| 江汉平原9.0 ka B.P.以来的气候演化:来自江陵剖面沉积物记录 |
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| 引用本文： | 谢远云,李长安,王秋良,殷鸿福.江汉平原9.0 ka B.P.以来的气候演化:来自江陵剖面沉积物记录[J].地理科学,2006,26(2):199-204. |
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| 作者姓名： | 谢远云 李长安 王秋良 殷鸿福 |
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| 作者单位： | 吉林大学地球科学学院,吉林,长春,130061;哈尔滨师范大学地理系,黑龙江,哈尔滨,150080;中国地质大学地球科学学院,湖北,武汉,430074;中国地质大学地球科学学院,湖北,武汉,430074 |
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| 摘 要： | 对2002年9月在荆州市江陵县发现的9 ka B.P.以来的江陵剖面进行14C测年、粒度、TOC、TN、δ13C、孢粉等综合分析,重建江汉平原江陵地区9 ka B.P.以来古气候古环境演化:9.0~6.07 ka B.P.为高温阶段,其间8.1 ka B.P.记录到一次较明显降温事件;6.07~4.60 ka B.P.为冷干期;4.60~3.44 ka B.P.间气候波动频繁,为全新世第二个暖湿期前期阶段;3.44~2.50 ka B.P.为高温期,湖沼泥炭发育,是全新世第二个暖湿期后期阶段,为稳定的暖湿阶段;2.50 ka B.P.以来温度相对较低,为冷期。江陵地区近9 ka B.P.以来气候变化不仅与国内大量研究资料相一致,且在许多较大气候事件上与世界许多研究结果一致,表明江陵气候变化具有全球性。
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| 关 键 词： | 江汉平原 江陵地区 9.O ka B.P. 气候演化 |
| 文章编号： | 1000-0690（2006）02-0199-06 |
| 收稿时间： | 11 15 2004 12:00AM |
| 修稿时间： | 2004-11-152005-03-12 |
Climatic Change Since 9 ka B. P.: Evidence from Jiangling Area, Jianghan Plain, China |
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| XIE Yuan-Yun,LI Chang-An,WANG Qiu-Liang,YIN Hong-Fu.Climatic Change Since 9 ka B. P.: Evidence from Jiangling Area, Jianghan Plain, China[J].Scientia Geographica Sinica,2006,26(2):199-204. |
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| Authors: | XIE Yuan-Yun LI Chang-An WANG Qiu-Liang YIN Hong-Fu |
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| Institution: | 1. College of Earth Sciences, Jilin University, Changchun, Jilin 130061;2. Geography Department, Harbin Normal University, Harbin, Heilongjiang 150080;3. Faculty of Earth Sciences, China University of Geology, Wuhan, Hubei 430074 |
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| Abstract: | Jiangling Section covering the last 9000 years, found at Jiangling County, Jingzhou City, Hubei Province in September 2002, is so far the first Holocene geological section at the Jianghan Plain. By analyzing several palaeoclimatic proxies such as TOC, TN, δ13Corg, grain size and pollen, we reconstruct the climatic and environmental changes since 9 ka B.P. at the Jianghan Plain. The climate in this area was warm and wet in the period of about 9.0-6.07 ka B.P., while, a cooling event occurring around 8.1 ka B.P. is recorded by Jiangling Section; coldness and aridity period was between 6.07-4.60 ka B.P.; climatic fluctuation is especially frequent between 4.60-3.44 ka B.P.; altithermal period was between 3.44-2.50 ka B. P., meanwhile, limnic peat is widely developed; and a cold period occurred after 2.50 ka B. P. The climatic changes over the last 9 000 years in Jiangling area were coincident with large numbers of research information from domestic, moreover, many obvious climatic events were in good agreement with many international study result. It is showed that climatic change in Jiangling region is characterized by globality. |
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| Keywords: | Jianghan Plain Jiangling area 9 0 ka B P climatic change |
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