Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran

Upper Triassic (Norian) strata of the Miankuhi Formation in northeastern Iran have been studied palynologically, revealing a diverse but poorly preserved association of dinoflagellate cysts. Based on representatives of the genera Hebecysta, Heibergella, Rhaetogonyaulax and Sverdrupiella, the strata...

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Published in:Journal of Micropalaeontology
Main Authors: Ghasemi-Nejad, Ebrahim, Head, Martin J., Zamani, Maryam
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1144/jm.27.2.125
https://jm.copernicus.org/articles/27/125/2008/
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spelling ftcopernicus:oai:publications.copernicus.org:jm65585 2023-05-15T15:01:05+02:00 Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran Ghasemi-Nejad, Ebrahim Head, Martin J. Zamani, Maryam 2018-09-27 application/pdf https://doi.org/10.1144/jm.27.2.125 https://jm.copernicus.org/articles/27/125/2008/ eng eng doi:10.1144/jm.27.2.125 https://jm.copernicus.org/articles/27/125/2008/ eISSN: 2041-4978 Text 2018 ftcopernicus https://doi.org/10.1144/jm.27.2.125 2020-07-20T16:26:48Z Upper Triassic (Norian) strata of the Miankuhi Formation in northeastern Iran have been studied palynologically, revealing a diverse but poorly preserved association of dinoflagellate cysts. Based on representatives of the genera Hebecysta, Heibergella, Rhaetogonyaulax and Sverdrupiella, the strata are assigned to the middle of the Hebecysta balmei Zone with an inferred age of early Late Norian. The association shows similarities with assemblages from Australia, New Zealand, Indonesia, Northwest Europe, arctic Canada and Alaska, indicating an interconnection of warm Tethyan waters during the Late Triassic. The occurrence of Sverdrupiella species in the clastic, near-shore marine deposits of Miankuhi, and their presence in similar sedimentary facies world-wide, indicate that this genus was well adapted to clastic shallow-marine environments. Text Arctic Alaska Copernicus Publications: E-Journals Arctic Canada New Zealand Journal of Micropalaeontology 27 2 125 134
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language English
description Upper Triassic (Norian) strata of the Miankuhi Formation in northeastern Iran have been studied palynologically, revealing a diverse but poorly preserved association of dinoflagellate cysts. Based on representatives of the genera Hebecysta, Heibergella, Rhaetogonyaulax and Sverdrupiella, the strata are assigned to the middle of the Hebecysta balmei Zone with an inferred age of early Late Norian. The association shows similarities with assemblages from Australia, New Zealand, Indonesia, Northwest Europe, arctic Canada and Alaska, indicating an interconnection of warm Tethyan waters during the Late Triassic. The occurrence of Sverdrupiella species in the clastic, near-shore marine deposits of Miankuhi, and their presence in similar sedimentary facies world-wide, indicate that this genus was well adapted to clastic shallow-marine environments.
format Text
author Ghasemi-Nejad, Ebrahim
Head, Martin J.
Zamani, Maryam
spellingShingle Ghasemi-Nejad, Ebrahim
Head, Martin J.
Zamani, Maryam
Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran
author_facet Ghasemi-Nejad, Ebrahim
Head, Martin J.
Zamani, Maryam
author_sort Ghasemi-Nejad, Ebrahim
title Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran
title_short Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran
title_full Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran
title_fullStr Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran
title_full_unstemmed Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran
title_sort dinoflagellate cysts from the upper triassic (norian) of northeastern iran
publishDate 2018
url https://doi.org/10.1144/jm.27.2.125
https://jm.copernicus.org/articles/27/125/2008/
geographic Arctic
Canada
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Alaska
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Alaska
op_source eISSN: 2041-4978
op_relation doi:10.1144/jm.27.2.125
https://jm.copernicus.org/articles/27/125/2008/
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