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Many shades of green: the dynamic tropical forest–savannah transition zones

机译:许多绿色阴影:动态的热带森林-热带草原过渡带

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摘要

The forest–savannah transition is the most widespread ecotone in tropical areas, separating two of the most productive terrestrial ecosystems. Here, we review current understanding of the factors that shape this transition, and how it may change under various drivers of local or global change. At broadest scales, the location of the transition is shaped by water availability, mediated strongly at local scales by fire regimes, herbivory pressure and spatial variation in soil properties. The frequently dynamic nature of this transition suggests that forest and savannah can exist as alternative stable states, maintained and separated by fire–grass feedbacks and tree shade–fire suppression feedback. However, this theory is still contested and the relative contributions of the main biotic and abiotic drivers and their interactions are yet not fully understood. These drivers interplay with a wide range of ecological processes and attributes at the global, continental, regional and local scales. The evolutionary history of the biotic and abiotic drivers and processes plays an important role in the current distributions of these transitions as well as in their species composition and ecosystem functioning. This ecotone can be sensitive to shifts in climate and other driving factors, but is also potentially stabilized by negative feedback processes. There is abundant evidence that these transitions are shifting under contemporary global and local changes, but the direction of shift varies according to region. However, it still remains uncertain how these transitions will respond to rapid and multi-faceted ongoing current changes, and how increasing human influence will interact with these shifts.This article is part of the themed issue ‘Tropical grassy biomes: linking ecology, human use and conservation’.
机译:森林大草原过渡是热带地区最普遍的过渡带,将两个生产力最高的陆地生态系统分隔开。在这里,我们回顾了目前对影响这一转变的因素的理解,以及在局部或全球变化的各种驱动因素下其如何变化。在最广泛的尺度上,过渡的位置是由水的可利用性决定的,在局部尺度上,火势,食草压力和土壤性质的空间变化强烈地介导了过渡。这种过渡的频繁动态性质表明,森林和大草原可以作为替代的稳定状态存在,并通过火草反馈和树荫火抑制反馈来维持和分隔。然而,该理论仍在争论之中,主要的生物和非生物驱动因素及其相互作用的相对贡献尚未得到充分理解。这些驱动因素与全球,大陆,区域和地方范围内的各种生态过程和属性相互作用。生物和非生物驱动因子和过程的进化历史在这些过渡的当前分布及其物种组成和生态系统功能中发挥着重要作用。这种过渡带可能对气候变化和其他驱动因素敏感,但也可能通过负反馈过程而稳定下来。有大量证据表明,这些转变在当代全球和局部变化的影响下正在发生转变,但是转变的方向因地区而异。但是,仍然不确定这些过渡如何应对快速,多方面的当前变化,以及人类日益增加的影响将如何与这些变化相互作用。本文是“热带草类生物群落:将生态学,人类利用联系起来”这一主题问题的一部分。和保护”。

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