鲍锟山,王国平,赵红梅,邢伟,吕宪国

• 1:中国科学院湿地生态环境重点实验室中国科学院东北地理与农业生态研究所
• 2:中国科学院研究生院

摘要(Abstract)：

气候变化是影响全球泥炭沼泽分布和演化的最重要的因子之一,而泥炭地由于自身的特点成为过去气候变化的良好地质档案。在介绍泥炭沉积过程及不同类型的泥炭沼泽的发育特点基础上,从过去气候变化的常用泥炭记录和泥炭地碳记录等方面总结了国际上针对泥炭地反演气候变化研究的若干重要进展,重点剖析了泥炭腐殖化度、植物残体、有壳变形虫、生物标志化合物、同位素和孢粉等泥炭地过去气候变化重建的代用指标的适用范围和优缺点,同时也分析了泥炭地碳累积和碳循环等热点研究问题。最后从泥炭地作为过去气候变化的记录档案、泥炭地对现在气候变化的响应与反馈及在泥炭地进行现场气候变化监测与实验等方面对泥炭地与气候变化研究进行了展望。

关键词(KeyWords)： 泥炭地;气候变化;地质记录;气候变化代用指标;碳累积;碳循环

Abstract:

Keywords:

基金项目(Foundation): 国家重点基础研究发展计划项目(No.2012CB956100);; 国家自然科学基金资助项目(No.40830535,40871089)

作者(Author): 鲍锟山,王国平,赵红梅,邢伟,吕宪国

DOI: 10.19839/j.cnki.dcxzz.2012.01.014

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