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Dababiya Egypt

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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 61–92.
... has been paid to the biostratigraphy of this area. This work describes the planktonic foraminiferal biostratigraphy of the upper Paleocene-lower Eocene composite stratigraphic section at Dababiya, ~23km south of Luxor in the upper Nile Valley (Egypt) which includes the recently designated Global...
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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): 105–122.
...William A. Berggren; Khaled Ouda Abstract We describe the upper Paleocene-lower Eocene planktonic foraminiferal biostratigraphy at Qreiya (southeastern exposure of Gebel Abu Had), about 50km ENE of Qena, Egypt. The ~54m thick section spans the Tarawan Chalk (~8.6m thick; Zone P4a+b) and the Esna...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 93–104.
... of monotonous, poorly fissile, olive-gray mudstone. However, the basal ~ 1.6m consist of dark to medium gray, variably fissile and phosphatic mudstone. This lithologically distinctive unit extends over a large part of Egypt and has been given the name ‘Dababiya Quarry Beds’ (Dupuis et al. 2003, chapter 3...
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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): 167–178.
... of the Dababiya section, Upper Nile Valley (Egypt) . Micropaleontology , volume 49 , supplement no. 1 , chapter 4, this volume. BERGGREN , W.A. , 2003 . Upper Paleocene-lower Eocene planktonic foraminiferal biostratigraphy of the Qreiya section, Upper Nile Valley (Egypt) . Micropaleontology...
FIGURES
Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2010
DOI: 10.2110/sepmsp.094.167
EISBN: 9781565762985
...), 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 onset of the CIE is somewhat...
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Journal Article
Journal: Geology
Published: 17 April 2021
Geology (2021) 49 (8): 993–998.
... the Dababiya Quarry Member of Egypt dating to the PETM. This assemblage—Ras Gharib A—is a snapshot of a time when tropical sea-surface temperatures approached limits lethal for many modern fishes. Despite extreme conditions, the Ras Gharib A fauna is compositionally similar to well-known, midlatitude...
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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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Image
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 June 2003
Micropaleontology (2003) 49 (Suppl_1): 1–13.
...M. M. Youssef Abstract The general tectonic framework of Egypt can be described in simple terms as comprising three units that have controlled the sedimentological history and the structural make up of the country; These are the Arabian-Nubian massif, the stable shelf and the unstable shelf...
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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 March 2013
Journal of the Geological Society (2013) 170 (2): 341–352.
... 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 ) and from central Sinai (Abu Zenima and Gebel...
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Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (3): 193–222.
... in the southern part of the Western Desert, Eastern Desert, Nile Valley, Safaga-Quseir region along the Red Sea coast and Sinai ( Hermina et al. 1989 ; see review in Ouda 2004). Recently the Dababiya section, 23km south of Luxor, Egypt, was chosen as the Global Standard Stratotype-section and Point (GSSP...
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Journal Article
Published: 01 September 2011
Journal of Micropalaeontology (2011) 30 (2): 167–182.
... Geology , 181 : 131 – 146 . Ernst S.R. Guasti E. Dupuis C. Speijer R.P. 2006 . Environmental perturbation in the southern Tethys across the Paleocene/Eocene boundary (Dababiya, Egypt): Foraminiferal and clay mineral records . Marine Micropaleontology , 60 : 89...
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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: 28 September 2016
Proceedings of the Yorkshire Geological Society (2016) 61 (2): 134–147.
... . Metropolitan Museum Journal , 26 , 5 – 48 . Aubry , M.-P. & Salem , R. 2012 . The Dababiya Core: A Window into Paleocene to Early Eocene depositional history in Egypt based on coccolith stratigraphy . In: Berggren , W.A. & Ouda , Kh. (eds) Early Paleogene history...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 123–138.
... Group on the Paleocene/Eocene Boundary , 2002 . 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...
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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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