Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.geomorph.2007.03.015 |
Rock varnish microlamination dating of late Quaternary geomorphic features in the drylands of western USA | |
Liu, Tanzhuo; Broecker, Wallace S. | |
通讯作者 | Liu, Tanzhuo |
来源期刊 | GEOMORPHOLOGY
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ISSN | 0169-555X |
EISSN | 1872-695X |
出版年 | 2008 |
卷号 | 93期号:3-4页码:501-523 |
英文摘要 | Varnish microlamination (VML) dating is a correlative age determination technique that can be used to date and correlate various geomorphic features in deserts. In this study, we establish a generalized late Quaternary (i.e., 0-300 ka) varnish layering sequence for the drylands of western USA and tentatively correlate it with the SPECMAP oxygen isotope record. We then use this climatically correlated varnish layering sequence as a correlative dating tool to determine surface exposure ages for late Quaternary geomorphic features in the study region. VML dating of alluvial fan deposits in Death Valley of eastern California indicates that, during the mid to late Pleistocene, 5-15 ky long aggradation events occurred during either wet or dry climatic periods and that major climate shifts between glacial and interglacial conditions may be the pacemaker for alteration of major episodes of fan aggradation. During the Holocene interglacial time, however, 0.5-1 ky long brief episodes of fan deposition may be linked to short periods of relatively wet climate. VML dating of alluvial desert pavements in Death Valley and the Mojave Desert reveals that pavements can be developed rapidly (< 10 ky) during the Holocene (and probably late Pleistocene) in the and lowlands (< 800 m msl) of these regions; but once formed, they may survive for 74-85 ky or even longer without being significantly disturbed by geomorphic processes operative at the pavement surface. Data from this study also support the currently accepted, "being born at the surface" model of desert pavement formation. VML dating of colluvial boulder deposits on the west slope of Yucca Mountain, southern Nevada, yields a minimum age of 46 ka for the emplacement of these deposits on the slope, suggesting that they were probably formed during the early phase of the last glaciation or before. These results, combined with those from our previous studies, demonstrate that VML dating has great potential to yield numerical age estimates for various late Quaternary geomorphic features in the western USA drylands. (c) 2007 Elsevier B.V. All rights reserved. |
英文关键词 | rock varnish VML dating alluvial fan colluvial boulder deposit desert pavement wet event late Quaternary western USA |
类型 | Review |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000255899700022 |
WOS关键词 | CIMA-VOLCANIC-FIELD ; EASTERN MOJAVE DESERT ; COLLUVIAL BOULDER DEPOSITS ; ALLUVIAL-FAN SURFACES ; RELATIVE-AGE METHODS ; DEATH-VALLEY ; LATE PLEISTOCENE ; CLIMATE-CHANGE ; LANDSCAPE EVOLUTION ; FLUVIAL TERRACES |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/157432 |
作者单位 | Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA |
推荐引用方式 GB/T 7714 | Liu, Tanzhuo,Broecker, Wallace S.. Rock varnish microlamination dating of late Quaternary geomorphic features in the drylands of western USA[J],2008,93(3-4):501-523. |
APA | Liu, Tanzhuo,&Broecker, Wallace S..(2008).Rock varnish microlamination dating of late Quaternary geomorphic features in the drylands of western USA.GEOMORPHOLOGY,93(3-4),501-523. |
MLA | Liu, Tanzhuo,et al."Rock varnish microlamination dating of late Quaternary geomorphic features in the drylands of western USA".GEOMORPHOLOGY 93.3-4(2008):501-523. |
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