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[1]
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Neorbitolinopsis conica (Matsumaru in Matsumaru and Furusawa, 2007) comb. nov., a Lower Cretaceous marker from the Orbitolina Limestone of Central Iran
Revue de Micropaléontologie,
2022
DOI:10.1016/j.revmic.2022.100680
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[2]
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Microfacies and depositional environment of Tarbur Formation (Upper
Cretaceous‐Lower
Palaeocene) Zagros area, southwestern Iran
Geological Journal,
2022
DOI:10.1002/gj.4450
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[3]
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The “Orbitolina Limestone” of central Iran: new data about microfacies, orbitolinid biostratigraphy, and palaeogeography
Facies,
2022
DOI:10.1007/s10347-022-00647-2
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[4]
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Neorbitolinopsis conica (Matsumaru in Matsumaru and Furusawa, 2007) comb. nov., a Lower Cretaceous marker from the Orbitolina Limestone of Central Iran
Revue de Micropaléontologie,
2022
DOI:10.1016/j.revmic.2022.100680
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[5]
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Microfacies and depositional environment of Tarbur Formation (Upper Cretaceous‐Lower Palaeocene) Zagros area, southwestern Iran
Geological Journal,
2022
DOI:10.1002/gj.4450
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[6]
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Neorbitolinopsis conica (Matsumaru in Matsumaru and Furusawa, 2007) comb. nov., a Lower Cretaceous marker from the Orbitolina Limestone of Central Iran
Revue de Micropaléontologie,
2022
DOI:10.1016/j.revmic.2022.100680
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[7]
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Microfacies and depositional environment of Tarbur Formation (Upper Cretaceous‐Lower Palaeocene) Zagros area, southwestern Iran
Geological Journal,
2022
DOI:10.1002/gj.4450
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[8]
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Stratigraphic distribution of shallow-water benthic foraminifera from the Lower Cretaceous Taft formation, Central Iran (Yazd Block), with evidence for the importance of hiatuses
Annales de Paléontologie,
2020
DOI:10.1016/j.annpal.2020.102399
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[9]
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Persiconus sarvaki gen. et sp. nov., a new complex orbitolinid (Foraminifera) from the Cenomanian of the Sarvak Formation (SW Iran, Zagros Zone)
Cretaceous Research,
2020
DOI:10.1016/j.cretres.2020.104380
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[10]
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Origin and evolutionary history of Anglonautilus (Nautilida, Cymatoceratidae) and a new species from the lower Aptian of Spain
Cretaceous Research,
2017
DOI:10.1016/j.cretres.2016.12.004
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