Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)

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-lac...

وصف كامل

محفوظ في:
التفاصيل البيبلوغرافية
المؤلف الرئيسي: Desruelles, Stéphane (author)
مؤلفون آخرون: Beuzen-Waller, Tara (author), Marrast, Anaïs (author), Fouache, Eric (author), Giraud, Jessica (author), Gernez, Guillaume (author), Beshkani, Amir (author), Bonilauri, Stéphanie (author), Lemée, Marion (author), Nacarro, Hugo (author)
منشور في: 2022
الموضوعات:
الوصول للمادة أونلاين:https://journals.openedition.org/geomorphologie/17247
https://depot.sorbonne.ae/handle/20.500.12458/1333
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author Desruelles, Stéphane
author2 Beuzen-Waller, Tara
Marrast, Anaïs
Fouache, Eric
Giraud, Jessica
Gernez, Guillaume
Beshkani, Amir
Bonilauri, Stéphanie
Lemée, Marion
Nacarro, Hugo
author2_role author
author
author
author
author
author
author
author
author
author_facet Desruelles, Stéphane
Beuzen-Waller, Tara
Marrast, Anaïs
Fouache, Eric
Giraud, Jessica
Gernez, Guillaume
Beshkani, Amir
Bonilauri, Stéphanie
Lemée, Marion
Nacarro, Hugo
author_role author
dc.creator.none.fl_str_mv Desruelles, Stéphane
Beuzen-Waller, Tara
Marrast, Anaïs
Fouache, Eric
Giraud, Jessica
Gernez, Guillaume
Beshkani, Amir
Bonilauri, Stéphanie
Lemée, Marion
Nacarro, Hugo
dc.date.none.fl_str_mv 2022-11-25T06:55:13Z
2022-11-25T06:55:13Z
2022
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv 10.4000/geomorphologie.17247
https://journals.openedition.org/geomorphologie/17247
https://depot.sorbonne.ae/handle/20.500.12458/1333
dc.language.none.fl_str_mv en
dc.relation.none.fl_str_mv Geomorphologie: Relief, Processus, Environnement
dc.subject.none.fl_str_mv Fluvial archives
Pluvial periods
Geoarchaeology
Hajar Mountains
Oman Archives fluviales
Périodes humides
Géoarchéologie
Jebel Hajar
Oman Relief, Processus, Environnement
dc.title.none.fl_str_mv Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
dc.type.none.fl_str_mv Controlled Vocabulary for Resource Type Genres::text::periodical::journal::contribution to journal::journal article
description 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.
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network_name_str Sorbonne University Abu Dhabi repository
oai_identifier_str oai:depot.sorbonne.ae:20.500.12458/1333
publishDate 2022
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spelling Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)Desruelles, StéphaneBeuzen-Waller, TaraMarrast, AnaïsFouache, EricGiraud, JessicaGernez, GuillaumeBeshkani, AmirBonilauri, StéphanieLemée, MarionNacarro, HugoFluvial archivesPluvial periodsGeoarchaeologyHajar MountainsOman Archives fluvialesPériodes humidesGéoarchéologieJebel HajarOman Relief, Processus, EnvironnementIn 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.2022-11-25T06:55:13Z2022-11-25T06:55:13Z2022Controlled Vocabulary for Resource Type Genres::text::periodical::journal::contribution to journal::journal articleapplication/pdf10.4000/geomorphologie.17247https://journals.openedition.org/geomorphologie/17247https://depot.sorbonne.ae/handle/20.500.12458/1333enGeomorphologie: Relief, Processus, Environnementoai:depot.sorbonne.ae:20.500.12458/13332022-11-25T18:00:25Z
spellingShingle Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
Desruelles, Stéphane
Fluvial archives
Pluvial periods
Geoarchaeology
Hajar Mountains
Oman Archives fluviales
Périodes humides
Géoarchéologie
Jebel Hajar
Oman Relief, Processus, Environnement
title Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
title_full Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
title_fullStr Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
title_full_unstemmed Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
title_short Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
title_sort Late Pleistocene-Holocene fluvial records of the Wadi Dishshah: hydro-climatic and archaeological implications (Southern piedmont of the Hajar Mountains, Oman)
topic Fluvial archives
Pluvial periods
Geoarchaeology
Hajar Mountains
Oman Archives fluviales
Périodes humides
Géoarchéologie
Jebel Hajar
Oman Relief, Processus, Environnement
url https://journals.openedition.org/geomorphologie/17247
https://depot.sorbonne.ae/handle/20.500.12458/1333