• 责任者：Zhao Yue (School of Marine Sciences ; China University of Geosciences ; Beijing100083 ; China) ; Ding Xuan
• 刊名：Quaternary Sciences
• 出版年：2011
• 卷期：31(2)
• 关键词：晚更新世 ; Upper Pleistocene ; 全新世 ; Holocene ; 季风 ; monsoon ; 印度尼西亚 ; Indonesia
• 页码：p.265-275
• 图表：4 illus., 1 table, 44 refs.
• 分类号：1400
• issnNo：ISSN1001-7410
• isbnNo：CN11-2708/P

The paper briefly shows the ways how Earth’s orbit affects the low-latitude processes such as the monsoon systems, emphasizing the significant role played by orbital forcing in the global climate system through low-latitudinal response. Based on analyses of δ¹⁸ O, δ¹³ C, AMS ¹⁴ C ages, planktonic foraminiferal assemblages, and on the sea surface temperature and salinity estimated by the planktonic foraminifera Modern Analog Technique, the authors reconstructed the paleoceanography records over the past ca.132 ka and obtained the following results: climate variation of the studied region was affected by glacial-interglacial sea-level fluctuation obviously, and followed by the 23 ka orbit precession cycle. The increased terrigenous material induced a high paleoproductivity when sea level was lower during the last glacial.