收稿日期: 1997-06-02
修回日期: 1997-10-28
网络出版日期: 1998-06-01
基金资助
国家自然科学基金重大项目“我国干旱半干旱区15万年来环境演变的动态过程与发展趋势”(项目编号:49291100)资助。
THE PROBLEMS AND PROGRESS IN THE STUDIES OF MECHANISMS FOR QUATERNARY CLIMATE CHANGES
Received date: 1997-06-02
Revised date: 1997-10-28
Online published: 1998-06-01
熊尚发，丁仲礼，刘东生 . 第四纪气候变化机制研究的进展与问题[J]. 地球科学进展, 1998 , 13(3) : 265 -272 . DOI: 10.11867/j.issn.1001-8166.1998.03.0265
Since 1950's when Emiliani obtained the first curve of the oxygen isotope records in the deep ocean sediments, the classical glaciation hypothesis developed by Penck had been replaced by the new discoveries which, by the works of Emiliani and of Shakeleton, demonstrated that during Quaternary period the cycles of glacial-interglacial were much more than four times. The correspondence between the paleoclimate records from deep ocean sediments as well as continental loess and the earth orbital parameters have established a solid framework for the study of climate change mechanisms. In recent years, the new discoveries including climatic instability during last glacial period have provided an opportunity to study the characteristics and mechanisms of the millennial scale climate changes. However, paleoclimatologists are still puzzled by the climate change mechanisms concerning the devolopment of glacial-interglacial cycles, the symchronic climate changes between Northern and Southern Hemisphere, and the operation of the climate instability.
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