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Physiographic and floristic gradients across topography in transitional seasonally dry evergreen forests of southeast Pará, Brazil

机译:巴西帕拉东南部过渡性季节性干燥常绿森林中地貌的生理和区系梯度

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Seasonally dry evergreen forests in southeast Pará, Brazil are transitional between taller closed forests of the interior Amazon Basin and woodland savannas (cerrados) of Brazil's south-central plains. We describe abiotic and biotic gradients in this region near the frontier town of Reden??o where forest structure and composition grade subtly across barely undulating topography. Annual precipitation averaged 1859 mm between 1995-2001, with nearly zero rainfall during the dry season months of June August. Annual vertical migrations of deep-soil water caused by seasonal rainfall underlie edaphic and floristic differences between high- and low-ground terrain. Low-ground soils are hydromorphic, shaped by perching water tables during the wet season, pale gray, brown, or white in color, with coarse texture, low moisture retention during the dry season, and relatively high macro-nutrient status in the surface horizons. Forest canopies on low ground are highly irregular, especially along seasonal streams, while overstory community composition differs demonstrably from that on high ground. High-ground soils are dystrophic, well-drained through the wet season, brown or red-yellow in color, with finer texture, higher moisture retention, and low macro-nutrient status in the surface horizons compared to low-ground soils. Forest canopies are, on average, taller, more regular, and more closed on high ground. Low-ground areas can be envisioned as energy and nutrient sinks, where, because of hydrologic cycles, canopy disturbance likely occurs more frequently than at high-ground positions if not necessarily at larger scales.
机译:巴西帕拉东南部的季节性干燥常绿森林在内部亚马逊盆地的较高封闭森林与巴西中南部平原的林地热带稀树草原(cerrados)之间过渡。我们描述了边境城镇Reden ?? o附近该地区的非生物和生物梯度,该地区的森林结构和组成在几乎没有起伏的地形中微妙地分级。在1995年至2001年之间,年平均降雨量为1859毫米,在8月的干旱季节,降雨量几乎为零。季节性降雨引起的深层水的年度垂直迁移是高地和低地地形之间的深层和植物性差异的基础。低地土壤是亲水性的,在雨季时栖息在地下水位上,呈浅灰色,棕色或白色,质地粗糙,在旱季保水率低,地表水平的宏观营养状况较高。低地上的林冠层高度不规则,尤其是沿季节性河流,而高楼层上的林间群落组成明显不同。与低地层土壤相比,高地层土壤营养不良,在雨季排水良好,棕褐色或红黄色,质地较细,水分保持力更高,表层的宏观养分含量较低。平均而言,林冠更高,更规则并且在高地上更封闭。可以将低地的区域设想为能量和营养的汇,由于水文循环的原因,如果不一定要扩大规模,则高地位置的冠层扰动可能比高地位置更频繁。

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