globalchange  > 气候变化与战略
CSCD记录号: CSCD:5345886
论文题名:
太湖西部地区8. 2 ka BP以来的高分辨率孢粉记录
其他题名: HIGH-RESOLUTION PALYNOLOGICAL RECORD IN THE WESTERN REGION OF TAIHU LAKE SINCE 8. 2 ka BP
作者: 陆福志1; 朱诚1; 马春梅1; 张文卿2; 李冰1; 李开封1
刊名: 地层学杂志
ISSN: 0253-4959
出版年: 2015
卷: 39, 期:1, 页码:133-138,173
语种: 中文
中文关键词: 气候地层 ; AMS~(14)C.孢粉记录 ; 植被演替 ; 全新世 ; 第四纪 ; 太湖两部地区 ; 江苏
英文关键词: climatic stratigraphy ; AMS~(14)C ; sporopollen record ; vegetation succession ; Holocene ; Quaternary ; the western region of Taihu Lake ; Jiangsu
WOS学科分类: GEOLOGY
WOS研究方向: Geology
中文摘要: 通过AMS~(14)C测年技术建立年代标尺,对太湖西部地区LTD-12号钻孔301 cm以上的岩芯进行高分辨率孢粉分析.重建太湖西部地区8. 2 ka BP以来的气候和植被,并探讨了太湖地区新石器文化对气候变化的响应。结果表明:1)太湖西部地区8. 2 ka BP以来的植被类型演替过程大体为:以松属常绿栋落叶栎-枫香为主的含针叶成分的常绿落叶阔叶林以落叶栎常绿栎-枫香树属为主的常绿落叶阔叶林以松属一楓香为主的针阔叶混交林以松属为主的次生性质的针叶林。2)太湖西部地区高分辨率孢粉记录的气候变化可划分为2个大的阶段:(a)8. 2~4. 4 ka BP为中全新世温暖湿润期,最适宜期出现在6. 9-5. 5 ka BP;(b)4. 4 ka BP~0 ka BP为晚全新世降温期,气候从暖稍湿向暖干过渡。3)太湖地区的新石器文化总体上响应于气候的变化。环太湖平原地区至今未发现10~7 ka BP的新石器遗址可能与当时过于潮湿和不稳定的气候环境有关;6. 9~5. 5 ka BP温暖湿润的气候适合人类的生存,促使了马家浜文化的出现、繁荣和发展;5. 0 ka BP左右的干燥降温事件可能导致了崧泽文化的衰落;良渚文化的消亡可能与4. 4 ka BP前后该地区的气候突变事件有关。
英文摘要: In this paper, by using AMS~(14)C method to establish the time scale and making high-resolution pollen analysis of the Drilling LTD-12 above 301 centimeters deep,we reconstructed the vegetation and climate of the western region of Taihu Lake since 8. 2 ka BP,and discussed the response of Neolithic Culture to climate change. The results showed that at the period of 8. 2 ka BP to 4. 4 ka BP, the climate was warm and humid on the whole,and the vegetation was evergreen and deciduous broad-leaved mixed forest containing a little conifers, mainly donated by Pinus,Quercus and Liquidambar, and the most optimum period appeared in the period of 6. 9 ka BP to 5. 5 ka BP. After 4. 4 ka BP, the climate was changing into cool and dry, comparing to the former period, and the vegetation was coniferous forest donated by Pinus, with a secondary property. The development of Neolithic Cultures in the region of Taihu Lake showed a good correlation with the climate change. For example, the Majiabang Culture and the Songze Culture appeared and prospered in the most warm and humid period of 6. 9 ka BP to 5. 5 ka BP,which was suitable for human being,s survival. However, the Songze Culture declined and finally disappeared when the climate changed into cool and dry. The pollen record also revealed that the disappearance of Liangzhu Culture may related to the 4. 2 ka event. Why there were not any found Neolithic site from early Holocene to 7 ka BP, it may be a result of extremely humid climate, which was not suite for survival.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/149077
Appears in Collections:气候变化与战略

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作者单位: 1.南京大学地理与海洋科学学院, 南京, 江苏 210023, 中国
2.中国地质调查局水文地质工程地质技术方法研究所, 保定, 河北 071051, 中国

Recommended Citation:
陆福志,朱诚,马春梅,等. 太湖西部地区8. 2 ka BP以来的高分辨率孢粉记录[J]. 地层学杂志,2015-01-01,39(1):133-138,173
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