The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain

The global stratotype sections and points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages have been defined in the coastal cliff along the Itzurun Beach at the town of Zumaia in the Basque Country, northern Spain. In the hemipelagic section exposed at Zumaia...

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Published in:Paleoceanography
Main Authors: Schmitz, B., Pujalte, V., Molina, E., Monechi, S., Orue-Etxebarria, X., Speijer, R. P., Alegret, L., Apellaniz, E., Arenillas, I., Aubry, M. P., Baceta, J. I., Berggren, W. A., Bernaola, G., Caballero, F., Clemmensen, A., Dinarès-Turell, J., Dupuis, C., Heilmann-Clausen, C., Orús, A. H., Knox, R., Martín-Rubio, M., Ortiz, S., Payros, A., Petrizzo, M. R., von Salis, K., Sprong, J., Steurbaut, E., Thomsen, E.
Other Authors: Schmitz, B.; Department of Geology, Lund University, SE-22362 Lund, Sweden, Pujalte, V.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Molina, E.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain, Monechi, S.; Department of Earth Sciences, Florence University, 50121 Florence, Italy, Orue-Etxebarria, X.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Speijer, R. P.; Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium, Alegret, L.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain, Apellaniz, E.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Arenillas, I.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain, Aubry, M. P.; Department of Geology, Rutgers University, Piscatatway, NJ 08854 USA., Baceta, J. I.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Berggren, W. A.; Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA, Bernaola, G.; Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain, Caballero, F.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Clemmensen, A.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark, Dinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Dupuis, C.; Laboratoire de Géologie Fondamentale et Appliquée, Faculté Polytechnique de Mons, B-7000 Mons, Belgium, Heilmann-Clausen, C.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark, Orús, A. H.; Eguzkialde 13, E-20271 Irura, Gipuzkoa, Spain, Knox, R.; British Geological Survey, Kingsley Durham Centre, Keyworth, Nottingham NG12 5GG, United Kingdom, Martín-Rubio, M.; Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain, Ortiz, S.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain, Payros, A.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Petrizzo, M. R.; Department of Earth Sciences, Milano University, 20133 Milano, Italy, von Salis, K.; Via Maistra 9, CH-7513 Silvaplana, Switzerland, Sprong, J.; Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium, Steurbaut, E.; Department of Paleontology, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium, Thomsen, E.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark, Department of Geology, Lund University, SE-22362 Lund, Sweden, Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain, Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain, Department of Earth Sciences, Florence University, 50121 Florence, Italy, Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium, Department of Geology, Rutgers University, Piscatatway, NJ 08854 USA., Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA, Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain, Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Laboratoire de Géologie Fondamentale et Appliquée, Faculté Polytechnique de Mons, B-7000 Mons, Belgium, Eguzkialde 13, E-20271 Irura, Gipuzkoa, Spain, British Geological Survey, Kingsley Durham Centre, Keyworth, Nottingham NG12 5GG, United Kingdom, Department of Earth Sciences, Milano University, 20133 Milano, Italy, Via Maistra 9, CH-7513 Silvaplana, Switzerland, Department of Paleontology, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium
Format: Article in Journal/Newspaper
Language:English
Published: IUGS 2011
Subjects:
Online Access:http://hdl.handle.net/2122/7307
id ftingv:oai:www.earth-prints.org:2122/7307
record_format openpolar
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic Chronostratigraphy
Cyclostratigraphy
pelagic succession
sea-level fall
04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating
processes
transport
04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy
spellingShingle Chronostratigraphy
Cyclostratigraphy
pelagic succession
sea-level fall
04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating
processes
transport
04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy
Schmitz, B.
Pujalte, V.
Molina, E.
Monechi, S.
Orue-Etxebarria, X.
Speijer, R. P.
Alegret, L.
Apellaniz, E.
Arenillas, I.
Aubry, M. P.
Baceta, J. I.
Berggren, W. A.
Bernaola, G.
Caballero, F.
Clemmensen, A.
Dinarès-Turell, J.
Dupuis, C.
Heilmann-Clausen, C.
Orús, A. H.
Knox, R.
Martín-Rubio, M.
Ortiz, S.
Payros, A.
Petrizzo, M. R.
von Salis, K.
Sprong, J.
Steurbaut, E.
Thomsen, E.
The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain
topic_facet Chronostratigraphy
Cyclostratigraphy
pelagic succession
sea-level fall
04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating
processes
transport
04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy
description The global stratotype sections and points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages have been defined in the coastal cliff along the Itzurun Beach at the town of Zumaia in the Basque Country, northern Spain. In the hemipelagic section exposed at Zumaia the base of the Selandian Stage has been placed at the base of the Itzurun Formation, ca. 49 m above the Cretaceous/ Paleogene boundary. At the base of the Selandian, marls replace the succession of Danian red limestone and limestone-marl couplets. The best marine, global correlation criterion for the basal Selandian is the second radiation of the important calcareous nannofossil group, the fasciculiths. Species such as Fasciculithus ulii, F. billii, F. janii, F. involutus, F.pileatus and F. tympaniformis have their first appearance in the interval from a few decimetres below up to 1.1 m above the base of the Selandian. The marker species for nannofossil Zone NP5, F. tympaniformis, first occurs 1.1 m above the base. Excellent cyclostratigraphy and magnetostratigraphy in the section creates further correlation potential, with the base of the Selandian occuring 30 precession cycles (630 kyr) above the top of magnetochron C27n. Profound changes in sedimentology related to a major sea-level fall characterize the Danian-Selandian transition in sections along the margins of the North Atlantic. The base of the Thanetian Stage is placed in the same section ca. 78 m above the Cretaceous/Paleogene boundary. It is defined at a level 2.8 m or eight precession cycles above the base of the core of the distinct clay-rich interval associated with the Mid-Paleocene Biotic Event, and it corresponds to the base of magnetochron C26n in the section. The base of the Thanetian is not associated with any significant change in marine micro-fauna or flora. The calcareous nannofossil Zone NP6, marked by the first occurrence of Heliolithus kleinpelli starts ca. 6.5 m below the base of the Thanetian. The definitions of the global stratotype ...
author2 Schmitz, B.; Department of Geology, Lund University, SE-22362 Lund, Sweden
Pujalte, V.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Molina, E.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain
Monechi, S.; Department of Earth Sciences, Florence University, 50121 Florence, Italy
Orue-Etxebarria, X.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Speijer, R. P.; Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium
Alegret, L.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain
Apellaniz, E.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Arenillas, I.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain
Aubry, M. P.; Department of Geology, Rutgers University, Piscatatway, NJ 08854 USA.
Baceta, J. I.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Berggren, W. A.; Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
Bernaola, G.; Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain
Caballero, F.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Clemmensen, A.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark
Dinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Dupuis, C.; Laboratoire de Géologie Fondamentale et Appliquée, Faculté Polytechnique de Mons, B-7000 Mons, Belgium
Heilmann-Clausen, C.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark
Orús, A. H.; Eguzkialde 13, E-20271 Irura, Gipuzkoa, Spain
Knox, R.; British Geological Survey, Kingsley Durham Centre, Keyworth, Nottingham NG12 5GG, United Kingdom
Martín-Rubio, M.; Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain
Ortiz, S.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain
Payros, A.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Petrizzo, M. R.; Department of Earth Sciences, Milano University, 20133 Milano, Italy
von Salis, K.; Via Maistra 9, CH-7513 Silvaplana, Switzerland
Sprong, J.; Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium
Steurbaut, E.; Department of Paleontology, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium
Thomsen, E.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark
Department of Geology, Lund University, SE-22362 Lund, Sweden
Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain
Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain
Department of Earth Sciences, Florence University, 50121 Florence, Italy
Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium
Department of Geology, Rutgers University, Piscatatway, NJ 08854 USA.
Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain
Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Laboratoire de Géologie Fondamentale et Appliquée, Faculté Polytechnique de Mons, B-7000 Mons, Belgium
Eguzkialde 13, E-20271 Irura, Gipuzkoa, Spain
British Geological Survey, Kingsley Durham Centre, Keyworth, Nottingham NG12 5GG, United Kingdom
Department of Earth Sciences, Milano University, 20133 Milano, Italy
Via Maistra 9, CH-7513 Silvaplana, Switzerland
Department of Paleontology, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium
format Article in Journal/Newspaper
author Schmitz, B.
Pujalte, V.
Molina, E.
Monechi, S.
Orue-Etxebarria, X.
Speijer, R. P.
Alegret, L.
Apellaniz, E.
Arenillas, I.
Aubry, M. P.
Baceta, J. I.
Berggren, W. A.
Bernaola, G.
Caballero, F.
Clemmensen, A.
Dinarès-Turell, J.
Dupuis, C.
Heilmann-Clausen, C.
Orús, A. H.
Knox, R.
Martín-Rubio, M.
Ortiz, S.
Payros, A.
Petrizzo, M. R.
von Salis, K.
Sprong, J.
Steurbaut, E.
Thomsen, E.
author_facet Schmitz, B.
Pujalte, V.
Molina, E.
Monechi, S.
Orue-Etxebarria, X.
Speijer, R. P.
Alegret, L.
Apellaniz, E.
Arenillas, I.
Aubry, M. P.
Baceta, J. I.
Berggren, W. A.
Bernaola, G.
Caballero, F.
Clemmensen, A.
Dinarès-Turell, J.
Dupuis, C.
Heilmann-Clausen, C.
Orús, A. H.
Knox, R.
Martín-Rubio, M.
Ortiz, S.
Payros, A.
Petrizzo, M. R.
von Salis, K.
Sprong, J.
Steurbaut, E.
Thomsen, E.
author_sort Schmitz, B.
title The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain
title_short The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain
title_full The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain
title_fullStr The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain
title_full_unstemmed The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain
title_sort global stratotype sections and points for the bases of the selandian (middle paleocene) and thanetian (upper paleocene) stages at zumaia, spain
publisher IUGS
publishDate 2011
url http://hdl.handle.net/2122/7307
genre North Atlantic
genre_facet North Atlantic
op_relation Episodes
4/34 (2011)
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spelling ftingv:oai:www.earth-prints.org:2122/7307 2023-05-15T17:36:55+02:00 The Global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages at Zumaia, Spain Schmitz, B. Pujalte, V. Molina, E. Monechi, S. Orue-Etxebarria, X. Speijer, R. P. Alegret, L. Apellaniz, E. Arenillas, I. Aubry, M. P. Baceta, J. I. Berggren, W. A. Bernaola, G. Caballero, F. Clemmensen, A. Dinarès-Turell, J. Dupuis, C. Heilmann-Clausen, C. Orús, A. H. Knox, R. Martín-Rubio, M. Ortiz, S. Payros, A. Petrizzo, M. R. von Salis, K. Sprong, J. Steurbaut, E. Thomsen, E. Schmitz, B.; Department of Geology, Lund University, SE-22362 Lund, Sweden Pujalte, V.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Molina, E.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain Monechi, S.; Department of Earth Sciences, Florence University, 50121 Florence, Italy Orue-Etxebarria, X.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Speijer, R. P.; Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium Alegret, L.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain Apellaniz, E.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Arenillas, I.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain Aubry, M. P.; Department of Geology, Rutgers University, Piscatatway, NJ 08854 USA. Baceta, J. I.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Berggren, W. A.; Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA Bernaola, G.; Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain Caballero, F.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Clemmensen, A.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark Dinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Dupuis, C.; Laboratoire de Géologie Fondamentale et Appliquée, Faculté Polytechnique de Mons, B-7000 Mons, Belgium Heilmann-Clausen, C.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark Orús, A. H.; Eguzkialde 13, E-20271 Irura, Gipuzkoa, Spain Knox, R.; British Geological Survey, Kingsley Durham Centre, Keyworth, Nottingham NG12 5GG, United Kingdom Martín-Rubio, M.; Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain Ortiz, S.; Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain Payros, A.; Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Petrizzo, M. R.; Department of Earth Sciences, Milano University, 20133 Milano, Italy von Salis, K.; Via Maistra 9, CH-7513 Silvaplana, Switzerland Sprong, J.; Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium Steurbaut, E.; Department of Paleontology, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium Thomsen, E.; Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark Department of Geology, Lund University, SE-22362 Lund, Sweden Department of Stratigraphy and Paleontology, University of the Basque Country, E-48080 Bilbao, Spain Department of Earth Sciences, Zaragoza University, E-50009 Zaragoza, Spain Department of Earth Sciences, Florence University, 50121 Florence, Italy Department of Earth and Environmental Sciences, K.U. Leuven, B-3001 Leuven, Belgium Department of Geology, Rutgers University, Piscatatway, NJ 08854 USA. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA Department of Mining and Metallurgic Engineering and Material Sciences, University of the Basque Country, E-48901 Barakaldo, Spain Department of Earth Sciences, Århus University, DK-8000 Århus C, Denmark Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Laboratoire de Géologie Fondamentale et Appliquée, Faculté Polytechnique de Mons, B-7000 Mons, Belgium Eguzkialde 13, E-20271 Irura, Gipuzkoa, Spain British Geological Survey, Kingsley Durham Centre, Keyworth, Nottingham NG12 5GG, United Kingdom Department of Earth Sciences, Milano University, 20133 Milano, Italy Via Maistra 9, CH-7513 Silvaplana, Switzerland Department of Paleontology, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium 2011-12 http://hdl.handle.net/2122/7307 en eng IUGS Episodes 4/34 (2011) Adatte, T., Bolle, M.P., de Kaenel, E., Gawenda, P., Winkler, W. and von Salis, K., 2000. 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Shell Internationale Petroleum Maatschappij, B.V., Den Haag, 239 pp. http://hdl.handle.net/2122/7307 restricted Chronostratigraphy Cyclostratigraphy pelagic succession sea-level fall 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating processes transport 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy article 2011 ftingv 2022-07-29T06:06:05Z The global stratotype sections and points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) stages have been defined in the coastal cliff along the Itzurun Beach at the town of Zumaia in the Basque Country, northern Spain. In the hemipelagic section exposed at Zumaia the base of the Selandian Stage has been placed at the base of the Itzurun Formation, ca. 49 m above the Cretaceous/ Paleogene boundary. At the base of the Selandian, marls replace the succession of Danian red limestone and limestone-marl couplets. The best marine, global correlation criterion for the basal Selandian is the second radiation of the important calcareous nannofossil group, the fasciculiths. Species such as Fasciculithus ulii, F. billii, F. janii, F. involutus, F.pileatus and F. tympaniformis have their first appearance in the interval from a few decimetres below up to 1.1 m above the base of the Selandian. The marker species for nannofossil Zone NP5, F. tympaniformis, first occurs 1.1 m above the base. Excellent cyclostratigraphy and magnetostratigraphy in the section creates further correlation potential, with the base of the Selandian occuring 30 precession cycles (630 kyr) above the top of magnetochron C27n. Profound changes in sedimentology related to a major sea-level fall characterize the Danian-Selandian transition in sections along the margins of the North Atlantic. The base of the Thanetian Stage is placed in the same section ca. 78 m above the Cretaceous/Paleogene boundary. It is defined at a level 2.8 m or eight precession cycles above the base of the core of the distinct clay-rich interval associated with the Mid-Paleocene Biotic Event, and it corresponds to the base of magnetochron C26n in the section. The base of the Thanetian is not associated with any significant change in marine micro-fauna or flora. The calcareous nannofossil Zone NP6, marked by the first occurrence of Heliolithus kleinpelli starts ca. 6.5 m below the base of the Thanetian. The definitions of the global stratotype ... Article in Journal/Newspaper North Atlantic Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Paleoceanography 26 2 n/a n/a