Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt

Abstract This study investigates ostracod faunas from the well-preserved Paleocene to lower Eocene sedimentary succession at Wadi Tarfa, North Eastern Desert, Egypt. A total of 22 species and subspecies across 16 genera and 8 families were identified across 57 samples. Three zones were identified: D...

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Main Authors: Ahmed Samir, El Sayed M. Moneer, Islam El-Sheikh, Youssef S. Bazeen
Format: Article
Language:English
Published: Nature Portfolio 2025-02-01
Series:Scientific Reports
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Online Access:https://doi.org/10.1038/s41598-025-89560-6
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author Ahmed Samir
El Sayed M. Moneer
Islam El-Sheikh
Youssef S. Bazeen
author_facet Ahmed Samir
El Sayed M. Moneer
Islam El-Sheikh
Youssef S. Bazeen
author_sort Ahmed Samir
collection DOAJ
description Abstract This study investigates ostracod faunas from the well-preserved Paleocene to lower Eocene sedimentary succession at Wadi Tarfa, North Eastern Desert, Egypt. A total of 22 species and subspecies across 16 genera and 8 families were identified across 57 samples. Three zones were identified: Doricythereis jordanica jordanica Zone, Cytheropteron toshkaensis Zone, and Phalcocythere horraensis Zone, based on the stratigraphic distribution of ostracod fauna. However, correlations with other sections revealed inconsistencies in the first and last occurrences of ostracod species, indicating complexities in regional biostratigraphic correlation by ostracod fauna and the influence of localized depositional factors. Both R-mode and Q-mode clustering analyses were applied to ostracod assemblages, identifying four distinct faunal clusters and five biofacies, reflecting depositional changes from outer neritic to upper bathyal environments. The late Paleocene revealed reduced ostracod diversity, correlating with a deepening marine environment, particularly in the Tarawan Formation. Non-Metric Multidimensional Scaling (NMDS) analyses indicated significant paleobiogeographic connections between North African and Levantine sites, while faunal differentiation was greater in West African and Middle Eastern regions due to marine barriers.
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spelling doaj-art-e3c3c7fa1da94d039693fe4a568fd73c2025-08-20T03:04:38ZengNature PortfolioScientific Reports2045-23222025-02-0115111810.1038/s41598-025-89560-6Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, EgyptAhmed Samir0El Sayed M. Moneer1Islam El-Sheikh2Youssef S. Bazeen3Geology Department, Faculty of Science, Al-Azhar UniversityGeology Department, Faculty of Science, Al-Azhar UniversityGeology Department, Faculty of Science, Al-Azhar University, Assiut BranchGeology Department, Faculty of Science, Al-Azhar UniversityAbstract This study investigates ostracod faunas from the well-preserved Paleocene to lower Eocene sedimentary succession at Wadi Tarfa, North Eastern Desert, Egypt. A total of 22 species and subspecies across 16 genera and 8 families were identified across 57 samples. Three zones were identified: Doricythereis jordanica jordanica Zone, Cytheropteron toshkaensis Zone, and Phalcocythere horraensis Zone, based on the stratigraphic distribution of ostracod fauna. However, correlations with other sections revealed inconsistencies in the first and last occurrences of ostracod species, indicating complexities in regional biostratigraphic correlation by ostracod fauna and the influence of localized depositional factors. Both R-mode and Q-mode clustering analyses were applied to ostracod assemblages, identifying four distinct faunal clusters and five biofacies, reflecting depositional changes from outer neritic to upper bathyal environments. The late Paleocene revealed reduced ostracod diversity, correlating with a deepening marine environment, particularly in the Tarawan Formation. Non-Metric Multidimensional Scaling (NMDS) analyses indicated significant paleobiogeographic connections between North African and Levantine sites, while faunal differentiation was greater in West African and Middle Eastern regions due to marine barriers.https://doi.org/10.1038/s41598-025-89560-6OstracodaPaleocene-early EoceneEastern DesertBiostratigraphyPaleobathymeteryTythian affinity
spellingShingle Ahmed Samir
El Sayed M. Moneer
Islam El-Sheikh
Youssef S. Bazeen
Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt
Scientific Reports
Ostracoda
Paleocene-early Eocene
Eastern Desert
Biostratigraphy
Paleobathymetery
Tythian affinity
title Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt
title_full Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt
title_fullStr Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt
title_full_unstemmed Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt
title_short Paleoenvironmental and paleobiogeographical significance of Paleocene – early Eocene ostracods in Wadi Tarfa, North Eastern Desert, Egypt
title_sort paleoenvironmental and paleobiogeographical significance of paleocene early eocene ostracods in wadi tarfa north eastern desert egypt
topic Ostracoda
Paleocene-early Eocene
Eastern Desert
Biostratigraphy
Paleobathymetery
Tythian affinity
url https://doi.org/10.1038/s41598-025-89560-6
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