2015
DOI: 10.1016/j.quascirev.2015.03.025
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Nile behaviour and Late Palaeolithic humans in Upper Egypt during the Late Pleistocene

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Cited by 70 publications
(47 citation statements)
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“…To date, there is little consensus on the behavior of the late Pleistocene Nile, particularly for the main Nile during the last glacial maximum (LGM). Several models have been proposed, including a highly braided river with a much‐reduced discharge, a suspended‐load river, and that sand dunes dammed the Nile at specific places during the LGM, creating large lakes . Further south, in Sudan, correlation between Nile flows and sapropel S2 suggests a time of high water influx to the main Nile at ~55 ka, while during the LGM, both the White and the Blue Nile exhibit very low water discharge and high seasonality .…”
Section: Discussion Topicsmentioning
confidence: 99%
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“…To date, there is little consensus on the behavior of the late Pleistocene Nile, particularly for the main Nile during the last glacial maximum (LGM). Several models have been proposed, including a highly braided river with a much‐reduced discharge, a suspended‐load river, and that sand dunes dammed the Nile at specific places during the LGM, creating large lakes . Further south, in Sudan, correlation between Nile flows and sapropel S2 suggests a time of high water influx to the main Nile at ~55 ka, while during the LGM, both the White and the Blue Nile exhibit very low water discharge and high seasonality .…”
Section: Discussion Topicsmentioning
confidence: 99%
“…Only scarce evidence for human presence across the Abydos High Desert landscape dates to the last 70 ka . Conversely, the Nile Valley in Upper and Middle Egypt shows an exceptional increase in the number of sites during the LP . The LP lithic assemblages portray great variability, and some even retain several MP/MSA characteristics, such as the Levallois method .…”
Section: Discussion Topicsmentioning
confidence: 99%
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