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北京地区15000年以来环境变迁中灾害性气候突变事件的讨论
DISASTROUS ABRUPT CLIMATE EVENTS OF ENVIRONMENT CHANGE IN BEIJING IN RECENT 15 000 YEARS
【摘要】 通过高分辨率孢粉分析及烧失量、炭屑实验结果的统计分析,结合14C、古地磁等,对北京房山东甘池15000a以来植被变化和环境变迁进行了较为深入的研究,特别强调气候变化的灾害性突变事件。初步得知约在14100~14000aB.P.前后曾出现与哥得堡反转相对应的事件,在10000aB.P.左右出现类似与新仙女木事件相对应的事件,在大约5770aB.P.和4560aB.P.左右及2850~2650aB.P.出现了大暖期的突然降温事件。
【Abstract】 In this paper, 197 samples were gathered from a 820 cm profile in Dongganchi of Fangshan, Beijing. They provided a continuous records of vegetation and environmental changes over ca. 15000a. B. P.. By these records, it is concluded that about 14100-14000aB.P.,the climate was cold and dry, which corresponds to Gothenburg Drift and interval between 10620 to 10310aB. P.. The rapid decline in pollen,charcoal concentrations and LOI implied a more colder climate and probably corresponded to Younger Dry as cooling event,at 5770aB.P.and 4650aB.P.and 2850-2650aB.P.,while the decline of forest cover showed three abrupt cold episodes.
【Key words】 Dongganchi; 15000aB.P.; Sporopollen analysis; Paleo-environment; Abrupt climate event; Climate anomaly;
- 【文献出处】 灾害学 ,JOURNAL OF CATASTROPHOLOGY , 编辑部邮箱 ,1996年02期
- 【分类号】P467
- 【被引频次】16
- 【下载频次】302