0000000000299702

AUTHOR

Amir Mohammad Jamali

showing 4 related works from this author

Integrated bio- and carbon-isotope stratigraphy of the Upper Cretaceous Gurpi Formation (Iran): A new reference for the eastern Tethys and its implic…

2018

29 pages; International audience; A high-resolution stratigraphic analysis of the Upper Cretaceous Gurpi Formation has been undertaken in the Shahneshin section (Zagros Basin, Iran). New results on calcareous nannofossils, planktic foraminifers, dinoflagellate cysts and high-resolution carbon and oxygen stable isotopes form the basis of a reference section for the eastern Tethys that spans the upper Coniacian to the late Danian. Carbon-isotope correlation to Gubbio, Italy and the NW German chalk allows for the identification of many isotopic events as well as for the definition of new events in the Campanian and Maastrichtian. Our results allow for a review of the accurate position of the C…

010506 paleontologyStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryStage (stratigraphy)Calcareous nannofossils14. Life underwater0105 earth and related environmental sciencesbiologyStable isotope ratioDinoflagellate cystsCarbon isotopesDinoflagellatePaleontologyPlanktic foraminiferaPlanktonbiology.organism_classificationZagrosCretaceousStratigraphy13. Climate actionIsotopes of carbonTethyan realm[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyConiacian–MaastrichtianGeologyCretaceous Research
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Biostratigraphy and isotope stratigraphy of upper Maastrichtian–Danian marine deposits of the Kopet-Dagh Basin, northeast Iran

2018

Abstract Biostratigraphy, using foraminifera and echinoids, plus high-resolution carbon isotope stratigraphy of the upper Maastrichtian–Danian interval in the western part of the Kopet-Dagh Basin in northeast Iran are outlined. Our study of shallow-marine carbonate platform deposits of the Kalat Formation, rich in larger benthic foraminifera (predominantly Clypeorbis mammillatus Schlumberger, Lepidorbitoides sp. and Siderolites calcitrapoides Lamarck), has allowed the definition of a C. mammillatus-S. calcitrapoides Assemblage Zone, of late Maastrichtian age. Clypeorbis mammillatus is here recorded for the first time from the Maastrichtian Kalat Formation and represents the most easterly fi…

010506 paleontologybiologyCarbonate platformMesozoic Cenozoic Clypeorbis mammillatus Kalat Formation Chehel Kaman Formation Planktonic foraminifera Isotope stratigraphy.PaleontologyBiozoneBiostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousForaminiferaPaleontologyStratigraphyEchinocorysCenozoicGeology0105 earth and related environmental sciences
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Planktonic foraminifera biozones and isotope stratigraphy of the Cenomanian-Turonian boundary in the western part of the Kopet-Dagh Basin, NE Iran

2018

Abstract A biostratigraphic study based on the planktonic foraminifera and isotope stratigraphy of the Cenomanian-Turonian interval has been undertaken in the western part of the Kopet-Dagh Basin (NE Iran). In this research, two stratigraphic sections including: Maraveh Tappeh and Qareh Galdy have been sampled and studied. Based on planktonic foraminifera, three biozones were assigned to this interval. These are the Rotalipora cushmani Zone, Whiteinella archaeocretacea Zone and Helvetoglobotruncana helvetica Zone, These biostratigraphic data confirm a gradual faunal turnover of planktonic foraminifera, at the Cenomanian-Turonian boundary in Whiteinella archaeocretacea Zone characterized by:…

010506 paleontologybiologyδ18OGeologyBiozoneBiostratigraphyStructural basin010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesForaminiferaPaleontologyStratigraphyBiostratigraphy Light isotopes Cenomanian-Turonian boundary Kopet-Dagh basin NE IranCenomanianSiltstoneGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of African Earth Sciences
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Turonian-Maastrichtian biostratigraphy and isotope stratigraphy of the Kopet-Dagh Basin deposits, northeastern Neo-Tethys, Iran

2021

Abstract Planktonic foraminiferal biostratigraphy and isotope stratigraphy analyses of Turonian-Maastrichtian deposits have been carried out in the western part of the Kopet-Dagh Basin. The identification of the planktonic foraminiferal assemblages has led to the recognition of twelve Upper Cretaceous zones (Helvetoglobotruncana helvetica Zone to the Contusotruncana contusa-Abathomphalus mayaroensis zone) from the Tethyan realm. The obtained stable carbon isotope profile correlates with other reference curves, revealing many Late Cretaceous events including the Hitchwood, Navigation, Light Point, East Cliff, White Fall, Late Campanian Event (LCE), Campanian-Maastrichtian Boundary Event (CMB…

Planktonic foraminiferageographygeography.geographical_feature_categoryStable isotope ratioPalaeoenvironmental conditionsPaleontologyBiostratigraphyStructural basinOceanographyStable isotopeUpper cretaceousCretaceousTectonicsPaleontologyStratigraphyIsotopes of carbonCliffEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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