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首页> 外文期刊>Journal of Vegetation Science >Spatial and temporal variability during primary succession on tropical coastal sand dunes
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Spatial and temporal variability during primary succession on tropical coastal sand dunes

机译:热带沿海沙丘一次演替过程中的时空变化

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摘要

We studied primary succession on mobile tropical coastal sand dunes over an 8-yr period. Every six months, we monitored changes in species composition and sand movement in permanent quadrats located on the windward slopes. the arms and the crests. Our results indicate that sand movement decreased over time but was significantly higher on the slopes and crests than on the arms. In all cases. there were seasonal fluctuations in sand movement which increased during the period with strong northerly winds and decreased during the rainy season. Sand movement was significantly correlated with species distribution. Plant cover and species richness increased at all three locations. Diversity increased on the slope, decreased on the arms and remained unchanged on the crest. However, the equitability values indicated the dominance of a few species, especially at the end of the study period. Temporal trends and species turnover rates differed among locations. Species turnover occurred first on the arms (1994), then on the crests ( 1998) and lastly on the slopes (at the end of the study period). In all cases the tall grass, Schizachyrium scoparium var. littoralis. became dominant over the endemic legume, Chamaecrista chamaecristoides var. chamaecristoides. Similar to temperate dunes, primary succession on tropical sand dunes was spatially and temporally heterogeneous.
机译:我们研究了8年期间热带移动沿海沙丘的主要演替。每六个月,我们监测位于迎风坡上的永久四方类动物的物种组成和沙运动的变化。武器和波峰。我们的结果表明,随着时间的流逝,沙的运动减少了,但坡度和波峰的沙运动明显高于臂部。在所有情况下。沙运动有季节性波动,在强北风期间增加,而在雨季减少。沙运动与物种分布显着相关。这三个地点的植物覆盖率和物种丰富度均增加。坡度上的多样性增加,手臂上的多样性降低,而波峰上的多样性则保持不变。但是,公平值表明了少数物种的优势,尤其是在研究期末。时间趋势和物种周转率因位置而异。物种更新首先发生在武器上(1994年),然后发生在波峰(1998年)上,最后发生在斜坡上(在研究期末)。在所有情况下,高草,Schizachyrium scoparium v​​ar。沿海地区。占主导地位的地方豆科植物Chamaecrista chamaecristoides var。 Chamaecristoides。与温带沙丘相似,热带沙丘上的原始演替在时间和空间上是异质的。

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