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Dababiya Egypt

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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 61-92.
... at Dababiya, ~23km south of Luxor in the upper Nile Valley (Egypt) which includes the recently designated Global Standard Stratotype-section and Point (GSSP) of the Paleocene/Eocene boundary. The measured ~130m thick (composite) section, extends from the Tarawan Chalk through the Esna Shale (>120m thick...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 41-59.
... lithostratigraphic unit in a typical succession of five characteristic beds that can be followed throughout Upper Egypt, and at the base of which the GSSP is defined. We formally describe this unit as the Dababiya Quarry Beds at the same time as we subdivide the Esna Shale Formation into three formal...
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Journal Article
Published: 01 December 2006
Micropaleontology (2006) 52 (5): 433-447.
... in the outer neritic Dababiya section (Egypt), the Global Stratotype Section and Point (GSSP) for the P/E boundary, is of great importance for correlation with other P/E boundary sites. We illustrate the 46 most representative benthic foraminiferal taxa (belonging to 27 genera) in order to compare the taxonomy...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 93-104.
..., Dababiya and at other localities in central Egypt also displays features that have been documented from the CIE interval in Paleocene/Eocene boundary marine sections in many parts of the world (e.g., Norris and Röhl 1999 ; Bains et al. 1998 ; Bowen et al. 2001 ). These features include the occurrence...
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Series: SEPM Special Publication
Published: 01 January 2010
DOI: 10.2110/sepmsp.094.167
EISBN: 9781565762985
... Section and Point (GSSP), defining the base of the Ypresian Stage (lowest Eocene), located in the Dababiya Quarry near Luxor in Upper Egypt. The base of the Eocene represents the beginning of the Paleocene–Eocene Thermal Maximum (PETM) identified by a negative carbon isotope (δ 13 C) excursion. While...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 105-122.
... the top of the CIE-interval (sample Qb 18.5). Globanomalina pseudomenardii has a similar distribution pattern in the G. Owaina ( Ouda et al. 2003 , chapter 9, this volume) and Dababiya ( Berggren and Ouda 2003 , chapter 4, this volume) sections as well as in several other sections in Egypt ( Speijer...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 167-178.
...; Dababiya:, Berggren and Ouda 2003 , chapter 4; Qreiya: Berggren and Ouda 2003 , chapter 6, this volume). A slightly earlier occurrence of Ig. broedermanni and Ac. esnaensis is was expected between samples AG 7 and AG 6, based on the LO of Ac. angulos a 50-to 60cm above. Elsewhere in Egypt the LOs...
FIGURES
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 147-166.
...; the sections are thus considerably less complete than at Dababiya, ~25km to the north. The recently revised Paleocene/Eocene boundary is located in both sections within the lower part of the Esna Shale at ~12m and 16.3m, respectively, above the base of the Esna Shale. The CIE-interval is reduced in both...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 139-146.
...Dennis V. Kent; Christian Dupuis Abstract A paleomagnetic study of the Paleocene-Eocene Esna Shale and Tarawan Chalk at the Dababiya and Qreiya sections near Luxor in central Egypt reveals stable normal and reverse polarity magnetizations. However, these (neritic) pelagic marine sediments have...
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Location of <b>Dababiya</b> (D) and Qreiya (Q) sampling localities in central Egyp...
Published: 01 June 2003
TEXT-FIGURE 1 Location of Dababiya (D) and Qreiya (Q) sampling localities in central Egypt.
Journal Article
Published: 01 December 2013
Clays and Clay Minerals (2013) 61 (6): 551-565.
... and fossil contents of Qaret El-Muluk Formation at Wadi El Natrun Depression, Western Desert, Egypt . Facies , 37 , 211 – 224 . Ernst S.R. Guasti E. Dupuis C. Speijer R.P. ( 2006 ) Environmental perturbation in the southern Tethys across the Paleocene/Eocene boundary (Dababiya...
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Journal Article
Published: 28 September 2016
Proceedings of the Yorkshire Geological Society (2016) 61 (2): 134-147.
... Formation is not known on the West Bank, but can be seen c. 35 km SE in the Dababiya Quarry where the Tarawan Chalk Formation reaches a thickness of 15 – 20 m ( Dupuis et al. 2003 ). Table 1. Upper Paleocene-Lower Eocene lithostratigraphical succession in Upper Egypt and thicknesses in the West...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 1-13.
... characteristics along these wrench belts are more or less correlatable in both style and age. TEXT-FIGURE 6 Geological map of the Dababiya area. (After Omara et al. 1972 ) TEXT-FIGURE 1 Rosette diagrams showing the major tectonic trends of Egypt (After Meshref 1990 ). REFERENCES...
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Journal Article
Published: 01 March 2013
Journal of the Geological Society (2013) 170 (2): 341-352.
... . 2007 ). Replicate analyses indicated a precision better than 5%. In addition, P tot analyses were performed on several other sections from the central Eastern Desert of Egypt (e.g. Gebel Duwi, Bolle et al . (2000) ; Dababiya Global Stratotype Section and Point (GSSP), Dupuis et al . 2003...
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Journal Article
Published: 01 January 2007
Micropaleontology (2007) 53 (1-2): 127-144.
... is considered one of the most complete sections across the K/P boundary in Egypt where all the exposed rocks at G. El Keeh belong to the lower Eocene Egma Formation. A nearly complete sucession of Paleocene nannofossil biozones is recorded from the Esna Formation at G. El Mishiti. They are arranged from base...
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Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2424(03)
... continuously well-exposed outcrops and well-preserved material for micropaleontological research. For these reasons, the global boundary stratotype section and point (GSSP) for the Paleocene-Eocene boundary has recently been defined in Egypt within the Dababiya Quarry section, near Luxor in the Nile Valley...
Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (3): 193-222.
... to eutrophic environment. A similar pattern was observed in the uppermost part of the CIE interval in Dababiya section, Southern Egypt ( Dupuis et al. 20003 ), Alemadilla section, Spain ( Monechi et al. 2000b ) and ODP Site 690, Southern high latitudes ( Bralower 2002 ) DSDP Sites 213, Indian Ocean and 401...
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Journal Article
Published: 01 September 2011
Journal of Micropalaeontology (2011) 30 (2): 167-182.
... rare. In this study, we focus on the micropalaeontology (calcareous nannofossils and benthic foraminifera), mineralogy and trace element geochemistry of the LDE in the Qreiya 3 section from the southern Tethyan margin in Egypt. In this section, the LDE is characterized by the occurrence of anomalous...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 15-40.
...Khaled Ouda Abstract The search for a Global Standard Stratotype-section and Point (GSSP) for the Paleocene/Eocene boundary has resulted in several concurrent studies of the Upper Paleocene-Lower Eocene interval in sections across Egypt from the Eastern and Western Deserts to Upper Egypt where...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 123-138.
... . Proposal: Global Stratotype-section and Point (GSSP) at the Dababiya section (Egypt) for the Base of the Eocene Series . International Subcommission on Paleogene Stratigraphy, Internal Report , 58 pp. BALASHOV , Y.A. , RONOV , A.B. , MIGDISOV , A.A. , and TURANSKAYA , N.V. , 1964...
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