Late Cenomanian ostracod faunas from the area south of Ain Sukhna, western side of the Gulf of Suez, Egypt
Summary: Ostracod faunas from an exposure of the Cenomanian Galala Formation in the area south of Ain Sukhna on the western side of the Gulf of Suez have yielded 11 species belonging to 10 genera. The recorded speciesare have been taxonomically described, discussed where required, and illustrated. T...
| Permalink: | http://skupni.nsk.hr/Record/nsk.NSK01000739846/Details |
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| Matična publikacija: |
Geologia Croatica 62 (2009), 1 ; str. 19-30 |
| Glavni autor: | Boukhary, Mohamed (-) |
| Ostali autori: | Morsi, Abdel-Mohsen M. (-), Eissa, Ragy, Kerdany, Moustafa |
| Vrsta građe: | Članak |
| Jezik: | eng |
| Predmet: | |
| Online pristup: |
Geologia Croatica |
| LEADER | 01756caa a2200337 i 4500 | ||
|---|---|---|---|
| 001 | NSK01000739846 | ||
| 003 | HR-ZaNSK | ||
| 005 | 20121112093734.0 | ||
| 007 | ta | ||
| 008 | 100527s2009 ci ||| ||eng | ||
| 035 | |a (HR-ZaNSK)000739846 | ||
| 040 | |a HR-ZaNSK |b hrv |c HR-ZaNSK |e ppiak | ||
| 042 | |a croatica | ||
| 044 | |a ci |c hr | ||
| 080 | |a 56 |2 MRF 1998. | ||
| 080 | |a 55 |2 MRF 1998. | ||
| 100 | 1 | |a Boukhary, Mohamed | |
| 245 | 1 | 0 | |a Late Cenomanian ostracod faunas from the area south of Ain Sukhna, western side of the Gulf of Suez, Egypt / |c Mohamed Boukhary, Abdel-Mohsen M. Morsi, Ragy Eissa, Moustafa Kerdany. |
| 300 | |b Ilustr. | ||
| 504 | |a Bibliografija: 56 jed | ||
| 520 | 8 | |a Summary: Ostracod faunas from an exposure of the Cenomanian Galala Formation in the area south of Ain Sukhna on the western side of the Gulf of Suez have yielded 11 species belonging to 10 genera. The recorded speciesare have been taxonomically described, discussed where required, and illustrated. The ostracod assemblage is characteristic for the late Cenomanian. It is composed of taxa of a typical marine shelf setting. The majority of the recorded species have a vastly extended geographic distribution in the areas along the southern shores of Tethys, indicating the absence of significant geographic barriers along this stretch during the late Cenomanian | |
| 653 | 0 | |a Ostrakodi |a Biostratigrafija | |
| 653 | 4 | |a Cenomanij | |
| 653 | 5 | |a Egipat |a Tetis (ocean) | |
| 700 | 1 | |a Morsi, Abdel-Mohsen M. | |
| 700 | 1 | |a Eissa, Ragy | |
| 700 | 1 | |a Kerdany, Moustafa | |
| 773 | 0 | |t Geologia Croatica |x 1330-030X |g 62 (2009), 1 ; str. 19-30 | |
| 981 | |b B06/09 |p CRO | ||
| 998 | |a dalo100708 |c vol2o121112 | ||
| 856 | 4 | 2 | |u http://hrcak.srce.hr/geologia-croatica |y Geologia Croatica |