基于孢粉的古气候参数定量重建:一种新思路及其在中国的应用实例
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  • 英文篇名:A novel procedure for pollen-based quantitative paleoclimate reconstructions and its application in China
  • 作者:陈建徽 ; 吕飞亚 ; 黄小忠 ; H ; J ; B ; Birks ; R ; J ; Telford ; 张生瑞 ; 许清海 ; 赵艳 ; 王海鹏 ; 周爱锋 ; 黄伟 ; 刘建宝 ; 魏国英
  • 英文作者:Chen J H;Lv F Y;Huang X Z;Birks H J B;Telford R J;Zhang S R;Xu Q H;Zhao Y;Wang H P;Zhou A F;Huang W;Liu J B;Wei G Y;Department of Biology and Bjerknes Centre for Climate Research,University of Bergen;
  • 关键词:孢粉 ; 定量重建 ; 显著性检验 ; 季风边缘区
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:兰州大学资源环境学院西部环境教育部重点实验室;Department of Biology and Bjerknes Centre for Climate Research,University of Bergen;河北师范大学泥河湾考古研究院;中国科学院地理科学与资源研究所;中国科学院大学;
  • 出版日期:2018-01-20
  • 出版单位:中国科学:地球科学
  • 年:2018
  • 期:v.48
  • 基金:国家自然科学基金项目(批准号:41471162、41571182);; 国家重点研发计划项目(编号:2017YFA0603402)资助
  • 语种:中文;
  • 页:JDXK201801003
  • 页数:9
  • CN:01
  • ISSN:11-5842/P
  • 分类号:46-54
摘要
传统的孢粉-古气候定量重建评估主要衡量校准集对现代气候状况的模拟结果或化石样品与校准集样品的可比程度,客观上导致特定地点重建气候参数的取舍缺少明确标准.基于国际上通过随机数据开展定量重建显著性检验的新方法,充分利用中国环境梯度大、植被类型丰富、现代表土孢粉数据完善等优势,提出一种孢粉-古气候参数定量重建的新思路:首先确定控制化石孢粉组成变化最主要环境因子,随后通过限制其他环境因子来构造校准集以开展该因子的定量重建,最后完成重建结果显著性评估.将该思路应用于分别位于黄土高原东、西两侧的吕梁山公海和六盘山天池化石孢粉序列,所获得的年降水量P_(ann)定量重建不仅具有统计上的显著性(p<0.001),且相互间在共同时段表现出良好、稳定的相关关系,均指示了约3300cal a BP以来的东亚夏季风降水快速下降,显示其具备降低基于孢粉的古气候参数定量重建不确定性的较大潜力.
        
引文
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    1)根据现有资料,中国北方全新世年均温度变幅不超过5℃(Wang等,2001;Ge等,2007;方修琦和侯光良,2011),而全新世大暖期与现代年均温差为2~3℃(Jiang等,2012).事实上,此处取±2℃或±3℃所获重建结果变化基本一致(图略)

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