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- W1982481921 abstract "New age estimates for samples representing different sedimentary units of the coastal ridges along El-Omayid-Burg El-Arab, northwestern coast of Egypt reveal that the Coastal (first) ridge is related to Holocene high sea level, aminozone “A”, with evidence of recent (0.6±0.1 ka) ooid contributions. The El-Max-Abu Sir (second) ridge appears to be associated with the Last Interglacial and related to Oxygen Isotope Substages (OIS) 5c/5a. Beach boulders at the bottom of the Gebel Maryut (third) ridge are related to the Last Interglacial high-stand (OIS 5e), while the molluscan and Cardium limestones are related to a Cardium beach of lagoonal to shallow marine environment. This beach represents a coastal barrier, which existed between 208±59 to 292±48 ka, and is related to aminozones F-G and OIS 7-9. Complex paleosols are developed on the northern flanks of both the second and the third ridges with an estimate age of 67±31 ka and aminozone “C”. These appear related to interstadial conditions at the early Last Glacial Stage. The paleosols (Pink limestone) at the top of the Khashm El-Ish (fourth) ridge show a wide range of ages, giving age estimates between 360±140 and 584±317 ka indicating a Middle Pleistocene age." @default.
- W1982481921 created "2016-06-24" @default.
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- W1982481921 date "2000-07-01" @default.
- W1982481921 modified "2023-09-26" @default.
- W1982481921 title "Quaternary shoreline development: the northwestern coast of Egypt" @default.
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- W1982481921 doi "https://doi.org/10.1016/s0277-3791(99)00097-9" @default.
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