Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus

The existing chronostratigraphic framework in NW Cyprus of two-phase, Early and Late Miocene reef and associated facies development is tested and improved using a combination of calcareous nannofossil, benthic and planktonic foraminiferal, and also Sr isotope dating. Following localized Late Oligoce...

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Published in:Journal of the Geological Society
Main Authors: Cannings T., Balmer E. M., Coletti G., Ickert R. B., Kroon D., Raffi I., Robertson A. H. F.
Other Authors: Cannings, T, Balmer, E, Coletti, G, Ickert, R, Kroon, D, Raffi, I, Robertson, A
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society Publishing House 2021
Subjects:
Online Access:https://hdl.handle.net/10281/396747
https://doi.org/10.1144/jgs2020-081
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spelling ftunivmilanobic:oai:boa.unimib.it:10281/396747 2024-04-14T08:04:00+00:00 Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus Cannings T. Balmer E. M. Coletti G. Ickert R. B. Kroon D. Raffi I. Robertson A. H. F. Cannings, T Balmer, E Coletti, G Ickert, R Kroon, D Raffi, I Robertson, A 2021 STAMPA https://hdl.handle.net/10281/396747 https://doi.org/10.1144/jgs2020-081 eng eng Geological Society Publishing House country:GB info:eu-repo/semantics/altIdentifier/wos/WOS:000614227300001 volume:178 issue:2 journal:JOURNAL OF THE GEOLOGICAL SOCIETY https://hdl.handle.net/10281/396747 doi:10.1144/jgs2020-081 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85103471731 info:eu-repo/semantics/closedAccess Reef Miocene Cypru Climate Change Stratigraphy info:eu-repo/semantics/article 2021 ftunivmilanobic https://doi.org/10.1144/jgs2020-081 2024-03-21T17:21:22Z The existing chronostratigraphic framework in NW Cyprus of two-phase, Early and Late Miocene reef and associated facies development is tested and improved using a combination of calcareous nannofossil, benthic and planktonic foraminiferal, and also Sr isotope dating. Following localized Late Oligocene neritic carbonate deposition (e.g. benthic foraminiferal shoals), reefs and related facies (Terra Member) began to develop c. 24 Ma (Aquitanian) and terminated c. 16 Ma (end-Burdigalian). Early Miocene reef and marginal facies were then extensively redeposited as multiple debris-flow deposits until c. 13.7 Ma, influenced by a combination of global sea-level fall (related to growth of the East Antarctic Ice Sheet) and local-to regional-scale tectonics. Reef growth and related deposition resumed (Koronia Member) c. 9.1 Ma (Tortonian), then terminated by c. 6.1 Ma (Middle Messinian), followed by the Messinian salinity crisis. Neritic accumulation in NW Cyprus began earlier (Late Oligocene), than in southern Cyprus (Early Miocene). The Early Miocene reefs developed on a roughly north–south-trending structural high in the west (Akamas Peninsula area) whereas the Late Miocene reefs developed on both flanks of the neotectonic Polis graben. The two-phase reef development is mirrored in SE Cyprus and in some other Mediterranean areas (e.g. southern Turkey, Israel, Italy, southern Spain). Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive) Antarctic East Antarctic Ice Sheet Journal of the Geological Society 178 2
institution Open Polar
collection Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive)
op_collection_id ftunivmilanobic
language English
topic Reef
Miocene
Cypru
Climate Change
Stratigraphy
spellingShingle Reef
Miocene
Cypru
Climate Change
Stratigraphy
Cannings T.
Balmer E. M.
Coletti G.
Ickert R. B.
Kroon D.
Raffi I.
Robertson A. H. F.
Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
topic_facet Reef
Miocene
Cypru
Climate Change
Stratigraphy
description The existing chronostratigraphic framework in NW Cyprus of two-phase, Early and Late Miocene reef and associated facies development is tested and improved using a combination of calcareous nannofossil, benthic and planktonic foraminiferal, and also Sr isotope dating. Following localized Late Oligocene neritic carbonate deposition (e.g. benthic foraminiferal shoals), reefs and related facies (Terra Member) began to develop c. 24 Ma (Aquitanian) and terminated c. 16 Ma (end-Burdigalian). Early Miocene reef and marginal facies were then extensively redeposited as multiple debris-flow deposits until c. 13.7 Ma, influenced by a combination of global sea-level fall (related to growth of the East Antarctic Ice Sheet) and local-to regional-scale tectonics. Reef growth and related deposition resumed (Koronia Member) c. 9.1 Ma (Tortonian), then terminated by c. 6.1 Ma (Middle Messinian), followed by the Messinian salinity crisis. Neritic accumulation in NW Cyprus began earlier (Late Oligocene), than in southern Cyprus (Early Miocene). The Early Miocene reefs developed on a roughly north–south-trending structural high in the west (Akamas Peninsula area) whereas the Late Miocene reefs developed on both flanks of the neotectonic Polis graben. The two-phase reef development is mirrored in SE Cyprus and in some other Mediterranean areas (e.g. southern Turkey, Israel, Italy, southern Spain).
author2 Cannings, T
Balmer, E
Coletti, G
Ickert, R
Kroon, D
Raffi, I
Robertson, A
format Article in Journal/Newspaper
author Cannings T.
Balmer E. M.
Coletti G.
Ickert R. B.
Kroon D.
Raffi I.
Robertson A. H. F.
author_facet Cannings T.
Balmer E. M.
Coletti G.
Ickert R. B.
Kroon D.
Raffi I.
Robertson A. H. F.
author_sort Cannings T.
title Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
title_short Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
title_full Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
title_fullStr Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
title_full_unstemmed Microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
title_sort microfossil and strontium isotope chronology used to identify the controls of miocene reefs and related facies in nw cyprus
publisher Geological Society Publishing House
publishDate 2021
url https://hdl.handle.net/10281/396747
https://doi.org/10.1144/jgs2020-081
geographic Antarctic
East Antarctic Ice Sheet
geographic_facet Antarctic
East Antarctic Ice Sheet
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000614227300001
volume:178
issue:2
journal:JOURNAL OF THE GEOLOGICAL SOCIETY
https://hdl.handle.net/10281/396747
doi:10.1144/jgs2020-081
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85103471731
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1144/jgs2020-081
container_title Journal of the Geological Society
container_volume 178
container_issue 2
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