• 责任者：Wu Wenxiang (Institute of Geographic Sciences and Natural Resources Research ; Chinese Academy of Sciences ; Beijing 100101 ; China) ; Fang Qian
• 刊名：Marine Geology & Quaternary Geology
• 出版年：2013
• 卷期：33(6)
• 关键词：全新世 ; Holocene ; 古气候 ; paleoclimate ; 中国 ; China
• 页码：p.129-137
• 图表：74 refs.
• 分类号：1400
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

     The Longshan period（5.0-4.0 kaBP）is a key period for generation and development of the Chi- nese civilization. However, the climatic background of this period remains in dilemma. In this paper, based on historical documents, archaeological evidence, and high-resolution natural records reported dur- ing the past few decades, the climatic change during Longshan epoch was reconstructed following synthesis method recommended by IGBP. Our results indicate that the Longshang Epoch was not a uniform warm period as traditional researches suggested. It could be further divided into the early-middle Longshan WarmPeriod（5.0-4. 5 kaBP）, middle-late Longshan Cold Period（4. 5-4. 0 kaBP）,and a pronounced cooling event by the end of the Longshan period（4.2-4.0 kaBP）. The reconstructed climatic changes of the Longshan period are well correlated with the climatic records in the other parts of the world, indicating that it is at least a semi-sphere phenomenon.