Seong, Yeong Bae Dorn, Ronald I. Yu, Byung Yong 2024-01-20T03:02:55Z 2024-01-20T03:02:55Z 2021-09-04 2016-11 0012-8252 https://pubs.kist.re.kr/handle/201004/123519 This paper integrates prior scholarship on desert pavements with a case study of pavements on stream terraces in the Sonoran Desert to analyze the processes and site conditions that facilitate the survival of ancient desert pavements. This synthesis identifies vital factors, key factors, and site-specific factors promoting pavement stability. Hyperaridity is the vital factor in pavements surviving for 10(6) years or more, aided by minimal bioturbation and clast-size reduction. Three key factors aid in pavements surviving for 10(4) to 10(5) years: accumulation of allochthonous dust underneath pavement cobbles; a flat topography; and a lack of headward retreating swales or gullies. A unified explanation for pavement longevity, however, did not emerge from a literature review, because a variety of site-specific factors can also promote pavement antiquity including: resistant bedrock beneath the pavement; disk-shaped cobbles to promote dust accumulation; and rnicroclimatological and ecological reasons for minimal bioturbation. Both key and site-specific explanations for pavement longevity apply well to a case study of pavements on stream terraces in the Sonoran Desert, central Arizona. The buildup of cosmogenic Be-10 and in situ C-14, optically stimulated luminescence and varnish microlamination ages reveal stable pavements range in age between similar to 30 and 332 ka with conditions for longevity including: flat surface topography; pavements underlain by consolidated granitic bedrock; a lack of headward-retreating gullies and swales; (87)sr/(86)sr analyses indicating the infiltration of allochthonous dust floating disk-shaped pavement cobbles; and a quartzite lithology resistant to disintegration. However, Be-10 ages also indicate evidence for the instability of desert pavements on stream terraces underlain by unconsolidated playa clays and unconsolidated fanglomerate; these weaker materials allowed the growth of headward-retreating swales, that in turn promoted exposure of newer gravels by surface erosion. (C) 2016 Elsevier B.V. All rights reserved. English ELSEVIER ALLUVIAL-FAN SURFACES CIMA-VOLCANIC-FIELD SITU COSMOGENIC C-14 EASTERN LIBYAN PLATEAU HOLOCENE ROCK-VARNISH HE-3 EXPOSURE AGES DRY VALLEYS REGION MOJAVE-DESERT ATACAMA DESERT LANDSCAPE EVOLUTION Evaluating the life expectancy of a desert pavement Article 10.1016/j.earscirev.2016.08.005 1 EARTH-SCIENCE REVIEWS, v.162, pp.129 - 154 EARTH-SCIENCE REVIEWS 162 129 154 scie scopus 000388776700008 2-s2.0-84988976633 Geosciences, Multidisciplinary Geology Review ALLUVIAL-FAN SURFACES CIMA-VOLCANIC-FIELD SITU COSMOGENIC C-14 EASTERN LIBYAN PLATEAU HOLOCENE ROCK-VARNISH HE-3 EXPOSURE AGES DRY VALLEYS REGION MOJAVE-DESERT ATACAMA DESERT LANDSCAPE EVOLUTION Cosmogenic nuclides Geomorphology Landform evolution Quaternary Soils