Geological Records for Holocene Climatic and Environmental Changes Derived from Glacial, Periglacial and Lake Sediments
详细信息
- 责任者：Li Shijie (State Key Laboratory for Environment Geochemistry ; Institute of Geochemistry ; Chinese Academy of Sciences ; Guiyang 550002 ; China) ; Chen Wei
- 刊名：Quaternary Sciences
- 出版年：2012
- 卷期：32(1)
- 关键词：全新世 ; Holocene ; 古气候 ; paleoclimate ; 青藏高原 ; Qinghai-Tibetan Plateau
- 页码：p.151-157
- 图表：7 illus., 2 tables, 34 refs.
- 分类号：1400
- issnNo：ISSN1001-7410
- isbnNo：CN11-2708/P
摘要
Holocene is called as an epoch of interglacial with a time period of about 10 000 years. With strong climate fluctuations during this epoch, human civilization has emerged and dramatically advanced. However, the climate warming at present day has drawn all governments and scientists concerns over the world to pay great attention to this situation. IPCC has published several versions of evaluation about climate warming and its impact on human society. However, climate fluctuated frequently in tens year, century or millenary cycles during Holocene period. Therefore, the processes and mechanics of climate fluctuation during the Holocene period are basic scientific problems which needs to be well understood for predicting and modeling climate changes and its impact in the future.