收稿日期: 1997-04-28
修回日期: 1997-09-15
网络出版日期: 1998-04-01
基金资助
国家自然科学基金项目“桂林20万年石笋高分辨率古环境重建”( 项目编号: 49472170) 和地矿部岩溶动力学开放研究实验室资助。
A SURVEY OF RESEARCHES ON PALEOCLIMATIC CHANGE UP TO 200 000 A BP IN CHINA AND SOME SUGGESTIONS
Received date: 1997-04-28
Revised date: 1997-09-15
Online published: 1998-04-01
李彬，袁道先 . 中国近20万年以来古气候研究概况及其发展方向[J]. 地球科学进展, 1998 , 13(2) : 192 -197 . DOI: 10.11867/j.issn.1001-8166.1998.02.0192
Global change is one of the key problems that human faces, and the understanding on the past global change, especially on the paleoclimatic change up to 200 000 a BP, is the key to forecasting future climatic change. Based on the studies on the loess, the lake deposits, the ice cores, the marine sediments and the cave sediments, some important results have been got in China. But there are still so medeficiency, i. e. low resolution records, lack of systematical information in some areas and comprehensive mechanism studies etc. Considering these deficiency and the special regional superiority in China, we should give more effective studies on some important areas and periods in order to understand further the influence of the uplift of Qinghai-Xizang plateau on the East Asia's climate, the evolution of the East Asia monsoon and so on.
Key words： Paleoclimate study; Sediment; Ice core; China.
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