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Feedbacks between phosphorus deposition and canopy cover: The emergence of multiple stable states in tropical dry forests

机译:磷沉积与冠层覆盖之间的反馈:热带干旱森林中多个稳定状态的出现

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摘要

Dry forests represent a large percentage of tropical forests and are vulnerable to both anthropogenic and natural disturbances, yet important aspects of their sensitivity to disruption remain poorly understood. It is particularly unclear how changes in land-use or tropical storm patterns may affect the resiliency of phosphorus (P)-limited neotropical forests. In these systems, vegetation is sustained in the long-term by atmospheric P-inputs through rainfall, dust, or fog. Past research supports the idea that dust and fog deposition are dependent on canopy density (e.g. leaf area index). Thus, the canopy may function as a 'trap' for P, enabling a positive feedback between vegetation and P-deposition. We developed a conceptual model to investigate how Neotropical vegetation may respond to reduced P-deposition due to canopy losses. The model suggests that a canopy-deposition feedback may induce bistable vegetation dynamics; under some conditions, forests may be unable to naturally recover from relatively small disturbances.
机译:干旱森林占热带森林的很大比例,并且容易受到人为和自然干扰的影响,但是人们对其破坏敏感性的重要方面仍然知之甚少。尚不清楚土地利用或热带风暴的变化如何影响磷(P)受限的新热带森林的复原力。在这些系统中,通过降雨,灰尘或雾气通过大气中的P输入来长期维持植被。过去的研究支持以下观点:灰尘和雾气的沉积取决于冠层密度(例如叶面积指数)。因此,冠层可以充当P的“陷阱”,从而在植被和P沉积之间实现正反馈。我们开发了一个概念模型来研究新热带植被如何响应因冠层损失而减少的P沉积。该模型表明,冠层沉积反馈可能引起双稳态植被动态。在某些情况下,森林可能无法从较小的干扰中自然恢复。

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