globalchange  > 气候变化与战略
CSCD记录号: CSCD:5116545
论文题名:
江苏省江都市大桥镇ZKA4钻孔第四纪孢粉组合及其环境变化研究
其他题名: PALYNOLOGICAL ASSEMBLAGES FROM THE BOREHOLE ZKA4AT DAQIAO TOWN, JIANGDU CITY, JIANGSU PROVINCE AND THEIR ENVIRONMENTAL MEANINGS
作者: 张宗言1; 于俊杰1; 蒋仁1; 韩芳2; 柯学1; 徐亚东3; 何卫红3
刊名: 微体古生物学报
ISSN: 1000-0674
出版年: 2014
卷: 31, 期:1, 页码:1162-1167
语种: 中文
中文关键词: 孢粉组合 ; 第四纪 ; 气候变化 ; 江都 ; 江苏
英文关键词: Palynological assemblage ; Quaternary ; climate change ; Jiangdu City ; Jiangsu Province ; East China
WOS学科分类: BIOLOGY
WOS研究方向: Life Sciences & Biomedicine - Other Topics
中文摘要: 本文依据江苏省江都市大桥镇第四系钻孔(ZKA4)中孢粉的分布, 自下至上划分了11个孢粉组合:1.Betula-Ulmus-Artemisia, 2.Ulmus-Chenopodiaceae-Quercus, 3.Artemisia-Gramineae-Quercus, 4.Liquidambar-Polypodiaceae-Ulmus, 5.Pinus-Quercus-Betula-Juglans, 6.Quercus-Juglans-Artemisia, 7.Quercus-Polygonum-Juglans-Carya, 8.Betula-Gramineae-Artemisia, 9.Quercus-Polypodiaceae, 10.Podocarpus-Triorites-Polypodiaceae, 11.Pinus-Podocarpus-Juglans-Pterocarya。依据孢粉组合, 识别出更新世以来七个气候冷暖变化阶段。孢粉组合1为常绿落叶针阔叶混交林, 气候以冷干为主, 向上气候回暖;孢粉组合2为高寒灌丛落叶针阔叶混交林, 以冷干为主;孢粉组合3为草本落叶针阔叶混交林, 较前一阶段气候变暖, 偏暖干;孢粉组合4-5以落叶阔叶为主, 整体上以变暖为主;孢粉组合6-7为落叶针阔叶混交林, 整体气候为暖湿, 早期略干;孢粉组合8-9为以针叶为主的针阔叶混交林, 气候温凉偏湿;孢粉组合10-11为常绿落叶阔叶混交林, 气候以湿暖为主。
英文摘要: Based on the data of palynology from the borehole ZKA4at Daqiao town, Jiangdu, Jiangsu Province, 11 assemblages are recognized as follows:1.Betula-Ulmus-Artemisia, 2.Ulmus-Chenopodiaceae-Quercus, 3.Artemisia-Gramineae-Quercus, 4.Liquidambar-Polypodiaceae-Ulmus, 5.Pinus-Quercus-Betula-Juglans, 6.Quercus-Juglans-Artemisia, 7.Quercus-Polygonum-Juglans-Carya, 8.Betula-Gramineae-Artemisia, 9.Quercus-Polypodiaceae, 10. Podocarpus-Triorites-Polypodiaceae, and 11.Pinus-Podocarpus-Juglans-Pterocarya.Based on palynological assemblage(PA), seven stages of climate change have been identified:Stage 1(corresponding to PA 1)was characterized by evergreen and deciduous broad-leaved mixed forests, representing a cold and dry, with subsequent warmer climate; Stage 2(corresponding to PA 2)was dominated by alpine shrubs, deciduous broad-leaved mixed forests, representing a cold and dry climate;Stage 3(corresponding to PA 3)was dominated by herb deciduous broad-leaved mixed forests, show the beginning of a warm and dry climate;Stage 4(corresponding to PA 4-5)was associated with deciduous broad-leaved forests, displaying the overall warmer climate;Stage 5(corresponding to PA 6-7)was dominated by deciduous broad-leaved mixed forests, indicating it was warm and slightly dry;Stage 6(corresponding to PA 8-9) was dominated by the coniferous forests(consisting mainly of coniferous and broad-leaved mixed forests), representing a cool and wet climate;Stage 7(corresponding to PA 10-11)was associated with evergreen and deciduous broadleaved mixed forests, mainly representing a warm and wet climate.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/148488
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作者单位: 1.南京地质矿产研究所, 南京, 江苏 210016, 中国
2.中国地质大学(武汉)地球科学学院, 武汉, 湖北 430074, 中国
3.中国地质大学(武汉)地球科学学院, 生物地质与环境地质国家重点实验室, 武汉, 湖北 430074, 中国

Recommended Citation:
张宗言,于俊杰,蒋仁,等. 江苏省江都市大桥镇ZKA4钻孔第四纪孢粉组合及其环境变化研究[J]. 微体古生物学报,2014-01-01,31(1):1162-1167
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