Salinity episodes and their reversal in the late pliocene of south-western Australia

被引:8
作者
Dodson, JR [1 ]
Lu, HY
机构
[1] Univ Western Australia, Sch Earth & Geog Sci, Perth, WA 6009, Australia
[2] Brunel Univ, Inst Environm, Uxbridge UB8 9PH, Middx, England
[3] Chinese Acad Sci, Inst Earth Environm, Xian, Shaanxi, Peoples R China
基金
澳大利亚研究理事会;
关键词
salinity; dust load; climate change; pliocene; SW Australia;
D O I
10.1016/j.palaeo.2005.06.006
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
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.
引用
收藏
页码:296 / 304
页数:9
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