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| 云南鹤庆盆地中更新世以来的孢粉记录及其植被与气候变化 | |
| 引用本文： | 肖霞云,沈吉,肖海丰,童国榜.云南鹤庆盆地中更新世以来的孢粉记录及其植被与气候变化[J].湖泊科学,2006,18(4):369-376. |
| 作者姓名： | 肖霞云 沈吉 肖海丰 童国榜 |
| 作者单位： | 1. 中国科学院南京地理与湖泊研究所,南京,210008;中国科学院研究生院,北京,100039 2. 中国科学院南京地理与湖泊研究所,南京,210008 3. 中国地质科学院水文地质环境地质研究所,正定,050803 |
| 基金项目： | 国家高技术研究发展计划(863计划) |
| 摘 要： | 通过对“中国大陆环境钻探计划”首钻——云南鹤庆深钻前155 m约800 ka以来的岩芯进行孢粉研究,探讨了云南鹤庆盆地中更新世以来的植被演替与古气候变迁．研究表明鹤庆盆地周围山地的植被在约800 kaBP至6．98 kaBP之间经历了以松为主的针叶林、山地针阔叶混交林、寒温性针叶林的多次相互演替;从6．98 kaBP开始,植被发生了转折性变化,森林植被迅速退化,以草本为主,此时开始受到人类活动的影响,人类活动表现在砍伐森林和种植农作物等方面.与植被演替相应的古气候可划分为五个大的阶段,包含多次冷暖、干湿旋回． |
| 关 键 词： | 孢粉记录 植被演替 气候变化 中更新世 鹤庆盆地 |
| 收稿时间： | 2005-08-22 |
| 修稿时间： | 2005-09-22 |
Pollen records and vegetation and climate changes in Heqing Basin, Yunnan Province since middle Pleistocene |
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| XIAO Xiayun,SHEN Ji,XIAO Haifeng and TONG Guobang.Pollen records and vegetation and climate changes in Heqing Basin, Yunnan Province since middle Pleistocene[J].Journal of Lake Science,2006,18(4):369-376. | |
| Authors: | XIAO Xiayun SHEN Ji XIAO Haifeng and TONG Guobang |
| Institution: | Nanjing Institute of Geography and Limnology, CAS, Nanjing 210008, P. R. China;Graduate School, CAS, Beijing 100039, P. R. China,Nanjing Institute of Geography and Limnology, CAS, Nanjing 210008, P. R. China,Nanjing Institute of Geography and Limnology, CAS, Nanjing 210008, P. R. China;Graduate School, CAS, Beijing 100039, P. R. China and Institute of Hydrogeology and Engineering Geology, CAGS, Shijiazhuang 050061, P. R. China |
| Abstract: | Vegetational succession and climatic change since middle Pleistocene in Heqing Basin in Yunnan Province are discussed according to the sporopollen analysis for the top 155m length core and about 800 kaBP history from Heqing deep drilling core. This core is the first drilling core of Environmental Drilling Programme in Chinese continent. The results show that vegetation in the surrounding mountains in Heqing cathchment experienced many times changes among coniferous forest dominated by Pinus, montane coniferous and broadleaved mixed forest and cool temperate coniferous forest during the period about 800 kaBP to 6. 98 kaBP. From 6. 98 kaBP to today, vegetation has immensely changed, such as forest degraded quickly and vegetation dominated by herbs, when human activities have begun affecting vegetation. Human activities represent disafforestation and planting crops and so on. Climate corresponding to vegetation evolution may be divided into five stages and contains many times cool and warm, dry and humid gyrations since about 800 kaBP. |
| Keywords: | Sporopollen record vegetational succession climatic change middle Pleistocene Heqing Basin |
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