Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)

In this paper, to study biostratigraphy of Paleogene deposits based on foraminifera fauna in NW of Jiroft located in the Central Iran zone, two stratigraphic sections, namely Sabzevaran (354 m) and Sad (132 m) sections were selected. Planktonic foraminifera and large benthic foraminifera were identi...

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Main Authors: Hosseini Raviz, Seyed Mohammad Reza, Afghah, Massih, Shirazi, Mahnaz Parvaneh Nejad, Department Of Geology, Payame Noor University
Format: Text
Language:English
Published: Zenodo 2020
Subjects:
Eocene
Oligocene
Planktonic Foraminifera
Larger Benthic Foraminifera
Jiroft
Central Iran
Planktonic foraminifera
Online Access:https://dx.doi.org/10.5281/zenodo.3936164
https://zenodo.org/record/3936164
id ftdatacite:10.5281/zenodo.3936164
record_format openpolar
spelling ftdatacite:10.5281/zenodo.3936164 2023-05-15T18:00:25+02:00 Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran) Hosseini Raviz, Seyed Mohammad Reza Afghah, Massih Shirazi, Mahnaz Parvaneh Nejad Department Of Geology, Payame Noor University 2020 https://dx.doi.org/10.5281/zenodo.3936164 https://zenodo.org/record/3936164 en eng Zenodo https://zenodo.org/communities/biosyslit https://dx.doi.org/10.5281/zenodo.3936165 https://zenodo.org/communities/biosyslit Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode CC-BY-4.0 info:eu-repo/semantics/openAccess CC-BY Eocene Oligocene Planktonic Foraminifera Larger Benthic Foraminifera Jiroft Central Iran Text Journal article article-journal ScholarlyArticle 2020 ftdatacite https://doi.org/10.5281/zenodo.3936164 https://doi.org/10.5281/zenodo.3936165 2021-11-05T12:55:41Z In this paper, to study biostratigraphy of Paleogene deposits based on foraminifera fauna in NW of Jiroft located in the Central Iran zone, two stratigraphic sections, namely Sabzevaran (354 m) and Sad (132 m) sections were selected. Planktonic foraminifera and large benthic foraminifera were identified in both sections. Faunal assemblages and vertical distribution of identified species support presence of 5 planktonic foraminiferal and 2 large benthic foraminiferal biozones in the Sabzevaran section showing Middle Eocene to Chattian age. In addition, presence of planktonic foraminiferal assemblage along with 2 large benthic foraminiferal biozones confirms the Late Eocene to Chattian age for the Sad section. Text Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Eocene
Oligocene
Planktonic Foraminifera
Larger Benthic Foraminifera
Jiroft
Central Iran
spellingShingle Eocene
Oligocene
Planktonic Foraminifera
Larger Benthic Foraminifera
Jiroft
Central Iran
Hosseini Raviz, Seyed Mohammad Reza
Afghah, Massih
Shirazi, Mahnaz Parvaneh Nejad
Department Of Geology, Payame Noor University
Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)
topic_facet Eocene
Oligocene
Planktonic Foraminifera
Larger Benthic Foraminifera
Jiroft
Central Iran
description In this paper, to study biostratigraphy of Paleogene deposits based on foraminifera fauna in NW of Jiroft located in the Central Iran zone, two stratigraphic sections, namely Sabzevaran (354 m) and Sad (132 m) sections were selected. Planktonic foraminifera and large benthic foraminifera were identified in both sections. Faunal assemblages and vertical distribution of identified species support presence of 5 planktonic foraminiferal and 2 large benthic foraminiferal biozones in the Sabzevaran section showing Middle Eocene to Chattian age. In addition, presence of planktonic foraminiferal assemblage along with 2 large benthic foraminiferal biozones confirms the Late Eocene to Chattian age for the Sad section.
format Text
author Hosseini Raviz, Seyed Mohammad Reza
Afghah, Massih
Shirazi, Mahnaz Parvaneh Nejad
Department Of Geology, Payame Noor University
author_facet Hosseini Raviz, Seyed Mohammad Reza
Afghah, Massih
Shirazi, Mahnaz Parvaneh Nejad
Department Of Geology, Payame Noor University
author_sort Hosseini Raviz, Seyed Mohammad Reza
title Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)
title_short Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)
title_full Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)
title_fullStr Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)
title_full_unstemmed Biostratigraphy of Late Eocene-Oligocene Deposits based on Planktonic and Larger Benthic Foraminifera in the Sabzevaran and Sad Sections, NW Jiroft (Iran)
title_sort biostratigraphy of late eocene-oligocene deposits based on planktonic and larger benthic foraminifera in the sabzevaran and sad sections, nw jiroft (iran)
publisher Zenodo
publishDate 2020
url https://dx.doi.org/10.5281/zenodo.3936164
https://zenodo.org/record/3936164
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://zenodo.org/communities/biosyslit
https://dx.doi.org/10.5281/zenodo.3936165
https://zenodo.org/communities/biosyslit
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
CC-BY-4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.3936164
https://doi.org/10.5281/zenodo.3936165
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