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Flooding effects on phosphorus dynamics in an Amazonian mangrove forest,TI Flooding effects on phosphorus dynamics in an Amazonian mangrove forest, Northern Brazil

机译:洪水对亚马逊红树林中磷动力学的影响,TI洪水对亚马逊红树林中磷动力学的影响

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Aims and methods We examined porewater salinity, soil redox potential (Eh), soil extractable phosphate (extr.-P), leaf phosphorus (leaf-P) and plant growth in relation to inundation frequency (IF) and mangrove species distributions along a 600 m transect in the Bragan a Peninsula, North Brazil. Results The forest species composition changed across the tidal zone with Avicennia germinans dominating (99.1%) the high intertidal (HI) zone where the IF was 41-67 d.y(-1), Rhizophora mangle, Laguncularia racemosa and A. germinans co-occured in the mid intertidal (MI), and a mixed R. mangle (47.1%) - A, germinans (41.2%) stand occupied the low intertidal (LI) zone with an IF of 124-162 d.y(-1). Low IF resulted in high Eh levels (200 mV) in the HI zone relative to the LI where Eh ranged from 0-100 mV. The IF showed a significant positive correlation with extr.-P (r=0,89; p=0.05) and a negative association with Eh (r=-0,75; p=0.05). Conclusion An ANCOVA confirmed that Eh and extr.P were influenced by flooding. Variations in these factors were reflected in patterns of P leaf tissue concentrations across the gradient; however, a MANCOVA showed that leaf-P was not related to tree height, tree volume or basal area. Waterlogging conditions, porewater salinity, and P dynamics in the sediment appear to influence the forest structure. We suggest that P availability plays an important role in controling mangrove species distributions but not their growth.
机译:目的和方法我们研究了沿600年的淹水频率(IF)和红树林物种分布与孔隙水盐度,土壤氧化还原电势(Eh),土壤可提取磷酸盐(extr.-P),叶磷(叶-P)和植物生长相关的情况。巴西北部Bragan半岛的m断面。结果潮间带森林物种组成发生变化,其中以紫花苜蓿为主导的高潮间带(HI)带(99.1%),IF为41-67 dy(-1),曼氏根霉,小花紫菜和芽孢杆菌同时发生在潮间带中段(MI)和混合的R. mangle(47.1%)-A,发芽细菌(41.2%)占据了低潮间带(LI)区,IF为124-162 dy(-1)。相对于LI(Eh范围为0-100 mV)的LI,低IF导致HI区的Eh水平较高(200 mV)。 IF与extr.-P呈显着正相关(r = 0.89; p = 0.05),与Eh呈负相关(r = 0.75; p = 0.05)。结论ANCOVA证实Eh和extr.P受洪水影响。这些因子的变化反映在整个梯度上的P叶组织浓度模式中。然而,MANCOVA的研究表明,叶的P与树的高度,树的体积或基础面积无关。渍水条件,孔隙水盐度和沉积物中的磷动力学似乎会影响森林结构。我们认为磷的有效性在控制红树林物种分布中起着重要作用,但在其生长中却不起作用。

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