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 |
DOI | 10.1016/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。