Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland)
Planktonic foraminifera, calcareous dinocysts and nannofossils have been identified in thin sections of the “spotted limestone”, exposed in the Grajcarek Stream at Szlachtowa and assigned to the Pieniny Limestone Formation in the Magura Succession, Pieniny Klippen Belt (southern Poland). The new dat...
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Annales Societatis Geologorum Poloniae
2015
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ftjgq:oai:geojournals.pgi.gov.pl:article/23629 2023-05-15T18:00:38+02:00 Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) Pszczółkowski, Andrzej 2015-05-27 application/pdf https://gq.pgi.gov.pl/asgp/article/view/23629 eng eng Annales Societatis Geologorum Poloniae https://gq.pgi.gov.pl/asgp/article/view/23629/16432 Annales Societatis Geologorum Poloniae; Vol 85, No 1 (2015); 21-42, doi:10.14241/asgp.2014.001 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjgq 2019-08-13T19:05:52Z Planktonic foraminifera, calcareous dinocysts and nannofossils have been identified in thin sections of the “spotted limestone”, exposed in the Grajcarek Stream at Szlachtowa and assigned to the Pieniny Limestone Formation in the Magura Succession, Pieniny Klippen Belt (southern Poland). The new data indicate that the “spotted limestone” is older than was suggested in previous reports (Albian or Cenomanian?). The foraminiferal taxa belong mainly to the upper part of the Lower Aptian. The calcareous nannofossils may correspond to the Aptian NC6(?)–NC7 zones, whereas the assemblage of calcareous dinoflagellate cysts is less conclusive (Late Barremian–Aptian). Article in Journal/Newspaper Planktonic foraminifera Geological Quarterly |
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Open Polar |
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Geological Quarterly |
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ftjgq |
language |
English |
description |
Planktonic foraminifera, calcareous dinocysts and nannofossils have been identified in thin sections of the “spotted limestone”, exposed in the Grajcarek Stream at Szlachtowa and assigned to the Pieniny Limestone Formation in the Magura Succession, Pieniny Klippen Belt (southern Poland). The new data indicate that the “spotted limestone” is older than was suggested in previous reports (Albian or Cenomanian?). The foraminiferal taxa belong mainly to the upper part of the Lower Aptian. The calcareous nannofossils may correspond to the Aptian NC6(?)–NC7 zones, whereas the assemblage of calcareous dinoflagellate cysts is less conclusive (Late Barremian–Aptian). |
format |
Article in Journal/Newspaper |
author |
Pszczółkowski, Andrzej |
spellingShingle |
Pszczółkowski, Andrzej Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) |
author_facet |
Pszczółkowski, Andrzej |
author_sort |
Pszczółkowski, Andrzej |
title |
Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) |
title_short |
Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) |
title_full |
Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) |
title_fullStr |
Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) |
title_full_unstemmed |
Aptian age of the “spotted limestone” (Pieniny Limestone Formation) in Grajcarek Stream (Pieniny Klippen Belt, Poland) |
title_sort |
aptian age of the “spotted limestone” (pieniny limestone formation) in grajcarek stream (pieniny klippen belt, poland) |
publisher |
Annales Societatis Geologorum Poloniae |
publishDate |
2015 |
url |
https://gq.pgi.gov.pl/asgp/article/view/23629 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Annales Societatis Geologorum Poloniae; Vol 85, No 1 (2015); 21-42, doi:10.14241/asgp.2014.001 |
op_relation |
https://gq.pgi.gov.pl/asgp/article/view/23629/16432 |
_version_ |
1766169818461896704 |