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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Salinity episodes and their reversal in the late pliocene of south-western Australia
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Salinity episodes and their reversal in the late pliocene of south-western Australia

机译:西南澳大利亚晚新世的盐度事件及其逆转

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摘要

Fossil pollen and grain size analysis of sediments from Yallalie in south-western Australia is used to reconstruct the history of salinization and aridity of the region between 2.63 and 2.56 Ma. Three well-defined episodes of aridity are defined by a reduction in humid woodland and expansion of chenopod shrubland around 2.59, 2.56 and 2.558 Ma. Each episode lasted an estimated 2-3000 years. The grain size data supports the general aridity conclusion but also demonstrates there was a large amount of environmental variability, especially between about 2.59 and 2.56 Ma, which included short term wetting and drying cycles. These cycles are at sub-Milankovitch time scales and suggest that the vegetation patterns show much more inertia to change than do the sediment dynamics. The general pattern of change at Yallalie is similar to that revealed in the Chinese Loess and Red Clay sequence but the detail of change is much greater in the lake sediment than revealed for the aeolian sediment of central Asia. (c) 2005 Elsevier B.V. All rights reserved.
机译:来自澳大利亚西南部Yallalie的沉积物的化石花粉和粒度分析用于重建2.63至2.56 Ma之间区域的盐渍化和干旱历史。通过在2.59、2.56和2.558 Ma附近减少潮湿的林地和扩大chenopod灌木林,定义了三个明确的干旱时期。每个事件持续了大约2-3000年。晶粒度数据支持一般的干旱结论,但也表明存在很大的环境变异性,特别是在约2.59和2.56 Ma之间,其中包括短期润湿和干燥周期。这些周期处于亚米兰科维奇时间尺度以内,这表明与沉积动力学相比,植被格局显示出更多的惯性变化。 Yallalie的一般变化模式与中国黄土和红粘土序列中揭示的变化模式相似,但湖泊沉积物中变化的细节要比中亚风沙沉积物更为明显。 (c)2005 Elsevier B.V.保留所有权利。

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