Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley

23 species of ostracods and 20 species and species groups of planktonic foraminifera from the 80m thick Qeren Sartabasection, central Jordan Valley, are described and illustrated. The material is determined by planktonic foraminiferal biostratigraphy to belong to the latest Early Eocene (upper part...

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Published in:Journal of Micropalaeontology
Main Authors: Honigstein, A., Rosenfeld, A., Benjamini, C.
Format: Text
Language:English
Published: 2018
Subjects:
Planktonic foraminifera
Online Access:https://doi.org/10.1144/jm.10.1.95
https://jm.copernicus.org/articles/10/95/1991/
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spelling ftcopernicus:oai:publications.copernicus.org:jm65235 2023-05-15T18:00:32+02:00 Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley Honigstein, A. Rosenfeld, A. Benjamini, C. 2018-09-27 application/pdf https://doi.org/10.1144/jm.10.1.95 https://jm.copernicus.org/articles/10/95/1991/ eng eng doi:10.1144/jm.10.1.95 https://jm.copernicus.org/articles/10/95/1991/ eISSN: 2041-4978 Text 2018 ftcopernicus https://doi.org/10.1144/jm.10.1.95 2020-07-20T16:28:19Z 23 species of ostracods and 20 species and species groups of planktonic foraminifera from the 80m thick Qeren Sartabasection, central Jordan Valley, are described and illustrated. The material is determined by planktonic foraminiferal biostratigraphy to belong to the latest Early Eocene (upper part of Zone P9) and the early Middle Eocene (Zone P10). The palaeoecology is representative of a pelagic marine shelf, with periodic events of shallowing and hardground formation. Text Planktonic foraminifera Copernicus Publications: E-Journals Journal of Micropalaeontology 10 1 95 107
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description 23 species of ostracods and 20 species and species groups of planktonic foraminifera from the 80m thick Qeren Sartabasection, central Jordan Valley, are described and illustrated. The material is determined by planktonic foraminiferal biostratigraphy to belong to the latest Early Eocene (upper part of Zone P9) and the early Middle Eocene (Zone P10). The palaeoecology is representative of a pelagic marine shelf, with periodic events of shallowing and hardground formation.
format Text
author Honigstein, A.
Rosenfeld, A.
Benjamini, C.
spellingShingle Honigstein, A.
Rosenfeld, A.
Benjamini, C.
Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
author_facet Honigstein, A.
Rosenfeld, A.
Benjamini, C.
author_sort Honigstein, A.
title Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
title_short Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
title_full Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
title_fullStr Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
title_full_unstemmed Ostracods and foraminifera from the Early - Middle Eocene of Qeren Sartaba, Jordan Valley
title_sort ostracods and foraminifera from the early - middle eocene of qeren sartaba, jordan valley
publishDate 2018
url https://doi.org/10.1144/jm.10.1.95
https://jm.copernicus.org/articles/10/95/1991/
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source eISSN: 2041-4978
op_relation doi:10.1144/jm.10.1.95
https://jm.copernicus.org/articles/10/95/1991/
op_doi https://doi.org/10.1144/jm.10.1.95
container_title Journal of Micropalaeontology
container_volume 10
container_issue 1
container_start_page 95
op_container_end_page 107
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