秘鲁亚马逊雨林的原生林和次生林Igapó:植物区系、物理结构和土壤容重的预测值

R. Myster
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引用次数: 1

摘要

Igapó森林是亚马逊雨林的重要组成部分。因此,了解它们的植物区系和物理结构,以及它们如何受到土壤的影响是很重要的。描述了秘鲁洛雷托省16个原生林[10]和次生林[20]igapó样地的植物区系和物理结构,并计算了线性回归,以探讨土壤体积密度是否可以预测结构参数。10种林分中,蚕豆科、锦葵科和茜草科是最常见的科,云杉Calycophyllum spuceanum, Ceiba samauma, Inga spp,雪松,Copaifera reticulata, Phytelephas macrocarpa, Guazuma rosea和Piptadenia pteroclada是最常见的种。随着洪水的增加,容重、茎密度、茎粗、物种丰富度、fisher α、基面积和地上生物量均呈下降趋势。在20个森林中,荨麻科、茜草科和大戟科是最常见的科,膜蕨科、腺蕨科、桂花科和节肢动物科是最常见的种。海岛20林的茎数最多,4个月以上的水下10林的茎数最少;平均茎粗、物种丰富度、费氏α、基面积和地上生物量均以沙滩20林最小,1 ~ 2个月的水下10林最高。土壤容重较好地预测了平均茎粗、物种丰富度和fisher α,随着土壤沙质程度的增加,这三者均降低。我的结论是,随着土壤含沙量减少而粘土含量增加,森林结构复杂性增加,20森林中不可预测的洪水比10森林接受的可预测的洪水脉冲更能减少结构,土壤容重可能对igapó森林的多样性起因果作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Primary and Secondary Igapó Forests in the Peruvian Amazon: Floristics, Physical Structure and the Predictive Value of Soil Bulk Density
Igapó forests are a key part of the Amazon.  And so, it is important to know their floristics and physical structure, and how they may be influenced by their soil.  The floristics and physical structure of 16 primary [1o] and secondary [2o] igapó forest plots in Loreto Province, Peru was described and linear regressions were computed to explore whether soil bulk density could predict structural parameters. In the 1o forest, Fabaceae, Malvaceae and Rubiaceae were the most common families and Calycophyllum spruceanum, Ceiba samauma, Inga spp., Cedrela odorata, Copaifera reticulata, Phytelephas macrocarpa, Guazuma rosea, and Piptadenia pteroclada were the most common species. And as flooding increased, bulk density, stem density, stem size, species richness, Fishers α, basal area and above-ground biomass all decreased. In the 2o forest, Urticaceae, Rubiaceae and Euphorbiaceae were the most common families and Cecropia membranacea, Sapium glandulosum, Pourouma guianensis and Byrsonima arthropoda were the most common species. The number of stems was greatest in the island 2o forest and lowest in the 1o forest under water for more than four months, and mean stem size, species richness, Fishers α, basal area and above-ground biomass was lowest in the sandy beach 2o forest and highest in the 1o forest under water one to two months. Soil bulk density predicted mean stem size, species richness and Fishers α well, where all three decreased as soils became more sandy. I conclude that as soil becomes less sandy with more clay content there is an increase in forest structural complexity, unpredictable flooding in 2o forests reduces structure more than the predictable flood pulse 1o forests receive, and soil bulk density may have a causal role for diversity in igapó forests.
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