New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey
WOS: 000412609000039 Early-Middle Miocene is a period of significant geological events (such as global marine transgression) on the Alpine-Himalayan belt. The Kahramanmaras Basin is located in transition between the Taurides and Arabian Plate, which are important segments of Alpine-Himalayan Belt. E...
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ftmuglauniv:oai:acikerisim.mu.edu.tr:20.500.12809/1810 2024-09-15T18:30:48+00:00 New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey Darbaş, Güldemin Gül, Murat MÜ, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü Gül, Murat 2017 application/pdf https://hdl.handle.net/20.500.12809/1810 https://doi.org/10.1016/j.jafrearsci.2017.07.010 eng eng Pergamon-Elsevier Science Ltd Journal of African Earth Sciences Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı 1464-343X 1879-1956 https://doi.org/10.1016/j.jafrearsci.2017.07.010 https://hdl.handle.net/20.500.12809/1810 doi:10.1016/j.jafrearsci.2017.07.010 134 457 465 info:eu-repo/semantics/closedAccess Planktonic Foraminifera Early-Middle Miocene (Burdigalian-Langhian) Kilisecik Formation Kahramanmaral Turkey article 2017 ftmuglauniv https://doi.org/20.500.12809/181010.1016/j.jafrearsci.2017.07.010 2024-07-12T03:03:28Z WOS: 000412609000039 Early-Middle Miocene is a period of significant geological events (such as global marine transgression) on the Alpine-Himalayan belt. The Kahramanmaras Basin is located in transition between the Taurides and Arabian Plate, which are important segments of Alpine-Himalayan Belt. Eleven planktonic foraminifera species belonging to Dentoglobigerina, Globigerina, Globoquadrina, Globigerinoides, Praeorbulina and Globigerinella genera have been identified by micropaleontological studies. Planktonic foraminiferal assemblage demonstrates that the Kilisecik Formation is not older than the Burdigalian as suggested by concomitant presence of G. bisphaericus, and not younger than Langhian as suggested by last occurrence of Praeorbulina glomerosa. Globigerinoides spp, Praeorbulina glomerasa and Dentoglobigerina altispira indicate the existence of a warm climatic condition in the Early-Middle Miocene period (the Burdigalian-Langhian time). (C) 2017 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Planktonic foraminifera Muğla Sıtkı Koçman University Institutional Repository (DSpace@Muğla) Journal of African Earth Sciences 134 457 465 |
institution |
Open Polar |
collection |
Muğla Sıtkı Koçman University Institutional Repository (DSpace@Muğla) |
op_collection_id |
ftmuglauniv |
language |
English |
topic |
Planktonic Foraminifera Early-Middle Miocene (Burdigalian-Langhian) Kilisecik Formation Kahramanmaral Turkey |
spellingShingle |
Planktonic Foraminifera Early-Middle Miocene (Burdigalian-Langhian) Kilisecik Formation Kahramanmaral Turkey Darbaş, Güldemin Gül, Murat New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey |
topic_facet |
Planktonic Foraminifera Early-Middle Miocene (Burdigalian-Langhian) Kilisecik Formation Kahramanmaral Turkey |
description |
WOS: 000412609000039 Early-Middle Miocene is a period of significant geological events (such as global marine transgression) on the Alpine-Himalayan belt. The Kahramanmaras Basin is located in transition between the Taurides and Arabian Plate, which are important segments of Alpine-Himalayan Belt. Eleven planktonic foraminifera species belonging to Dentoglobigerina, Globigerina, Globoquadrina, Globigerinoides, Praeorbulina and Globigerinella genera have been identified by micropaleontological studies. Planktonic foraminiferal assemblage demonstrates that the Kilisecik Formation is not older than the Burdigalian as suggested by concomitant presence of G. bisphaericus, and not younger than Langhian as suggested by last occurrence of Praeorbulina glomerosa. Globigerinoides spp, Praeorbulina glomerasa and Dentoglobigerina altispira indicate the existence of a warm climatic condition in the Early-Middle Miocene period (the Burdigalian-Langhian time). (C) 2017 Elsevier Ltd. All rights reserved. |
author2 |
MÜ, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü Gül, Murat |
format |
Article in Journal/Newspaper |
author |
Darbaş, Güldemin Gül, Murat |
author_facet |
Darbaş, Güldemin Gül, Murat |
author_sort |
Darbaş, Güldemin |
title |
New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey |
title_short |
New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey |
title_full |
New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey |
title_fullStr |
New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey |
title_full_unstemmed |
New observations of planktonic foraminifera from the Burdigalian-Langhian deposits (Kilisecik Formation) of Kahramanmara/Turkey |
title_sort |
new observations of planktonic foraminifera from the burdigalian-langhian deposits (kilisecik formation) of kahramanmara/turkey |
publisher |
Pergamon-Elsevier Science Ltd |
publishDate |
2017 |
url |
https://hdl.handle.net/20.500.12809/1810 https://doi.org/10.1016/j.jafrearsci.2017.07.010 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
Journal of African Earth Sciences Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı 1464-343X 1879-1956 https://doi.org/10.1016/j.jafrearsci.2017.07.010 https://hdl.handle.net/20.500.12809/1810 doi:10.1016/j.jafrearsci.2017.07.010 134 457 465 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/20.500.12809/181010.1016/j.jafrearsci.2017.07.010 |
container_title |
Journal of African Earth Sciences |
container_volume |
134 |
container_start_page |
457 |
op_container_end_page |
465 |
_version_ |
1810472316365176832 |