山地河流浅滩生境潜流层大型无脊椎动物群落拓殖  

Recolonization of hyporheic microinvertebrate communities in a mountain stream

作　　者：张跃伟[1,2,3] 袁兴中[1,2,3] 刘红[3] 任海庆[1,2,3] 邓伟[1,2,3] 岳俊生[1,2,3] 

机构地区：[1]煤矿灾害动力学与控制国家重点实验室,重庆400030 [2]西南资源开发及环境灾害控制工程教育部重点实验室,重庆400030 [3]重庆大学资源及环境科学学院,重庆400030

出　　处：《生态学报》2016年第15期4873-4880,共8页Acta Ecologica Sinica

基　　金：国家自然科学基金项目(51179214)

摘　　要：通过包埋人工基质法研究大型无脊椎动物在山地河流潜流层中的拓殖过程。结果表明:群落个体密度在7—29 d呈"J"型增长,在29 d后骤然降低,55 d后呈波动趋势;物种丰富度在1—29 d呈增加趋势,29 d后呈波动状态;群落的生物量总体呈增加趋势。群落的物种丰富度、密度和生物量在第29、71和83天时没有显著性差异(P>0.05),Shannon-Wiener多样性指数和Pielou均匀度指数在第55、71、83天没有显著性差异(P>0.05),综合不同拓殖时间段物种的主成分分析,表明潜流层大型无脊椎动物群落在55 d后趋于稳定。群落优势种为摇蚊(Camptochironomus sp.)、河蚬(Corbicula fluminea)、四节蜉(Baetis sp.)、动蜉(Cinygmina sp.)、纹石蛾(Hydropsyche sp.)和扁泥甲科的一种(Psephenidae)。滤食者和收集者在整个拓殖过程中均是优势功能摄食群。群落拓殖过程是一个群落自身恢复能力和外部环境影响相互作用的过程,拓殖初期潜流层的结构是影响着无脊椎动物迁入的主要因素,中期动物的生活史特征起主要作用,稳定期之后群落可能受到各因素的综合影响。The stream hyporheic zone is an ecotone of surface water-ground water interactions, is rich in biodiversity, and is an important component of stream ecosystems. The hyporheie microinvertebrates inhabiting the hyporheic zone directly influence the matter and energy dynamics of the hyporheic zone, are potential indicators of the ecological health of the river, adjust the functions of environment purification and ecological buffering, and play an important role in the structure and function of stream ecosystems. The composition and distribution of the hyporheie macroinvertebrates are affected by natural factors and human activities. The recolonization processes of hyporheic microinvertebrate communities were studied using artificial substrates in a mountain stream. Our results indicate that the individual density of mieroinvertebrates showed the J type growth curve from 7 to 29 days, declined suddenly after 29 days, and showed a fluctuating trend after 55 days. The trend of decline after 29 days was not only influenced by environmental capacity and interspecific competition, but also by external environment factors. During this period, sustained rainfall caused floods in the study area. The richness of macroinvertebrates showed an increasing trend from 1 to 29 days and a fluctuating trend after 29 days. The biomass ofmacroinvertebrates generally showed an increasing trend. The richness, density, and biomass of macroinvertebrate communities showed no significant difference at 29, 71, and 83 days （P 〉 0.05）. The Shannon-Wiener and Pielou indices also showed no significant difference at 55, 71, and 83 days （P 〉 0.05）. The species density before and after disturbance was used to indicate the recovery state of the community. However, in the long time scale, using only species density did not accurately reveal the recovery state of the stream ecosystem, because of the influence of environmental factors and life history strategy. According to the comprehensive analysis based on these trends and the principal co

关 键 词：潜流层 大型无脊椎动物 功能摄食类群 扰动 恢复 拓殖过程 

分 类 号：Q958[生物学—动物学]