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甘青地区末次冰消期以来植被与气候演化的孢粉记录对比分析 |
Vegetation and Climate Changes Based on the Pollen Records in Gansu-Qinghai Area since the Last Deglaciation |
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DOI: |
中文关键词: 甘青地区 末次冰消期 孢粉纪录 环境变化 A/C值 |
英文关键词:Gansu-Qinghai area Last deglaciation Pollen record Environmental change A/C ratio |
基金项目:国家自然科学基金 |
作者 | 单位 | 魏海成,马海州,潘安定,山发寿 | 1. 中国科学院青海盐湖研究所,青海西宁,810008 中国科学院研究生院,北京,100039 2. 中国科学院青海盐湖研究所,青海西宁,810008 3. 广州大学地理科学学院,广东广州,510006 |
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中文摘要: |
选用甘青地区达连海、青海湖、苏家湾、大地湾4个典型高分辨率的钻孔资料进行对比分析,阐明了该地区末次冰消期以来气候变化规律与主要气候事件,初步探讨了该地区植被纬向时空演化规律。结果显示末次冰消期大致开始于15.2—14.6ka BP之间,冰消期期间该地区气候表现为冷暖波动频繁,气候不稳定,植被类型由东向西为草原-荒漠化草原。全新世早期阶段10.4—8.2kaBP气候表现为温干,植被类型由东向西为疏林草原-草原。全新世中期8.2—4.3kaBP气候温暖湿润,植被发育良好,由东向西出现森林-森林草原植被。4.3kaBP以后该地区气候总体向凉千方向发展,3.9~3.4kaBP期间陇中地区气候波动较显著,植被类型草原-森林草原交替出现。晚全新世后期2.3~0kaBP气候冷干,从东到西发育草原-荒漠化草原植被。 |
英文摘要: |
The paper analyses the high resolution pollen records of Dalianhai lake, Qinghai lake, Sujiawan and Dadiwan sediment in Gansu-Qinghai area since the last deglaciation. And disscuses the climate change, cold-dry climate incidents and vegetation distribution from east to west in this area. It is shown that the late glacial began between 15.2 - 14. 6 ka BP, the climate was cold and humid during the early period, cold and dry during the late period, and totally unstable;meadows-desert steppe vegetation developod from east to west. In early Holocene the climate was temperate and dry, shrub meadows-meadow appeared in this area. During the middle Holocene climate was warm and wet, conifer and broad-leavod deciduous mixed forest developed. Climate became cold and dry since 3.9 - 3.4 ka BP. In early period climate was relatively warm and wet, meadows-shrub meadow vegetation developed in east of the area;in late period(2. 3 -0 ka BP) climate was dry and cold, vegetation involved to meadows-desert steppe. |
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