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Tailoring restoration interventions to the grassland-savanna-forest complex in central Brazil

机译:为巴西中部的草原-热带草原-森林综合体量身定制恢复干预措施

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Defining the reference system for restoration projects in regions characterized by complex vegetation mosaics is challenging. Here we use the Cerrado region of Brazil as an example of the importance of clearly defining multiple natural and anthropogenically altered states in grassland-savanna-forest mosaics. We define three main, natural vegetation types-grassland, savanna, and scleromorphic (cerradao) forest-to (1) distinguish between original and degraded states and (2) set appropriate targets for and guide restoration. We contend that the differences in Cerrado vegetation composition originally were driven by soil conditions and secondarily by fire frequency and precipitation patterns that differ from the core to the edge of the Cerrado region. Grasslands are found on the shallowest, least fertile soils and/or in waterlogged soils; scleromorphic forests are generally located on deeper, more fertile soils; and savannas occupy an intermediate position. In recent decades, this biophysical template has been overlain by a range of human land-use intensities that strongly affect resilience, resulting in alternative anthropogenic states. For example, areas that were originally scleromorphic forest are likely to regenerate naturally following low- or medium-intensity land use due to extensive resprouting of woody plants, whereas grassland restoration requires reintroduction of grass and forb species that do not tolerate soil disturbance and exotic grass competition. Planting trees into historic grasslands results in inappropriate restoration targets and often restoration failure. Correctly identifying original vegetation types is critical to most effectively allocate scarce restoration funding.
机译:为以复杂植被镶嵌为特征的区域的修复项目定义参考系统具有挑战性。在这里,我们以巴西的塞拉多地区为例,说明在草原-热带稀树草原-森林马赛克中明确定义多个自然和人为改变的州的重要性。我们定义了三种主要的自然植被类型:草地,热带稀树草原和硬皮(锯齿)森林,以(1)区分原始状态和退化状态,(2)设定适当的目标并指导恢复。我们认为,塞拉多植被组成的差异最初是由土壤条件驱动的,其次是由从塞拉多地区的核心到边缘不同的火灾频率和降水模式。草原位于最浅,最不肥沃的土壤和/或浸水的土壤中;硬皮森林通常位于更深,更肥沃的土壤上;稀树草原处于中间位置。在最近的几十年中,这种生物物理模板被一系列人类土地利用强度所覆盖,这些强度严重影响了复原力,导致了其他人类活动状态。例如,由于木本植物的大量繁殖,原本属于硬质森林的地区很可能在低强度或中等强度的土地利用后自然再生,而草地恢复需要重新引入不容忍土壤干扰和外来草种的草和forb物种竞争。在历史悠久的草原上植树会导致不适当的恢复目标,并经常导致恢复失败。正确识别原始植被类型对于最有效地分配稀缺的修复资金至关重要。

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