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Ingestion of charcoal by the Amazonian earthworm Pontoscolex corethrurus: A potential for tropical soil fertility

机译:亚马逊earthPontoscolex corethrurus摄入木炭:热带土壤肥力的潜力

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Pontoscolex corethrurus (Annelida: Oligocheata: Glossoscolecidae) is a small terrestrial earthworm which commonly inhabits rain forest soils over the whole Amazonian basin (Rmbke et al., 1999). Its important burrowing activity through the topsoil, associated with its efficient digestive system (Zhang et al., 1993; Barros et al., 2001), allows it to thrive in soils poor in organic matter, such as those found in areas now deforested for the need of agriculture. In the absence of organic input to the soil, excessive casting activity of this species may cause damage to permanent pastures through the coalescence of earthworm casts, leading to appearance of a thick compact surface crust (Chauvel et al., 1999). However, the detrimental influence of this species may be questioned when the agricultural use of the land is only temporary, as in slash-and-burn shifting agriculture, or when available carbon is regularly added to the soil. We hypothesized that P. corethrurus could be responsible for the observedincrease in soil fertility which has been reported to occur in Amazonian Dark Earths formed during Pre-Colombian times (Myers et al., 2003; Steiner et al., 2004). Using a quantitative optical method (Topoliantz et al., 2000), we investigated the distribution of humus components in soils under shifting cultivation, still practised by Wayana and Aluku people settled along the Maroni river, French Guiana (Topoliantz et al., 2005b). This method allowed us to estimate the relative volume of components of the soil matrix, including plant tissues at varying stages of decomposition, mineral particles of varying size and nature, aggregates of varying colour, size and shape.
机译:Pontoscolex corethrurus(Annelida:Oligocheata:Glossoscolecidae)是一种小型陆地worm,通常栖息于整个亚马逊河流域的雨林土壤中(Rmbke等,1999)。它通过有效的消化系统在表层土壤中的重要穴居活动(Zhang等,1993; Barros等,2001)使它能够在有机质贫乏的土壤中壮成长,例如在如今被砍伐森林的地区农业的需要。在没有有机物输入土壤的情况下,该物种过度的铸造活动可能通过worm的聚结对永久性牧场造成损害,从而导致出现厚实的致密地壳(Chauvel等,1999)。但是,当土地的农业用途只是临时性的(如刀耕火种的农业),或将可利用的碳定期添加到土壤中时,该物种的有害影响可能会受到质疑。我们假设,P。corethrurus可能是导致土壤肥力增加的原因,据报道这是在前哥伦布时期形成的亚马逊黑土中发生的(Myers等,2003; Steiner等,2004)。使用定量光学方法(Topoliantz等,2000),我们调查了在轮耕条件下土壤中腐殖质成分的分布情况,但仍沿沿法属圭亚那马罗尼河定居的Wayana和Aluku人仍在实践(Topoliantz等,2005b)。 。这种方法使我们能够估计土壤基质成分的相对体积,包括分解过程不同阶段的植物组织,大小和性质不同的矿物颗粒,颜色,大小和形状不同的聚集体。

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