3.8 Article

Belemnite biostratigraphy of the upper Jurassic to lower Cretaceous strata in the Surghar range, NW Pakistan: Systematic and Paleobiogeographic implications

Journal

IRANIAN JOURNAL OF EARTH SCIENCES
Volume 13, Issue 1, Pages 1-13

Publisher

ISLAMIC AZAD UNIV, MASHHAD BRANCH

Keywords

Belemnites; Biostratigraphy; Jurassic-Cretaceous; Paleobiogeography

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Four belemnite genera and twelve age-diagnostic species were identified from the Upper Jurassic-Lower Cretaceous sequence of the Chichali Formation in northwest Pakistan. Based on the identified belemnites, four local biozones were established, revealing the migration pathways and distinctive paleobiogeographic provinces of belemnites in the Tethyan and Boreal Realms. The paleoceanic settings indicate a persistent oceanic connection between the Indo-Pacific and Mediterranean Provinces during the Lower Cretaceous, with the Boreal and Tethyan Realms also connected by shallow-water routes.
Four belemnite genera and twelve age-diagnostic species were identified from the from Upper Jurassic-Lower Cretaceous sequence of the Chichali Formation, northwest Pakistan. Four local biozones were established based on the identified belemnites. These biozones are arranged from base to top as follows; Hibolithes pilleti/Hibolithes jaculoides/Hibolithes hastatus Zone of Kimmeridgian age, Hibolithes marwicki marwicki/Hibolithes arkelli Zone of Tithonian age, Belemnopsis malucana Zone defines Tithonian- Berriasian boundary, and Neohibolites ewaldi/Hibolithes longior/Belemnopsis jonkeri Zone of Velanginian age. The biostratigraphic and paleogeographic occurrences of belemnites in the Tethyan and Boreal Realms were used to identify the migration pathways and distinctive paleobiogeographic provinces of belemnites. The paleoceanic settings closely linked the Upper Jurassic strata (similar to Biozones 1-2, representing the Kimmeridgian-Tithonian range) in the Tethyan and the Boreal Realms. The Lower Cretaceous (similar to Biozone 3, representing the Berriasian) strata also reveal a persistent oceanic connection between the Indo-Pacific and Mediterranean Provinces. However, the Boreal and Tethyan Realms were also connected in the Lower Cretaceous (similar to Biozone 4, representing the Velanginian strata) by shallow-water routes.

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