中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Leaf wax n-alkane carbon isotope values vary among major terrestrial plant groups: Different responses to precipitation amount and temperature, and implications for paleoenvironmental reconstruction

文献类型:期刊论文

作者Liu, Jinzhao1,2; An, Zhisheng1
刊名EARTH-SCIENCE REVIEWS
出版日期2020-03-01
卷号202页码:11
关键词Leaf wax n-alkane delta C-13 Plant groups Precipitation Temperature Global scale Paleoenvironmental reconstruction
ISSN号0012-8252
DOI10.1016/j.earscirev.2020.103081
通讯作者Liu, Jinzhao(liujinzhao@ieecas.cn)
英文摘要Studies focused on field measurements have been conducted to investigate how leaf wax n-alkane delta C-13 values vary among photosynthetic pathways (C-3 vs. C-4) or plant types (dicots, monocots, gymnosperms, magnoliids), and how n-alkane delta C-13 values respond to climate factors (precipitation, temperature). However, a systematic global analysis of plant n-alkane delta C-13 values with respect to major plant groups is still lacking, and the corresponding mechanism remains unknown. In this study, we compiled globally published n-alkanes delta C-13 data in modern plants. We find significantly negative correlations between delta C-13(wt) values and mean annual precipitation (MAP) for C-3 plants (R-2 = 0.30; p < .05), dicots (R-2 = 0.28; p < .05) and magnoliids (R-2 = 0.55; p < .05), but non-significant correlation between delta C-13(wt) values and MAP for C-4 plants (R-2 = 0.08; p = .12) or monocots (R-2 = 0.01; p = .89). However, there are significantly positive correlations between delta C-13(wt) values and mean annual temperature (MAT) in C-4 plants (R-2 = 0.33; p < .05) and monocots (R-2 = 0.35; p < .05), instead of weak correlations in C-3 plants (R-2 = 0.09; p <.05), dicots (R-2 = 0.03; p < .05) and gymnosperms (R-2= 0.06; p =.06). These results indicate that n-alkane delta C-13 values in C-3 dicots have more potential for paleoprecipitation reconstruction, while those in C-4 monocots are more likely to indicate paleotemperature changes. Our study supports use of leaf wax n-alkane delta C-13 values to gain information about paleoprecipitation and paleotemperature, but only in an appropriate paleoecological context
WOS关键词DELTA-D VALUES ; ATMOSPHERIC CO2 ; C-4 PHOTOSYNTHESIS ; LIPID BIOMARKERS ; LAKE-SEDIMENTS ; VEGETATION ; HYDROGEN ; DISCRIMINATION ; FRACTIONATION ; DISTRIBUTIONS
资助项目Chinese Academy of Sciences[QYZDY-SSW-DQC001] ; Chinese Academy of Sciences[132B61KYSB20170005] ; Chinese Academy of Sciences[ZDBS-LY-DQC033] ; National Natural Science Foundation of China[41420104008]
WOS研究方向Geology
语种英语
WOS记录号WOS:000526786000015
出版者ELSEVIER
资助机构Chinese Academy of Sciences ; National Natural Science Foundation of China
源URL[http://ir.ieecas.cn/handle/361006/14711]  
专题地球环境研究所_加速器质谱中心
第四纪科学与全球变化卓越创新中心
通讯作者Liu, Jinzhao
作者单位1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
2.CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China
推荐引用方式
GB/T 7714
Liu, Jinzhao,An, Zhisheng. Leaf wax n-alkane carbon isotope values vary among major terrestrial plant groups: Different responses to precipitation amount and temperature, and implications for paleoenvironmental reconstruction[J]. EARTH-SCIENCE REVIEWS,2020,202:11.
APA Liu, Jinzhao,&An, Zhisheng.(2020).Leaf wax n-alkane carbon isotope values vary among major terrestrial plant groups: Different responses to precipitation amount and temperature, and implications for paleoenvironmental reconstruction.EARTH-SCIENCE REVIEWS,202,11.
MLA Liu, Jinzhao,et al."Leaf wax n-alkane carbon isotope values vary among major terrestrial plant groups: Different responses to precipitation amount and temperature, and implications for paleoenvironmental reconstruction".EARTH-SCIENCE REVIEWS 202(2020):11.

入库方式: OAI收割

来源:地球环境研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。