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物种多样性和生物量分布规律对冻土活动层埋深变化的响应
引用本文:王增如,杨国靖,何晓波,叶柏生.物种多样性和生物量分布规律对冻土活动层埋深变化的响应[J].草业学报,2012,21(1):10-17.
作者姓名:王增如  杨国靖  何晓波  叶柏生
作者单位:中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室,甘肃兰州730000;中国科学院寒区旱区环境与工程研究所沙坡头沙漠试验研究站,甘肃兰州730000;中国科学院寒区旱区环境与工程研究所寒旱区水文与水土资源研究室,甘肃兰州,730000;中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室,甘肃兰州,730000
基金项目:国家重点基础研究发展计划(973计划),中国科学院知识创新项目,中国科学院战略性先导科技专项,国家自然科学基金
摘    要: 全球变化背景下,冻土环境变化对地上植被的影响是近年来倍受关注的重大科学问题。鉴于此,在长江源区冬克玛底流域分析了植物物种多样性和生物量空间分布规律及其对冻土活动层埋深变化的响应。结果表明,1)地上植被的物种多样性指数随着冻土活动层埋深的增加表现出非单调性递减;在冻土活动层埋深约2 m 时,物种多样性指数较高(Patrick 指数、Shannon Wiener指数和Simpson指数分别为:26.43±3.31,2.06±0.38 和0.83±0.08)。2)生物量的垂直分布规律整体表现出地下生物量明显高于地上生物量,地下生物量占总生物量的63% ~96%。3)地上生物量和地下生物量与活动层埋深均具有显著的相关性(R2 =0.65,P<0.01;R2  =0.79,P<0.01),随着活动层埋深的增加呈现出明显下降趋势。4)活动层埋深对0~40cm 深度的地下生物量的垂直分布具有显著影响。活动层埋深约1m 时,地下生物量垂直变化很小;活动层埋深大于1.5 m 时,呈倒金字塔形分布;活动层埋深大于3m 时,10~40cm 深度的地下生物量占总地下生物量的比例随着活动层埋深(3.11~4.81m)的增加而增加。

关 键 词:青藏高原  冻土活动层埋深  生物量  物种多样性  冬克玛底流域

Response of distribution patterns of plant species diversity and biomass to permafrost changes
WANG Zeng-ru , YANG Guo-jing , HE Xiao-bo , YE Bai-sheng.Response of distribution patterns of plant species diversity and biomass to permafrost changes[J].Acta Prataculturae Sinica,2012,21(1):10-17.
Authors:WANG Zeng-ru  YANG Guo-jing  HE Xiao-bo  YE Bai-sheng
Institution:1 (1.State Key Laboratory of Cryospheric Sciences,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China;2.Shapotou Desert Research and Experiment Station,Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,Lanzhou 730000,China;3.Division of Hydrology Water-Land Resources in Cold and Arid Regions,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China)
Abstract:With a background of global climate warming,the effects of permafrost changes on aboveground vegetation have attracted much attention.The effects of permafrost changes on distribution patterns of plant species diversities and biomass in the Dongkemadi River Basin(head water of Yangtze River) were investigated.1) Species diversity indexes non-monotonically decreased as the depth of the permafrost active layer increased,and the maximal values of species diversity indexes occurred at about 2 m depth of the permafrost active layer(the Partrick index,Shannon-Wiener index and Simpson index are respectively 26.43±3.31,2.06±0.38 and 0.83±0.08).2) In terms of the vertical distribution of biomass,underground biomass was considerably larger than aboveground biomass,underground biomass occupied 63%-96% of the total biomass.3) There was a significant correlation between biomass and depth of the permafrost active layer(R2=0.65,P<0.01 for aboveground biomass and R2=0.79,P<0.01 for underground biomass),and both aboveground and underground biomasses decreased as the depth of the permafrost active layer increased.4) The depth of the permafrost active layer had a considerable influence on the vertical distribution of underground biomass at soil depths of 0-40 cm: when the depth of the permafrost active layer was about 1 m,there was little vertical variation of underground biomass;but there was an obpyramidal pattern when the depth of permafrost active layer was larger than 1.5 m.When the depth of this layer was larger than 3 m,the ratio of underground biomass with soil depths of 10-40 cm to total underground biomass increased as the depth of the permafrost active layer increased.
Keywords:Qinghai-Tibet Plateau  depth of permafrost active layer  biomass  species biodiversity  Dongkemadi River Basin
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