2003
DOI: 10.1007/bf03043306
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High-resolution ostracode records of the paleocene/eocene transition in the South Eastern Desert of Egypt — Taxonomy, biostratigraphy, paleoecology and paleobiogeography

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Cited by 17 publications
(34 citation statements)
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“…Alocopocythere ramalia are considered to be middle neritic dwellers, which suggest that their disappearance is due to a rise in sea level (Morsi and Speijer, 2003). The same ostracod assemblage was recorded in the South Eastern Desert, indicating an outer shelf-bathyal environment (Morsi and Speijer, 2003). The Paleocene of the Safaga area yielded a similar ostracod assemblage, which is considered to indicate middle-outer neritic environment (Ismail and Ied, 2005).…”
Section: Paleoenvironmentsmentioning
confidence: 83%
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“…Alocopocythere ramalia are considered to be middle neritic dwellers, which suggest that their disappearance is due to a rise in sea level (Morsi and Speijer, 2003). The same ostracod assemblage was recorded in the South Eastern Desert, indicating an outer shelf-bathyal environment (Morsi and Speijer, 2003). The Paleocene of the Safaga area yielded a similar ostracod assemblage, which is considered to indicate middle-outer neritic environment (Ismail and Ied, 2005).…”
Section: Paleoenvironmentsmentioning
confidence: 83%
“…This assemblage is a combination of the South Tethyan Type (STT) and Esna Type (EST), indicating a transitional environment from middle shelf to outer shelf (Bassiouni and Luger, 1990). Alocopocythere ramalia are considered to be middle neritic dwellers, which suggest that their disappearance is due to a rise in sea level (Morsi and Speijer, 2003). The same ostracod assemblage was recorded in the South Eastern Desert, indicating an outer shelf-bathyal environment (Morsi and Speijer, 2003).…”
Section: Paleoenvironmentsmentioning
confidence: 92%
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