2012
DOI: 10.1016/j.quaint.2011.04.004
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Mid-Holocene occupation of Egypt and global climatic change

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Cited by 92 publications
(49 citation statements)
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“…Although it cannot be determined to what extent early-and middle-Holocene precipitation in the Fayum exceeded present levels, the presence of now-dry wadi systems along the north shore of the Fayum depression ( Figure 1b) confirms significantly greater rainfall at some point earlier in the Holocene (Phillipps et al, 2012. At this time, we do not have firm evidence whether a northward shift in the summer monsoon or a southward shift in the Mediterranean winter rains was responsible for this increase in precipitation.…”
Section: Hydrology and Paleoclimatementioning
confidence: 96%
“…Although it cannot be determined to what extent early-and middle-Holocene precipitation in the Fayum exceeded present levels, the presence of now-dry wadi systems along the north shore of the Fayum depression ( Figure 1b) confirms significantly greater rainfall at some point earlier in the Holocene (Phillipps et al, 2012. At this time, we do not have firm evidence whether a northward shift in the summer monsoon or a southward shift in the Mediterranean winter rains was responsible for this increase in precipitation.…”
Section: Hydrology and Paleoclimatementioning
confidence: 96%
“…In Upper Egypt, instead, there is a scanty evidence of occupation by hunter-gatherer communities seasonally moving from the Nile to both the Red Sea and the Western Desert oases (Vermeersch 2002). While climatic amelioration in the southern part of Egypt and southward was mainly related to the summer monsoon system, in the northern part of Egypt it seems to have been influenced also by Mediterranean winter rains (Moeyersons et al 1999;Phillipps et al 2012).…”
Section: The Greater Nile Valleymentioning
confidence: 96%
“…Major tributaries of the Nile, like Wadi Melik and Wadi Howar, as well as palaeolakes in southwestern Sudan, ran dry or diminished significantly (Gabriel and Kröpelin 1984;Kröpelin and Soulié-Märsche 1991;Nicoll 2004;Williams et al 2010). At least till around 6 cal kyr BP, Mediterranean rainfall brought wetter conditions in the Fayum, the Delta, the Oases, the Gilf Kebir and the Gebel Uweinat, and most certainly in the northern part of the Egyptian Nile Valley and the Eastern Desert (Phillipps et al 2012;Kröpelin 1987Kröpelin , 2005Moeyersons et al 1999).…”
Section: The Greater Nile Valleymentioning
confidence: 99%
“…The authors in their references do not refer to some other publications (Haas, 1989;Sch€ on, 1996;Jennerstrasse 8 2002;Wendrich et al, 2009;Kindermann 2010;Barich et al, 2012;Phillipps et al, 2012) which have extensive lists of 14 C dates.…”
Section: Contents Lists Available At Sciencedirectmentioning
confidence: 99%