植物生态学报 ›› 2006, Vol. 30 ›› Issue (3): 504-513.DOI: 10.17521/cjpe.2006.0067
接受日期:
2005-08-04
出版日期:
2006-05-30
发布日期:
2006-05-30
作者简介:
E-mail: yongchuanyang@yahoo.com.cn
基金资助:
YANG Yong-Chuan1,2,3(), DA Liang-Jun3,4
Accepted:
2005-08-04
Online:
2006-05-30
Published:
2006-05-30
摘要:
植物群落的本质特征之一是群落中的植物和环境之间存在一定的相互关系。湿润的丘陵地区是由水侵蚀而形成的包含各种干扰频率的生境复合体,作为中尺度的地形单位,可以通过侵蚀前线划分为上部坡面和下部坡面两个小尺度的地形单位,而上部坡面可以进一步划分为顶坡、上部边坡、谷头凹地等微地形单元,下部坡面可以进一步划分为下部边坡、麓坡、泛滥性阶地及谷床等微地形单元。上部坡面发育的是气候顶极群落,沿顶坡向谷头凹地,群落发生逐渐、连续的变化,下部坡面发育的为地形群落,其物种组成、结构以及其它生态特征与上部坡面具有显著的差异,而其微地形单元之间植被的变化不明显。干扰作用是不同地形植被分异的控制因子,也是地形植被维持和更新的关键因子。下部坡面以相对积极的土壤侵蚀、滑坡和崩塌等过程为特征,其植被更新依赖于频繁的地面干扰,而上部坡面长期稳定,其植被更新依赖于林窗动态。地形是影响植被格局的最重要的也是最基本的生境因子,其引起的生境生态位分化为物种的共存提供了条件,导致了小尺度空间内高生物多样性的形成和维持。
杨永川, 达良俊. 丘陵地区地形梯度上植被格局的分异研究概述. 植物生态学报, 2006, 30(3): 504-513. DOI: 10.17521/cjpe.2006.0067
YANG Yong-Chuan, DA Liang-Jun. A BRIEF REVIEW OF STUDIES ON DIFFERENTIATION OF VEGETATION PATTERN ALONG A TOPOGRAPHIC GRADIENT IN HILLY REGIONS. Chinese Journal of Plant Ecology, 2006, 30(3): 504-513. DOI: 10.17521/cjpe.2006.0067
图1 丘陵地微地形区分模式图(改自Nagamatsu & Miura, 1997) CS:顶坡 Crest slope US:上部边坡 Upper sideslope HH:谷头凹地 Head hollow LS:下部边坡 Lower sideslope FS:麓坡 Foot slope FT:泛滥性阶地 Flood terrace RB:谷床 Rive bed △和▲分别代表凸和凹的坡面变换 △ and ▲ indicate convex and concave break of slope, respectively
Fig.1 The schematic diagram of the micro-landforms in a hilly area(Modified from Nagamatsu & Miura, 1997)
图3 不同地貌特征的演替格局 箭头表示一次干扰,粗黑线表示顶极种
Fig.3 Illustration of succession pattern on sites with different geomorphic features The arrow indicates one disturbance and the thick black line indicates the climax species
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