/j.issn.1001-8166.1995.02.0136

干旱气候变化与可持续发展 上一篇    下一篇

国际第四纪地质学研究进展
周卫建,薛样煦   
  1. 中国科学院西安黄土与第四纪地质研究室  西安  710061
  • 收稿日期:1994-06-06 出版日期:1995-04-01
  • 通讯作者: 周卫建

DEVELOPMENTS IN STUDIES OF INTERNATIONAL QUATERNARY GEOLOGY

Zhou Weijian, Xue Xiangxi   

  1. Xi'an Laboratory of Loess and Quaternary Geology, Academia Sinica, Xi'an  710061
  • Received:1994-06-06 Online:1995-04-01 Published:1995-04-01

与人类环境关系密切的第四纪地质学在“过去的全球变化”研究中取得了一系列重要进展,主要体现在对末次冰期旋回的高分辨率环境信息的提取、高精度分析方法的建立、气候不稳定性的发现与研究以及穿越赤道的南北半球对比研究的开始等。

    This paper is to highlight a series of important developments in the study of "Past Global Change" in the recent years. The developments include:(1)extraction of high resolution environmental information for last glacial cycle;(2)establishment of high precision analytical methods;(3)suggestion of concepts of climatic instability and etc. (4)the start of comparison study of Northern and Southern hemispheres crossing the equator.
    Through the studies of ice cores such as GRIP, GISP2 and Vostok, deep sea cores, loess and vein calcite of Devils Hole, the historic picture of climatic instability can be reconstructed. On the background of glacial-interglacial cycle that is driven by orbital foring, the large amplitudes and high rates of temperature shifts reflects that climatic system is operated by more than one switch. Furthermore, some hypotheses such as climatic frequent oscillation caused by internal non-linear feedback of atmosphere-ice sheet-ocean system, climatic instability and asymmetric aperiodic change have been proposed.

[1] Faure H,Morner N-A,刘东生.INQUA对全球变化研究的贡献:研究现状.第四纪研究,1992,2:136-137.
[2] GRIP Member. Climate instability during the last interglacial period recorded in the GRIP ice core. Nature,1993,364:203-207.
[3] Dansgaard W et al. Evidence for general instabilty of past climate from a 250 ka ice-core record. Nature,1993,364:218-220.
[4] Taylor K C et al. The flickering switch of Late Pleistocene climate change. Nature,1993,361:432-436.
[5] Alley R B et al. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event.Nature,1993,362:527.
[6] Kerr Richard A. How ice age climate got the shakes. Nature,1993,260:527.
[7] Jouzel J et al. Exteeding the Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature,1993,364:407-412.
[8] Jouzel J et al. Vostok ice core: acontinuous isotope temperature record over the last climate cycle(160000 yrs). Nature,1987,329:403-413.
[9] Barnola J M et al. Vostok ice core provides 160000 year record of atmospheric CO2. Nature,1987,392:408-413.
[10] Genthon C et al. Vostok ice core, climate response to CO2 and orbital forcing changes over the last climatic cycle. Nature,1987,329:414-418.
[11] Isaac J winograd et al. Continuous 500000 year climate record from vein calcite in Devils Hole, Nevada. Science, 1992,258:255-260.
[12] Deck J Warren. Sea-surface temperature from coral skeletal strontium/calcium ratios.Science,1992,257:644-646.
[13] Mcintyre A and Cline R. Seasonal reconstructiona of the Earth's surface at the last glacial maximum. Geol Soc Am Map chart.Ser. 36,1981.
[14] Kukla G and Cilek V. Pio-Pleistocene megacycles, record of climate and tectonice. in press, 1994.

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