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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >How old is the human footprint in the world's largest alpine ecosystem? A review of multiproxy records from the Tibetan Plateau from the ecologists' viewpoint
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How old is the human footprint in the world's largest alpine ecosystem? A review of multiproxy records from the Tibetan Plateau from the ecologists' viewpoint

机译:在世界上最大的高山生态系统中,人类足迹的年龄有多大?从生态学家的角度回顾青藏高原的多代理记录

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The age at which a human environment was made is strongly debated in Quaternary science. The perception of the human footprint requires an understanding of the contrast between the present cultural environment and the natural vegetation. This is especially true for high altitude ecosystems, such as the world's largest alpine ecosystem, the 450,000 km~2 of golf-course-like pastures dominating the southeastern Tibetan Plateau. This ecosystem is widely considered to be natural, but only because of the unawareness of the effects of grazing management and the incorrect assessment of human signals in palaeo proxies. Here we posit the hypothesis that this ecosystem is a human-induced replacement. To test our hypothesis against defined a priori criteria, we 1) monitored vegetation in grazing exclosures; 2) produced floristically complete vegetation records; 3) compared the vegetation records with data of the nearest climate stations; 4) surveyed forest and experimental reforestation trials with endemic tree species; 5) analyzed pollen and re-evaluated published pollen diagrams; and 6) integrated these results with palaeopedological and anthracological results of previous studies. The results of long-term grazing exclosure experiments, the prevalence of grazing-adapted plant functional types, the occurrence of isolated vigorous forests in "alpine" pastures, and the successful reforestation trials in presently treeless pastures together suggest that dominant pastures replaced forests in the montane belt and tall grassland in the alpine belt. The spatial and temporal coincidence of palaeosols and archaeological sites with tree species charcoal, the decline in forest pollen during the mid-Holocene climatic optimum, and the first appearance of human indicator pollen are most parsimoniously explained by the early presence of foragers and pastoralists. The onset of pastoralism in the Tibetan Highlands is presumed to date from the 8th millennium BP.
机译:第四纪科学对人类环境的形成进行了激烈的辩论。对人类足迹的感知需要了解当前文化环境与自然植被之间的对比。对于高原生态系统(例如世界上最大的高山生态系统,占青藏高原东南部的450,000 km〜2高尔夫球场式牧场)尤其如此。人们普遍认为该生态系统是自然的,但这仅是由于不了解放牧管理的影响以及对古近代人类信号的不正确评估。在这里,我们提出这样一个假设,即该生态系统是人为替代。为了对照定义的先验标准检验我们的假设,我们:1)在放牧场所监测植被; 2)产生了植物区系完整的植被记录; 3)将植被记录与最近的气候站的数据进行比较; 4)进行森林调查和使用特有树种的实验性造林试验; 5)分析花粉并重新评估已发布的花粉图; 6)将这些结果与先前研究的古生物学和人类学结果相结合。长期放牧试验的结果,适应放牧的植物功能类型的流行,“高山”牧场中孤立茂盛的森林的发生以及目前无树牧场的成功造林试验共同表明,优势牧场取代了该地区的森林山地带和高山带中的高草原。早期觅食者和牧民的出现可以最简洁地解释古土壤和考古地点与树木木炭的时空一致性,全新世中期最佳气候期间森林花粉的减少以及人类指示花粉的首次出现。据推测,西藏高地牧民的起源可追溯到公元八千年。

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