Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey
Abstract: According to the literature, the Adana Basin, at the easternmost part of the Mediterra-nean Basin in southern Turkey, records the Pliocene stage with shallow-marine to fluvial deposits. Our micropalaeontological analysis of samples from the Adana Basin reveal Late Lago–Mare biofacies with...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1027.7824 2023-05-15T18:00:51+02:00 Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey Paola Cipollari Domenico Cosentino Giuditta Radeff Taylor F. Schildgen Costanza Faranda Francesco Grossi Elsa Gliozzi Alessandra Smedile Rocco Gennari Francis Ö. Dudas The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.7824 http://sp.lyellcollection.org/content/372/1/473.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.7824 http://sp.lyellcollection.org/content/372/1/473.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://sp.lyellcollection.org/content/372/1/473.full.pdf text ftciteseerx 2016-10-30T00:05:15Z Abstract: According to the literature, the Adana Basin, at the easternmost part of the Mediterra-nean Basin in southern Turkey, records the Pliocene stage with shallow-marine to fluvial deposits. Our micropalaeontological analysis of samples from the Adana Basin reveal Late Lago–Mare biofacies with Paratethyan ostracod assemblages pertaining to the Loxocorniculina djafarovi zone. Grey clays rich in planktonic foraminifera lie above the Lago–Mare deposits. Within the grey clays, the continuous occurrence of the calcareous nannofossil Reticulofenestra zancleana and the base of the Reticulofenestra pseudoumbilicus paracme points to an Early Zanclean age (5.332–5.199 Ma). Both ostracod and benthic foraminifera indicate epibathyal and bathyal environments. 87Sr/86Sr measurements on planktonic and benthic foraminifera fall below the mean global ocean value for the Early Zanclean, indicating potentially insufficient mixing of low 87Sr/86Sr Mediterranean brackish ‘Lago–Mare ’ water with the global ocean in the earliest Pliocene. We utilize the ages and palaeodepths of the marine sediments together with their modern elevations to determine uplift rates of the Adana Basin of 0.06 to 0.13 mm a21 since 5.2–5.3 Ma Text Planktonic foraminifera Unknown |
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English |
description |
Abstract: According to the literature, the Adana Basin, at the easternmost part of the Mediterra-nean Basin in southern Turkey, records the Pliocene stage with shallow-marine to fluvial deposits. Our micropalaeontological analysis of samples from the Adana Basin reveal Late Lago–Mare biofacies with Paratethyan ostracod assemblages pertaining to the Loxocorniculina djafarovi zone. Grey clays rich in planktonic foraminifera lie above the Lago–Mare deposits. Within the grey clays, the continuous occurrence of the calcareous nannofossil Reticulofenestra zancleana and the base of the Reticulofenestra pseudoumbilicus paracme points to an Early Zanclean age (5.332–5.199 Ma). Both ostracod and benthic foraminifera indicate epibathyal and bathyal environments. 87Sr/86Sr measurements on planktonic and benthic foraminifera fall below the mean global ocean value for the Early Zanclean, indicating potentially insufficient mixing of low 87Sr/86Sr Mediterranean brackish ‘Lago–Mare ’ water with the global ocean in the earliest Pliocene. We utilize the ages and palaeodepths of the marine sediments together with their modern elevations to determine uplift rates of the Adana Basin of 0.06 to 0.13 mm a21 since 5.2–5.3 Ma |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
author |
Paola Cipollari Domenico Cosentino Giuditta Radeff Taylor F. Schildgen Costanza Faranda Francesco Grossi Elsa Gliozzi Alessandra Smedile Rocco Gennari Francis Ö. Dudas |
spellingShingle |
Paola Cipollari Domenico Cosentino Giuditta Radeff Taylor F. Schildgen Costanza Faranda Francesco Grossi Elsa Gliozzi Alessandra Smedile Rocco Gennari Francis Ö. Dudas Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey |
author_facet |
Paola Cipollari Domenico Cosentino Giuditta Radeff Taylor F. Schildgen Costanza Faranda Francesco Grossi Elsa Gliozzi Alessandra Smedile Rocco Gennari Francis Ö. Dudas |
author_sort |
Paola Cipollari |
title |
Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey |
title_short |
Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey |
title_full |
Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey |
title_fullStr |
Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey |
title_full_unstemmed |
Easternmost Mediterranean evidence of the Zanclean flooding event and subsequent surface uplift: Adana Basin, southern Turkey |
title_sort |
easternmost mediterranean evidence of the zanclean flooding event and subsequent surface uplift: adana basin, southern turkey |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.7824 http://sp.lyellcollection.org/content/372/1/473.full.pdf |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
http://sp.lyellcollection.org/content/372/1/473.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.7824 http://sp.lyellcollection.org/content/372/1/473.full.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766170113924399104 |