广西马山岩溶植被年龄序列的群落特征
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广西大学林学院,广西大学林学院,广西大学林学院,广西大学林学院,亚热带农业生物资源保护与利用国家重点实验室;中国地质科学院岩溶地质研究所,中国科学院亚热带农业生态研究所,广西大学林学院,广西大学林学院,广西大学林学院,广西大学林学院,中国地质科学院岩溶地质研究所,广西大学林学院,广西大学林学院

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国家科技支撑(2011BAC09B02); 国家林业局重点资助项目(2010TK45)


Community characteristics in a chronosequence of karst vegetation in Mashan county, Guangxi
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State Key Laboratory for Conservation and Utilization of Subtropical Agro-bioresources,,,,,,,,,,,,

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    摘要:

    石漠化地区是我国西南植被恢复和生态重建的重点和难点地区。通过对马山县岩溶植被年龄序列(石漠、草丛、灌丛、小乔林和成熟林)5个演替阶段15个样地(20 m×50 m)的系统取样调查,研究了停止人为干扰后岩溶植被的更新、演替及群落特征的变化。结果表明:沿石漠、草丛、灌丛、小乔林、成熟林的顺向演替发展,群落各层次的覆盖度存在显著差异(P<0.05),乔木层覆盖度以成熟林最大,灌木层覆盖度以小乔林最高,而草本层覆盖度以灌丛最高;重要值≥10.00的科、属、种最大值出现在小乔林;不同演替阶段群落不同层次的结构明显不同,乔木层的植物密度存在显著差异(P<0.05),以小乔林最高;成熟林灌木层的植物密度显著低于小乔林和草丛(P<0.05),与石漠和灌丛差异不显著(P>0.05);森林阶段草本层的植物密度显著低于灌丛、草丛和石漠(P<0.05);群落的物种丰富度随着顺向演替发展而增加,但不同演替阶段不同层次的丰富度变化不同,草本层的物种丰富度以草丛阶段最大,成熟林最小;灌木层的丰富度以小乔林阶段最大,石漠阶段最小;乔木层的丰富度以小乔林最大,成熟林有所下降;不同演替阶段群落草本层的生态优势度无显著差异(P>0.05),而灌木层和乔木层均存在显著差异(P<0.05)。岩溶植被恢复可分为恶劣物理环境阈值和顶极种缺乏的阈值两个阶段,每一个阶段内由不同功能特征的驱动种和关键种决定着群落的演替方向和速度,越接近演替后期,顶极种越丰富,群落驱动种和关键种向高级、大型和长寿植物发展的趋势越明显。

    Abstract:

    Desertified karst region is a focal and difficult area of vegetation recovery and ecological restoration in southwest China. We investigated changes of the regeneration, succession and community characteristics in karst vegetation after stopping human disturbance, based on a chronosequence in the kart region of Mashan county. Our sampling includes 15 plots, each of 20 m×50 m representing five successional stages (desertified karst land, grassland, scrub, young forest and mature forest). We found that vegetation succession proceeded from desertified karst land to grassland to scrub to young forest, and finally to mature forest. Vegetation cover was significant different among different successional communities at three different layers(P<0.05). The greatest cover of arbor layer was found in mature forests, of shrub layer was in young forests, and of grass layer was in scrub stage, while the maximum number of species, genera and families with importance values (IV) ≥10.00 were found in young forests. Community structures of all layers were remarkably different among successional stages, so were plant density of the tree layer, with the maximum tree density found in young forests. Plant density of the shrub layer in the mature forests was significantly lower than that in young forests and grasslands(P<0.05), and was not significantly different with desertified karst lands and scrubs(P>0.05).Species richness of the communities increased with succession, but the changes were different among all layers in different successional stages. The greatest species richness in the grass layer was found in the grassland and the lowest in the mature forest; the greatest species richness in the shrub layer was found in the young forest and the lowest in the desertified karst land stage; the greatest species richness in the tree layer was found in the young forest and the least in the mature forest. Ecological dominance was not significantly different among grass layers in different successional stages(P>0.05), but significantly different among shrub and arbor layers in different successional stages(P<0.05). The restoration of karst vegetation can be divided into two stages, each with a threshold, i.e. harsh physical environments and deficiency of climax species, respectively. At each stage, the successive direction and speed depended on the presence of different driving and keystone species with different functional characteristics. The later a successional stage was, the more aboundance of climax species, and the more obvious it was that the driving and keystone species were those of advanced, large-sized and long-lived.

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温远光,雷丽群,朱宏光,刘虹,覃林,马祖陆,王克林,庄嘉,蓝嘉川,龙涛,陆晓明,邓艳,谢益君,王家妍.广西马山岩溶植被年龄序列的群落特征.生态学报,2013,33(18):5723~5730

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