首页> 外文期刊>Global change biology >Explaining fire-driven landscape transformation during the InitialTI Explaining fire-driven landscape transformation during the Initial Burning Period of New Zealand's prehistory
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Explaining fire-driven landscape transformation during the InitialTI Explaining fire-driven landscape transformation during the Initial Burning Period of New Zealand's prehistory

机译:解释InitialTI期间的火驱动景观转变解释新西兰史前初期燃烧期的火驱动景观转变

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At the time of Maori settlement, ca. 750 years ago, New Zealand's ecosystems experienced catastrophic change, including the introduction of fire to ignition-limited ecosystems and the resulting widespread loss of forest. While high-resolution sediment-charcoal analyses suggest this forest loss was rapid, Maori populations were small and transient during the Initial Burning Period and there is evidence for widespread fire activity in places where there is little archaeological evidence of human presence. These observations beg the question how did small populations manage to transform large areas so rapidly? Using a simulation model, we demonstrate how the relationship between time since fire and flammability in New Zealand's forests drives positive feedbacks that allow for rapid and extensive deforestation. Under ignition scenarios mirroring prehuman conditions, the model did not produce significant deforestation thus, it is extremely unlikely that deforestation could have occurred without human-initiated burning. Scenarios where ignition was spatio-temporally random also failed to result in deforestation. Rapid and widespread forest loss occurred in scenarios incorporating spatio-temporally savvy selection of ignition locations. Targeting ignitions in flammable vegetation was more important than targeting ignitions in years with favourable climatic conditions. However, targeting in space and time concurrently, such that flammable vegetation was ignited during favourable climatic years was the most efficient strategy of those simulated. Following the Initial Burning Period decadal ignitions would have been sufficient to maintain a deforested shrubland/grassland landscape. New Zealand's Initial Burning Period is one of many that occurred across eastern Polynesia following human settlement, and these events have left long-term legacy effects that remain evident in contemporary landscapes. Improving understanding of how humans shaped environments in New Zealand in the past has implications for eastern Polynesia as a whole.
机译:在毛利人定居时, 750年前,新西兰的生态系统发生了灾难性的变化,包括在点火受限的生态系统中引入了火,并导致了森林的广泛流失。尽管高分辨率的沉积物-木炭分析表明该森林的流失速度很快,但毛利人的种群在最初的燃烧时期很小且短暂,并且有证据表明在几乎没有人类存在的考古证据的地方发生了广泛的火灾。这些观察提出了一个问题,即小规模的人口如何迅速转变大面积?使用模拟模型,我们演示了自火灾以来的时间与新西兰森林的可燃性之间的关系如何推动积极反馈,从而允许迅速而广泛的森林砍伐。在反映人类前状况的点火场景下,该模型不会造成严重的森林砍伐,因此,如果没有人为引发的燃烧,就极不可能发生森林砍伐。点火时空随机的场景也未能导致森林砍伐。在结合时空明智地选择点火位置的情况下,森林迅速而广泛地流失。在可喜的气候条件下,针对可燃植物的点火比针对目标点火更为重要。但是,同时针对空间和时间进行定位,以便在有利的气候年点燃易燃植被是最有效的策略。在最初的燃烧期之后,年代际点火足以维持被砍伐的灌木丛/草地景观。新西兰的初始燃烧期是人类定居后在整个波利尼西亚东部发生的众多事件之一,这些事件留下了长期的遗产影响,在当代景观中仍然很明显。过去,人们对人类如何改变新西兰环境的认识的提高,对整个波利尼西亚东部都有影响。

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