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首页> 外文期刊>Journal of Palaeogeography >Distributional patterns of anemophilous tree pollen indicating the pathways of Indian monsoon through Qinghai–Tibetan Plateau
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Distributional patterns of anemophilous tree pollen indicating the pathways of Indian monsoon through Qinghai–Tibetan Plateau

机译:指示印度季风穿过青藏高原的风化花粉的分布模式

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The distribution pattern of vegetation on Qinghai–Tibetan Plateau is fundamentally influenced by the plateau climate, which is mainly controlled by Indian monsoon during summer. The long distance transportation of pollen (mostly anemophilous taxa) produced by trees on the plateau has been recorded by modern pollen samples in previous studies, and hypothesized to be a good indicator of monsoon dynamics. Here we use 270 surface pollen samples from Qinghai–Tibetan Plateau to test the distribution patterns of the anemophilous tree pollen. Meanwhile factors related to Indian monsoon affecting pollen transportation are simulated and analyzed. Results show that depositional patterns of anemophilous tree pollen, especially Abies , Pinus , Quercus and Betula are completely controlled by the pathways of Indian monsoon. This is reflected by climatic indicators of the atmospheric pressure pattern over June–July–August, by the precipitation pattern over June–July–August and by the topographic feature of the plateau. The spatial interpolation of thin plate spline results also display two depositional centers ( ca . 30°N, 95°E and 30°N, 105°E) of the anemophilous tree pollen. In contrast to previous conclusion that pollen distributional pattern is determined by mean annual precipitation, we argue that Indian monsoon is the essential controller because of the synchronization between timing of monsoon wind and timing of plants flowering. Our finding strongly suggests that distributional pattern of anemophilous tree pollen on the plateau is a good proxy of Indian monsoon.
机译:青藏高原的植被分布格局从根本上受高原气候的影响,高原气候主要受夏季的印度季风控制。在以前的研究中,现代花粉样品已记录了高原树木产生的花粉(主要是嗜性类群)的长距离运输,并被认为是季风动力学的良好指标。在这里,我们使用来自青藏高原的270个表面花粉样本来测试嗜性树花粉的分布模式。同时对与印度季风有关的影响花粉运输的因素进行了模拟分析。结果表明,印度季风的路径完全控制了嗜性树木花粉的沉积方式,尤其是冷杉,松,栎和桦。 6月至7月至8月的大气压力模式的气候指标,6月至7月至8月的降水模式以及高原的地形特征反映了这一点。薄板样条曲线结果的空间插值还显示了风化树花粉的两个沉积中心(大约30°N,95°E和30°N,105°E)。与以前的花粉分布模式是由年均降水量决定的结论相反,我们认为印度季风是主要的控制者,因为季风风的时机与植物开花的时机同步。我们的发现有力地表明,高原上的嗜性树花粉的分布模式是印度季风的良好代表。

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