Habitat Influence on the Molecular, Carbon and Hydrogen Isotope Compositions of Leaf Wax n-Alkanes in a Subalpine Basin, Central China

作     者：Chaoyang Yan Yiming Zhang Yanzhen Zhang Zhiqi Zhang Xianyu Huang Chaoyang Yan;Yiming Zhang;Yanzhen Zhang;Zhiqi Zhang;Xianyu Huang

作者机构：State Key Laboratory of Biogeology and Environmental GeologyChina University of GeosciencesWuhan 430078China Hubei Key Laboratory of Critical Zone EvolutionSchool of Geography and Information EngineeringChina University of GeosciencesWuhan 430078China 

出 版 物：《Journal of Earth Science》 (地球科学学刊（英文版）)

年 卷 期：2020年第31卷第4期

页      面：845-852页

核心收录：

学科分类：070902[理学-地球化学] 0709[理学-地质学] 07[理学] 0708[理学-地球物理学] 0704[理学-天文学] 0713[理学-生态学] 

基　　金：supported by the National Natural Science Foundation of China (No. 41877317) the State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences,Wuhan (No. GBL11612) the fundamental research funds for the central universities (Nos. CUGCJ1703,CUGQY1902)。 

主　　题：habitat n-alkane compound specific carbon isotope compound specific hydrogen isotope peat deposit 

摘      要：Epidermal leaf waxes of terrestrial higher plants have been widely utilized for the reconstructions of paleoenvironment and paleoclimate in peat deposits. In this study, specimens of four plant species growing in both peatland and non-peatland habitats were retrieved to compare their molecular, carbon(δ13 C) and hydrogen(δ2 H) isotopic compositions of leaf wax n-alkanes from a closed subalpine basin in Central China. Three of the four species show quite higher total concentrations of n-alkanes in the relatively dry non-peatland setting than in the peatland. In addition, the δ2 H values of long-chain n-alkanes are generally less depleted in the peatland and are comparable among different plant species, which is interpreted as the influence of inundation condition and the possible limited supply of photosynthetic products. This study reveals different patterns of plant wax molecular and isotopic compositions between peatland and the surrounding non-peatland conditions, and confirms the paleoenvironmental potential of leaf wax ratios on the peat sequences.