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Paleoenvironmental catastrophies on the Peruvian coast revealed in lagoon sediment cores from Pachacamac

机译:秘鲁海岸的古环境灾难在Pachacamac的泻湖沉积物核中揭示

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Paleoenvironmental reconstruction combining data from diatom, pollen, macrophytic, and archaeologicalanalyses had not been attempted previously for coastal Peru. We analyzed two radiocarbondatedsediment cores extracted from the “sacred” Urpi Kocha Lagoon at the pre-Hispanic religiouscenter of Pachacamac (ca. AD 350-1533), near Lima, to characterize the paleoenvironment of the site.The data reveal an environmental history characterized by alternating periods of severe drought andcatastrophic flood. Recurrent pulses with distinctive sediment, diatom, pollen, and macrophyticcharacteristics reflecting variations in water depth, substrate, turbidity and salinity, usually containa thick basal sandy storm deposit overlain by thin organic accumulations of peat, gyttja, and snails. Themost intense of these disturbance pulses, when correlated with pollen, plant macrofossils, radiocarbondates, and regional proxy data, provide local evidence of four major floods associated with sustained,catastrophic El Ni?o events, tsunamis and/or severe storms in the Andean highlands over the last 2000 years.
机译:秘鲁沿海地区以前从未尝试过结合硅藻,花粉,大植物和考古分析数据进行古环境重建。我们分析了从利马附近帕查卡马克(Pachacamac)前西班牙宗教中心(约公元350-1533年)的“神圣”乌尔比·科恰泻湖中提取的两个放射性碳酸盐岩沉积核,以表征该地点的古环境。数据揭示了以严重干旱和灾难性洪水的交替时期。周期性脉冲具有独特的沉积物,硅藻,花粉和宏观植物特征,反映了水深,底物,浊度和盐度的变化,通常包含厚厚的基底沙尘暴沉积物,其上覆盖着泥炭,gytja和蜗牛的薄薄有机物。这些干扰脉冲中最强烈的干扰脉冲,与花粉,植物大化石,放射性碳酸盐和区域代理数据相关联,可提供与安第斯高地持续,灾难性的厄尔尼诺事件,海啸和/或严重风暴有关的四次主要洪水的本地证据。在过去的2000年中。

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