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地球科学进展  2014, Vol. 29 Issue (12): 1341-1354    DOI: 10.11867/j.issn.1001-8166.2014.12.1341
综述与评述     
现代陆生植物碳同位素组成对气候变化的响应研究进展
刘贤赵1, 2, 张勇1, 宿庆3, 田艳林1, 全斌1, 王国安4
1.湖南科技大学建筑与城乡规划学院,湖南 湘潭 411201; 2.中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室,江苏 南京210008; 3.湖南科技大学生命科学学院,湖南 湘潭 411201; 4.中国农业大学资源与环境学院,北京100193
Research Progress in Responses of Modern Terrestrial Plant Carbon Isotope Composition to Climate Change
Liu Xianzhao1, 2, Zhang Yong1, Su Qing3, Tian Yanlin1, Quan Bin1, Wang Guoan4
1.College of Architecture and Urban Planning,Hunan University of Science and Technology,Xiangtan 411201,China; 2. State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,CAS,Nanjing 210008,China; 3. College of Life Science, Hunan University of Science and Technology,Xiangtan 411201,China; 4. College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China
 全文: PDF(1973 KB)  
摘要:

植物组织的碳同位素组成(13C)能够记录气候变化的信息,因而被作为指示气候环境变化的一个重要代用指标,并广泛应用于全球变化研究。然而,气候环境变化引起的现代植物13C及其指示的气候环境意义的不确定性限制了植物13C在气候环境变化等领域研究中的应用。在概述植物碳同位素分馏和不同光合型植物碳同位素分布的基础上,综述了温度、降水、大气CO2浓度和海拔高度等气候环境因子对陆生植物13C的影响以及它们之间的关系,分析了植物13C对气候因子变化的响应机理。指出为更准确地认识气候历史,在利用植物碳同位素技术进行全球变化的研究过程中,需要突出C4植物13C对气候环境参数的响应研究,加强不同尺度植物13C的转换关系以及与相关学科的交叉渗透、探索与多种代用指标和科学方法的联合研究。

关键词: 全球变化古气候重建碳同位素气候环境因子    
Abstract:

Global climate change has been one of the most concerned environmental problems in the world since the 1980s. Since stable carbon composition (13C) in plant tissues can record abundant information on climate changes, it has been widely used as an important climate proxy in global change studies and becomes a powerful tool for obtaining paleoclimate information, understanding paleoenvironment reconstruction and modern climate change, and predicting future climate trends. However, a lot of potential uncertainties have always involved in the reconstruction of paleoclimate and paleoenvironment by carbon isotope of the past period sediment or fossils. Among them, the most dominant uncertainty is due to our poor understanding of the relations between carbon isotope ratios of plants and climatic factors and the climatic and environmental significance indicated by modern plant 13C. This may limit the application of plant 13C in the study of climatic and environmental changes. Based on the Summary of plant 13C fractionation and carbon isotope distribution of different photosynthetic plants, the effects of environmental factors, e.g., temperature, precipitation, atmospheric CO2 concentration, and altitude on terrestrial plant 13C and their relationships were reviewed in this paper, and the response mechanism of plant 13C to climate changes were also analyzed. Furthermore, the current existing problems and the future prospects in carbon isotope study were discussed. It is pointed out that strengthening some studies such as the response of C4 plants 13C to climate environmental parameters, the transformation relation of different scale plant 13C, intersection and permeation of related disciplines, and various proxies and scientific method, will undoubtedly make us have a more accurate understanding of the climate history and eventually broaden the development of the field during the process of global change study by plant carbon isotope techniques.

Key words: Carbon isotope    Paleoclimate reconstruction    Global change.    Climatic and environmental factors
收稿日期: 2014-09-09 出版日期: 2014-12-20
:  P467  
基金资助:

湖南省教育厅重点项目“陆生草本植物氮同位素组成对气候温度变化的指示”(编号:14A054); 湖南省自然科学基金项目“陆生植物氮同位素组成及其与气候温度的关系研究”(编号:2015JJ2062)资助

作者简介: 刘贤赵(1970-),男,湖南隆回人,教授,主要从事碳氮同位素与气候环境重建研究.
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刘贤赵, 张勇, 宿庆, 田艳林, 全斌, 王国安. 现代陆生植物碳同位素组成对气候变化的响应研究进展[J]. 地球科学进展, 2014, 29(12): 1341-1354.

Liu Xianzhao, Zhang Yong, Su Qing, Tian Yanlin, Quan Bin, Wang Guoan. Research Progress in Responses of Modern Terrestrial Plant Carbon Isotope Composition to Climate Change. Advances in Earth Science, 2014, 29(12): 1341-1354.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2014.12.1341        http://www.adearth.ac.cn/CN/Y2014/V29/I12/1341

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