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土壤并不能解释中非热带雨林中的单优现象。

Soil does not explain monodominance in a Central African tropical forest.

机构信息

School of Geography, University of Leeds, Leeds, United Kingdom.

出版信息

PLoS One. 2011 Feb 10;6(2):e16996. doi: 10.1371/journal.pone.0016996.

Abstract

BACKGROUND

Soil characteristics have been hypothesised as one of the possible mechanisms leading to monodominance of Gilbertiodendron dewerei in some areas of Central Africa where higher-diversity forest would be expected. However, the differences in soil characteristics between the G. dewevrei-dominated forest and its adjacent mixed forest are still poorly understood. Here we present the soil characteristics of the G. dewevrei forest and quantify whether soil physical and chemical properties in this monodominant forest are significantly different from the adjacent mixed forest.

METHODOLOGY/PRINCIPAL FINDINGS: We sampled top soil (0-5, 5-10, 10-20, 20-30 cm) and subsoil (150-200 cm) using an augur in 6 × 1 ha areas of intact central Africa forest in SE Cameroon, three independent patches of G. dewevrei-dominated forest and three adjacent areas (450-800 m apart), all chosen to be topographically homogeneous. Analysis--subjected to Bonferroni correction procedure--revealed no significant differences between the monodominant and mixed forests in terms of soil texture, median particle size, bulk density, pH, carbon (C) content, nitrogen (N) content, C:N ratio, C:total NaOH-extractable P ratio and concentrations of labile phosphorous (P), inorganic NaOH-extractable P, total NaOH-extractable P, aluminium, barium, calcium, copper, iron, magnesium, manganese, molybdenum, nickel, potassium, selenium, silicon, sodium and zinc. Prior to Bonferroni correction procedure, there was a significant lower level of silicon concentration found in the monodominant than mixed forest deep soil; and a significant lower level of nickel concentration in the monodominant than mixed forest top soil. Nevertheless, these were likely to be the results of multiple tests of significance.

CONCLUSIONS/SIGNIFICANCE: Our results do not provide clear evidence of soil mediation for the location of monodominant forests in relation to adjacent mixed forests. It is also likely that G. dewevrei does not influence soil chemistry in the monodominant forests.

摘要

背景

土壤特性被认为是导致中非一些地区吉尔伯蒂odendron 德韦雷单优势群落形成的可能机制之一,在这些地区,原本应该存在更高多样性的森林。然而,关于 G. dewevrei 主导森林与其相邻混合林之间土壤特性的差异仍知之甚少。在这里,我们介绍了 G. dewevrei 森林的土壤特性,并量化了这种单优势森林的土壤物理和化学性质是否与相邻混合林有显著差异。

方法/主要发现:我们在喀麦隆东南部中非森林的 6×1 公顷未受干扰的区域内,使用 augur 采集了表层土(0-5、5-10、10-20、20-30 cm)和底土(150-200 cm),其中包括 3 个独立的 G. dewevrei 主导林斑块和 3 个相邻区域(相距 450-800 m),所有这些区域都选择在地形上是同质的。分析——经过 Bonferroni 校正程序——表明,在土壤质地、中值粒径、体积密度、pH 值、碳(C)含量、氮(N)含量、C:N 比、C:总 NaOH 可提取 P 比和可利用磷(P)、无机 NaOH 可提取 P、总 NaOH 可提取 P、铝、钡、钙、铜、铁、镁、锰、钼、镍、钾、硒、硅、钠和锌的浓度方面,单优势林和混合林之间没有显著差异。在进行 Bonferroni 校正程序之前,在单优势林的深层土壤中发现硅浓度显著低于混合林,而在单优势林的表层土壤中发现镍浓度显著低于混合林。然而,这可能是多次进行显著性检验的结果。

结论/意义:我们的结果并没有为单优势林相对于相邻混合林的位置提供土壤中介的明确证据。也有可能 G. dewevrei 不会影响单优势林中的土壤化学性质。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1f4d/3037391/46039308d889/pone.0016996.g001.jpg

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