机构地区:[1]School of Earth Sciences and Key Laboratory of Mineral Resources in Western China (Gansu Province),Lanzhou University [2]Agriculture Technology Department,Gansu Agriculture Technology College [3]Key Laboratory of Desert and Desertification,and Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences [4]Management Bureau of Qilianshan Mountains National Nature Reserve
出 处:《Science China Earth Sciences》2014年第4期662-670,共9页中国科学(地球科学英文版)
基 金:supported by National Basic Research Program of China(Grant No.2012CB822003);National Natural Science Foundation of China(Grant No.41172022);Specialized Research Fund for the Doctoral Program of Higher Education(Grant No.20120211110022)
摘 要:In this study, 39 leaf samples of three angiosperms (Betula albo-sinensis, tree species; and Caragana jubata and Berberis diaphana, shrub species) were collected in the middle-east parts at 2300-3640 m asl of the Qilian Mountains to study the varia- tions of leaf characteristics of angiosperms with altitude change in inland high-altitude regions of China. Five leaf indexes, viz. epidermal cell density (ED), stomatal density (SD), stomatal index (SI), leaf vein density (VD) and carbon isotopic ratio (c^13C) were analyzed in laboratory. The results show that there are significant or even very significant linear correlations between the five indexes and altitude, of which SD, SI and VD exhibit a negative correlation with altitude, while ED and Ot3C exhibit a positive correlation with altitude. Such a correlation assemblage is quite different from the situation in the low-altitude humid environment. Generally, only an assemblage of positive correlations can be observed between the indexes (viz. SD, SI and (~3C, etc.) and the altitude in the low-altitude humid environment, which were caused mainly by the plants' responses to the change of atmospheric CO2 concentration (Co). However, an assemblage of the negative and positive correlations found here may be attributed mainly to the plants' responses to the change of physiological drought caused by change of low temperature, and here it is preliminarily called the inland high-altitude pattern of plant leaf variations.In this study,39 leaf samples of three angiosperms(Betula albo-sinensis,tree species;and Caragana jubata and Berberis diaphana,shrub species) were collected in the middle-east parts at 2300–3640 m asl of the Qilian Mountains to study the variations of leaf characteristics of angiosperms with altitude change in inland high-altitude regions of China.Five leaf indexes,viz.epidermal cell density(ED),stomatal density(SD),stomatal index(SI),leaf vein density(VD) and carbon isotopic ratio(δ13C),were analyzed in laboratory.The results show that there are significant or even very significant linear correlations between the five indexes and altitude,of which SD,SI and VD exhibit a negative correlation with altitude,while ED and δ13C exhibit a positive correlation with altitude.Such a correlation assemblage is quite different from the situation in the low-altitude humid environment.Generally,only an assemblage of positive correlations can be observed between the indexes(viz.SD,SI and δ13C,etc.) and the altitude in the low-altitude humid environment,which were caused mainly by the plants' responses to the change of atmospheric CO2 concentration(Cα).However,an assemblage of the negative and positive correlations found here may be attributed mainly to the plants' responses to the change of physiological drought caused by change of low temperature,and here it is preliminarily called the inland high-altitude pattern of plant leaf variations.
关 键 词:Qilian Mountains angiosperm variations of leaf characteristics (SD SI ED VD δ13C) inland high-altitude pattern
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...