期刊文献+

陆生植物氮同位素组成与气候环境变化研究进展 被引量:28

Progress of Research on Relationships between Terrestrial Plant Nitrogen Isotope Composition and Climate Environment Change
原文传递
导出
摘要 近年来,由于植物氮同位素组成(δ15N)记载了气候环境变化的信息,因而被广泛应用于全球变化研究中,成为古气候环境再造和了解现代气候环境变化信息的有力工具。然而,人们对气候环境引起的δ15N变化及其指示的气候环境意义并不完全清楚,这就有可能限制植物δ15N在古气候环境变化等领域研究中的应用。在概述植物氮同位素分馏和植物不同氮源的氮同位素分布的基础上,分析了温度、降水、大气CO2浓度和海拔高度等气候环境因子对陆生植物δ15N的影响以及它们的关系。指出了目前研究中存在的问题及其研究前景,认为在全球变化研究中利用植物氮同位素技术不仅可以重建古气候环境(如重建大气CO2浓度变化),揭示历史时期温度、降水的变化,而且还可以在一定的时间和空间上综合反映生态系统氮循环的特征。 Recently, since stable nitrogen composition (δ15N) in plants records abundant climate and environment information (such as information on temperature, humidity, precipitation and environment isotopes composition) , it has been widely used in paleoctimate studies and becomes a powerful tool for understanding paleoenvironment reconstruction and modern climate change. However, some potential uncertainties have always involved in the reconstruction of paleoclimate and paleoenvironment. Among them, the most dominant uncertainty is due to our poor understanding of the relationship between nitrogen isotope ratios of plants and climatic factors, particularly the relationships among nitrogen isotope ratios, temperature and precipitation. Based on summarizing plant δ15NN fractionation and nitrogen isotope distribution of different N sources, the effects of environmental factors, e. g. , temper- ature, precipitation, atmospheric CO2 concentration, and altitude on terrestrial plant δ15N and their mechanism were analyzed in this paper. Furthermore, the existing and disputed problems in nitrogen isotope study were discussed, and the future trends of nitrogen isotope technique in global change research were prospected. It is pointed out that the technology of nitrogen isotope in plants could not only be used to rebuild paleoclimate ( such as reconstructing the sequences of atmospheric CO2 concentration changes) , revealing the trends of climate changes, but also in a certain time and space to reflect comprehensively the characteristics of nitrogen cycling in ecosystem. This will make more readers have a more profound understanding of the field and eventually broaden the development of the field.
出处 《地球科学进展》 CAS CSCD 北大核心 2014年第2期216-226,共11页 Advances in Earth Science
基金 山东省自然科学基金项目"陆生草本植物氮同位素组成对气候温度变化的指示"(编号:ZR2011DM007) 国家自然科学基金项目"小冰期以来山东半岛地区高分辨率气候环境变化的石笋记录"(编号:41171158)资助
关键词 氮同位素组成(δ15N) 气候环境因子 陆生植物 Stable nitrogen isotope composition Climatic and environmental factors Terrestrial plant.
  • 相关文献

参考文献67

  • 1Zhu H F, Shao X M, Yin Z Y, et al. August temperature variabil- ity in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings [ J ]. Palaeogeography, Palaeoclimatology, Palaeoecolo- gy, 2011, 305: 84-92.
  • 2袁子能,邢磊,张海龙,赵美训.生物标志物稳定氢同位素研究进展及在海洋古环境重建中的应用[J].地球科学进展,2012,27(3):276-283. 被引量:10
  • 3Hafida E B, Patterson R T. Influence of cellulose oxygen isotope variability in sub-fossil Sphagnum and plant macrofossil compo- nents on the reliability of paleoclimate records at the Mer Bleue Bog, Ottawa, Ontario, Canada[ J]. Organic Geochemistry, 2012, 43 : 39-49.
  • 4Meytal B H, Rebecca S R, Susan J C,et al. Evidence from chlor- in nitrogen isotopes for alternating nutrient regimes in the Eastern Mediterranean Sea [ J ]. Earth and Planetary Science Letters, 2010, 290 (1/2) : 102-107.
  • 5Verleyen E, Hodgson D A, Sabbe K, et al. Post-glacial regional climate variability along the East Antarctic coastal margin-Evi- dence from shallow marine and coastal terrestrial records [ J ]. Earth-Science Reviews, 2011, 104(4) : 199-212.
  • 6Valery J T,Zewdu E, Albert C,et al. Reconstructing palaeoenvir- onment from δ^13 C and δ^15N ransects values of soil organic matter: A calibration from arid and wetter elevation transects in Ethiopia [ J ]. Geoderma, 2008, 147 : 197-210.
  • 7李朝柱,张晓,许元斌,饶志国.黄土高原地区晚中新世以来陆地植被C_3/C_4植物相对丰度演化研究进展[J].地球科学进展,2012,27(3):284-291. 被引量:7
  • 8Reynard L M, Hedges R E. Stable hydrogen isotopes of bone col- lagen in palaeodietary and palaeoenvironmental reconstruction [ J ]. Journal of Archaeological Science, 2008, 35 : 1 934-1 942.
  • 9Wang G A, Li J Z, Liu X Z, et al. Variations in carbon isotope ratios of plants across a temperature gradient along the 400 mm iso- line of mean annual precipitation in north China and their rele- vance to paleovegetation reconstruction [ J ]. Quaternary Science Reviews, 2013, 63 : 83-90.
  • 10Ann-Kathrin S, Michael Z, Bjorn B, et al. The late Quaternary loess record of Tokaj, Hungary : Reconstructing palaeoenvironment, vegetation and climate using stable C and N isotopes and biomarkers[ J]. Quaternary International, 2011,240 : 52-61.

二级参考文献227

共引文献60

同被引文献407

引证文献28

二级引证文献109

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部