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Late Pleistocene palaeolake in the interior of Oman: A potential key-area for the dispersal of anatomically modern humans out-of-Africa?
Stockholm University, Faculty of Science, Department of Physical Geography and Quaternary Geology.
2012 (English)In: Journal of Quaternary Science, ISSN 0267-8179, E-ISSN 1099-1417Article in journal (Refereed) Published
Abstract [en]

Relict fluvial and lacustrine deposits in the interior of Oman near Saiwan consist of waterlain brecciaswith pebble imbrications and current ripples, covered by algal laminites containing calcified reeds and charcoalpieces. Geomorphological evidence suggests that the palaeolake covered a maximum surface of 1400 km2 and had amaximum depth of about 25 m. Optically stimulated luminescence (OSL) and thermally transferred OSL datingindicate that this palaeolake existed sometime between 132 and 104 ka. The rich archaeological evidence in the areasuggests substantial human occupation, possibly at the time when Palaeolake Saiwan existed. Interestingly, the lithictraditions of the archaeological material show no clear relation to coeval findings from neighbouring areas, putting aquestion mark on the origin of the culture found at Saiwan. This finding raises questions concerning the origin of thepopulation inhabiting Saiwan, as the site lies along one possible route for the dispersal of anatomically modern humansout-of-Africa.

Place, publisher, year, edition, pages
2012.
Keyword [en]
Anatomically modern humans; OSL; Palaeolake; Saiwan; TT-OSL.
National Category
Geosciences, Multidisciplinary
Research subject
Quarternary Geology
Identifiers
URN: urn:nbn:se:su:diva-85256OAI: oai:DiVA.org:su-85256DiVA: diva2:583162
Available from: 2013-01-07 Created: 2013-01-07 Last updated: 2017-12-06Bibliographically approved

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