干旱区生态环境知识资源中心(Arid): Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)

Arid

DOI	10.4000/geomorphologie.17247
	Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
	Beuzen-Waller, Tara; Desruelles, Stephane; Marrast, Anais; Giraud, Jessica; Gernez, Guillaume; Forman, Steven; Beshkani, Amir; Bonilauri, Stephanie; Lemee, Marion; Nacarro, Hugo; Fouache, Eric
通讯作者	Beuzen-Waller, T
来源期刊	GEOMORPHOLOGIE-RELIEF PROCESSUS ENVIRONNEMENT
ISSN	1266-5304
EISSN	1957-777X
出版年	2022
卷号	28 期号:4 页码:223-239
英文摘要	In Oman, quaternary climatic fluctuations alternated between humid and arid periods. Humid periods are a key component in landscape evolution and the history of early human-environment interactions, as they allowed for less-restrictive arid conditions by triggering increasing rainfall and fluvio-lacustrine activity. Fluvial archives are of great interest for understanding hydrosystems' local responses to quaternary regional climatic fluctuations. For the end of the Pleistocene and the Holocene, little data are available in Northern Oman to examine this topic and to compare it with archaeological site distribution and subsistence strategies, in particular with regard to water resources. Here, we will present fluvial records from a small wadi called Wadi Dishshah, located in the southern part of the Hajar Mountains' piedmont, near the Salakh Arch area. The study of the Wadi Dishshah relies on topographic surveys (aerial survey with drone), geomorphological mapping, morphostratigraphic analyses of natural and excavated sections, malacological analyses and age-dating using OSL and radiocarbon methods. Three phases of aggradation have been identified: the first one between 26,500 cal. BP and 11,300 cal. BP, a second between 6,200 cal. BP and 5,500 cal. BP and a late one around 2,800 cal. BP. The fluvial records from the Wadi Dishshah and its hydro-climatic significance are compared to the distribution of archaeological sites from the Salakh Arch area to discuss the relations between settlement strategies and surface flows. This work is the first case study of late Pleistocene - Holocene alluvial formations in this region of Oman.
英文关键词	Fluvial archives Pluvial periods Geoarchaeology Hajar Mountains Oman
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000990019700003
WOS关键词	SAUDI-ARABIA ; PLUVIAL PHASE ; NORTHERN OMAN ; HUMID PERIOD ; OASIS ; INTERIOR ; DEPOSITS ; YEMEN ; LAKE ; IRRIGATION
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/2XILL650/392942
推荐引用方式 GB/T 7714	Beuzen-Waller, Tara,Desruelles, Stephane,Marrast, Anais,et al. Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)[J],2022,28(4):223-239.
APA	Beuzen-Waller, Tara.,Desruelles, Stephane.,Marrast, Anais.,Giraud, Jessica.,Gernez, Guillaume.,...&Fouache, Eric.(2022).Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman).GEOMORPHOLOGIE-RELIEF PROCESSUS ENVIRONNEMENT,28(4),223-239.
MLA	Beuzen-Waller, Tara,et al."Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)".GEOMORPHOLOGIE-RELIEF PROCESSUS ENVIRONNEMENT 28.4(2022):223-239.