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《Journal of Glaciology and Geocryology》 2003-05
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Characteristics of δ~(13) C Values of Desert Plants and Their Water Utilization Efficiency Indicated by δ~(13) C Values in the Desert of Central Hexi Corridor Region

SU Pei\|xi,\ CHEN Huai\|shun,\ LI Qi\|sen (Linze Desert Ecosystem Station, CAREERI, CAS, Lanzhou Gansu 730000, China)  
Temperate desert plants always grow in the high temperature, arid and water deficit environment throughout a year. Different plants have different photosynthetic organs to adapt extreme environmental conditions. The purpose of this paper is to probe into the characteristics of\{δ 13 C\} of leaves and assimilating shoots and into water use efficiency (WUE) of desert plants, and to provide a theoretical basic for protecting and fostering natural ecosystems of desert regions. The results achieved by the present study will serve restoring the degraded vegetation and maintaining the stability of protective eco\|systems in the peripheric districts of oases. The\{δ 13 C\} values of leaves and assimilating shoots of desert plants in the desert of central Hexi Corridor region (39°19′~39°21′ N, 100°02′~100°21′ E, \{1 368\}~\{1 380\} m a.s.l.) were analyzed and discussed in this paper. \{δ 13 C\} of leaves and assimilating shoots and \{δ 13 C\} air were analysed with MAT\|252 mass spectrometer. The characteristics of\{δ 13 C\} of leaves or assimilating shoots and WUE of plants indicated by\{δ 13 C\} values in this region were also studied. At the same time, comparative studies of shelterbelt arborous species and some oasis crops were also carried out. The results indicate that the \{δ 13 C\} values of assimilating shoots of \%Haloxylon ammodendron\% and \%Calligonum mongolicum\% are \{-14.31‰\} and \{-14.8‰\} respectively, and stable carbon isotope discrimination (\%Δ\%) is between 5‰~6‰. The \{δ 13 C\} values of leaves for \%Caragana korshinskii, Nitraria sphaerocarpa, Hedysarum scoparium\% and \%Reaumuria soongorica\% are \{-25.75‰\}, \{-25.79‰\}, \{-26.38‰\} and \{-28.05‰\} respectively, while \%Δ\% is between 16‰~20‰.\;The long\|term water use efficiency of several desert plant species can be ranked in the general order: \%H. ammodendron≈C. mongolicumC. korshinskii≈N. sphaerocarpa≈H. \{scoparium\}R. soongorica\%.
【Fund】: 中国科学院知识创新工程方向性项目(KZCX3 SW 329);; 中国科学院知识创新工程重大项目(KZCX1 09 02);; 国家重点基础研究发展规划项目(G2000048704)资助
【CateGory Index】: Q948
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6 LIN Qing, WANG Shao ling, ZHAO Lin (State Key Laboratory of Frozen Soil Engineering, CAREERI, CAS, Lanzhou Gansu 730000,China);The Records of Atmospheric CO_2 Derived from the Stable Carbon Isotopic Composition of Buried Plant Tissues in Perennial Frozen Lacustrine Sediments[J];Journal of Glaciolgy and Geocryology;2001-01
7 CHEN Tuo~ 1, 2\},\ QIN Da\|he~ 1,\ HE Yuan\|qin~ 1,\ REN Jia\|wen~ 1,\ LIU Xiao\|hong~ 1 (1.Key Laboratory of Ice Core and Cold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000, China; 2.National Laboratory of Western Chinas Environmental;The Pattern of Stable Carbon Isotope Ratios in \%Sabina przewalskii\%[J];Journal of Glaciolgy and Geocryology;2002-05
8 LIU Xiao\|hong~ 1,\ QIN Da\|he~ 1,\ SHAO Xue\|mei~ 2,\ REN Jia\|wen~ 1,\ WANG Yu~ 1 (1.Key Laboratory of Ice Core and Cold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000; 2.Institute of Geographic Sciences and Natural Resources Research,;Stable Carbon Isotope of \%Abies spectabibis\% from Nyingchi County of Tibet Autonomous Region and Its Response to Climate Change[J];Journal of Glaciolgy and Geocryology;2002-05
9 LI Xiang bo 1 CHEN Jian fa 2 ZHANG Ping zhong 2 LIU Guang xiu 3 1 (Northwest Institute of Geology, CUNPE Lanzhou 730020) 2 (Lanzhou Institute of Geology Chinnse Academy of Sciences Lanzhou 730000) 3 (Lanzhou Institute of Glaciology;The Characteristics of Carbon Isotope Composition of Modern Plants over Qinghai Tibet Plateau (NE) and Its Climatic Information[J];ACTA SEDIMENTOLOGICA SINICA;1999-02
10 Li Xiubin(Institute of Geography,Chinese academy of Science and the State Planning ommission of P.R.China,Beijing 100101);A REVIEW OF THE INTERNATIONAL RESEARCHES ON LAND USE/LAND COVER CHANGE[J];ACTA GEOGRAPHICA SINICA;1996-06
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