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 |
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引用本文: | 张宗言,于俊杰,蒋仁,韩芳,柯学,徐亚东,何卫红.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(1):64-74. |
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作者姓名: | 张宗言 于俊杰 蒋仁 韩芳 柯学 徐亚东 何卫红 |
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作者单位: | ;1.南京地质矿产研究所;2.中国地质大学(武汉)地球科学学院;3.生物地质与环境地质国家重点实验室 |
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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-JuglansCarya,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。
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关 键 词: | 孢粉组合 第四纪 气候变化 江都 江苏 |
PALYNOLOGICAL ASSEMBLAGES FROM THE BOREHOLE ZKA4AT DAQIAO TOWN,JIANGDU CITY,JIANGSU PROVINCE AND THEIR ENVIRONMENTAL MEANINGS |
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Institution: | ,Nanjing Center,China Geological Survey,Faulty of Earth Sciences,China University of Geosciences,State Key Laboratory of Biological Geology and Environmental Geology,China University of Geosciences |
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Abstract: | Based on the data of palynology from the borehole ZKA4at Daqiao town,Jiangdu,Jiangsu Province,11assemblages are recognized as follows:1.Betula-Ulmus-Artemisia,2.Ulmus-Chenopodiaceae-Quercus,3.ArtemisiaGramineae-Quercus,4.Liquidambar-Polypodiaceae-Ulmus,5.Pinus-Quercus-Betula-Juglans,6.Quercus-JuglansArtemisia,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. |
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Keywords: | Palynological assemblage Quaternary climate change Jiangdu City Jiangsu Province East China |
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