The proposal of a GSSP for the Berriasian Stage (Cretaceous System): Part 2

• Autorzy: Wimbledon William A.P. , Reháková Daniela , Svobodová Andrea , Elbra Tiiu , Schnabl Petr , Pruner Petr , Šifnerová Krýstina , Kdýr Šimon , Frau Camille , Schnyder Johann , Galbrun Bruno , Vaňková Lucie , Dzyuba Oksana , Copestake Philip , Hunt Christopher O. , Riccardi Alberto , Poulton Terry P. , Bulot Luc G. , De Lena Luis

Identyfikatory

DOI

10.7306/VJ.18.7

• Języki publikacji: EN

Abstrakty

EN

In part 1 of this work we discussed the possibilities for the selection of a GSSP for the Berriasian Stage of the Cretaceous System, based on prevailing practical methods for correlation in that J/K interval, traditional usage and the consensus over the best boundary markers that had developed in the last forty years. This consensus has developed further, based on the results of multidisciplinary studies on numerous sites over the last decade. Here in Part 2 we give an account of the application of those results by the Berriasian Working Group (ISCS), and present the stratigraphic evidence that justifies the selection of the locality of Tré Maroua (Hautes-Alpes, SE France) as the proposed GSSP. We describe a 45 m-thick section in the Calcaires Blancs vocontiens – that part of the formation covering the calpionellid Chitinoidella, Remanei. Intermedia, Colomi, Alpina, Ferasini, Elliptica and Simplex biozones. The stratigraphic data collected here has been compiled as part of a wider comparative study of complementary Vocontian Basin sites (with localities at Charens, St Bertrand, Belvedere and Le Chouet). Evidence from Tré Maroua thus sits in this substantial regional biostratigraphic and magnetostratigraphic context. For the purposes of the GSSP definition, here we particularly concentrate on the unbroken sequence and biotic markers in the interval immediately below the boundary, the Colomi Subzone (covering circa 675,000 years), and immediately above, the Alpina Subzone (covering circa 725,000 years). Particularly significant fossil datums identified in the Tré Maroua profile are the primary basal Berriasian marker, the base of the Alpina Subzone (a widespread event marked by dominance of small Calpionella alpina, with rare Crassicollaria parvula and Tintinopsella carpathica): the base of the Berriasian Stage is placed at the base of bed 14, which coincides with the base of the Alpina Subzone. Secondary markers bracketing the base of the Calpionella Zone are the FOs of the calcareous nannofossil species Nannoconus wintereri, close below the boundary, and the FO of Nannoconus steinmannii minor, close above. The Tithonian/Berriasian boundary level occurs within M19n.2n, in common with many documented sites, and is just below the distinctive reversed magnetic subzone M19n.1r (the so-called Brodno reversal). We present data which is congruent with magnetostratigraphic and biostratigraphic data from other key localities in France and in wider regions (Le Chouet, Saint Bertrand, Puerto Escaño, Rio Argos, Bosso, Brodno, Kurovice, Theodosia…), and thus the characteristics and datums identified at Tré Maroua are key for correlation and, in general, they typify the J/K boundary interval in Tethys and connected seas

Słowa kluczowe

EN

Cretaceous; GSSP; biostratigraphy; magnetostratigraphy; Vocontian Basin; Berriasian stages

PL

Kreda; GSSP; biostratygrafia; magnetostratygrafia

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Volumina Jurassica
• Rocznik: 2020
• Tom: Vol. 18, no. 2
• Strony: 121--160
• Opis fizyczny: Bibliogr. 148 poz.

Twórcy

autor

Wimbledon William A.P.

• School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, United Kingdom

autor

Reháková Daniela

• Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University, Ilkovičova 6, 84215 Bratislava, Slovakia

autor

Svobodová Andrea

• The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic

autor

Elbra Tiiu

• The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic

autor

Schnabl Petr

• The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic

autor

Pruner Petr

• The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic

autor

Šifnerová Krýstina

• The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic

autor

Kdýr Šimon

• The Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague, Czech Republic

autor

Frau Camille

• Groupement d’Intérêt Paléontologique, Science et Exposition, 60 bd Georges Richard, 83000 Toulon, France

autor

Schnyder Johann

• Sorbonne Université, UPMC Université Paris 06, CNRS, Institut des Sciences de la Terre Paris (ISTeP), 75005 Paris, France

autor

Galbrun Bruno

• Sorbonne Université, UPMC Université Paris 06, CNRS, Institut des Sciences de la Terre Paris (ISTeP), 75005 Paris, France

autor

Vaňková Lucie

• Institute of Geology and Palaeontology, Faculty of Science, Charles University, Albertov 6, Prague 2, 128 43, Czech Republic

autor

Dzyuba Oksana

• Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of RAS, Acad. Koptyug av. 3, Novosibirsk 630090, Russia

autor

Copestake Philip

• Merlin Energy Resources Ltd., New Street, Ledbury, Herefordshire, HR8 2EJ, United Kingdom

autor

Hunt Christopher O.

• School of Biological & Environmental Sciences, Liverpool John Moores University, Byrom St., Liverpool L3 3AH, United Kingdom

autor

Riccardi Alberto

• CONICET – Museo de La Plata, Universidad Nacional de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina

autor

Poulton Terry P.

• Geological Survey of Canada, Calgary, Alberta, T2L 2Al, Canada

autor

Bulot Luc G.

• Aix-Marseille Université, CNRS, IRD, INRAE, Collège de France, Cerege, Site Saint-Charles, Case 67, 3, Place Victor Hugo, 13331 Marseille Cedex 3, France
• NARG, School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Williamson Building, Oxford Road, Manchester M13 9PL, United Kingdom

autor

De Lena Luis

• Department of Earth Sciences, University of Geneva, Geneva, 1205, Switzerland

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Uwagi

Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2020).