A global view on the Ordovician stratigraphy of southeastern Europe

Author:

Ferretti Annalisa1ORCID,Schönlaub Hans Peter2,Sachanski Valeri34,Bagnoli Gabriella5,Serpagli Enrico1,Vai Gian Battista6,Yanev Slavcho4,Radonjić Miloš7,Balica Constantin8,Bianchini Luca1,Colmenar Jorge9,Gutiérrez-Marco Juan Carlos10

Affiliation:

1. Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, Via Campi 103, I-41125 Modena, Italy

2. Commission for Geosciences, Austrian Academy of Sciences, Dr. Ignaz Seipel-Platz 2, A-1010 Vienna, Austria

3. Department of Geology and Geoinformatics, University of Mining and Geology, Studentski Grad, Prof. Boyan Kamenov Str., BG-1700 Sofia, Bulgaria

4. Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., Bl. 24, BG-1113 Sofia, Bulgaria

5. Department of Earth Sciences, University of Pisa, Via Santa Maria 53, I-56126 Pisa, Italy

6. Department of Biological, Geological and Environmental Sciences, University of Bologna, Piazza di Porta San Donato 1, I-40126 Bologna, Italy

7. Department of Regional Geology, Faculty of Mining and Geology, University of Belgrade, Kamenička 6, 11000 Belgrade, Serbia

8. Department of Geology, Faculty of Biology and Geology, ‘Babeş-Bolyai’ University, Strada M. Kogălniceanu 1, 400084 Cluj-Napoca, Romania

9. Instituto Geológico y Minero de España (IGME-CSIC), La Calera 1, E-28760 Tres Cantos, Spain

10. Departamento GEODESPAL, Facultad de Ciencias Geológicas, Instituto de Geociencias (CSIC, UCM), José Antonio Nováis 12, E-28040 Madrid, Spain

Abstract

AbstractThe Ordovician documented in southeastern Europe reflects different sedimentary environments, from shallow water to basin, belonging to diverse palaeogeographical domains. Some of these geological sectors and their palaeontological content have been well described for a long time such as the Carnic Alps, which represent one of the most continuous Paleozoic sequences in the world. For some other areas, the quality of the data is variable and the knowledge is less detailed, sometimes with lithostratigraphic units still to be formalized, which also reflects the fragmentary nature of the outcrops. The Ordovician stratigraphy of southeastern Europe with its diverse successions has been revised herein and integrated with new data in an attempt to develop a global scenario for this critical time interval in the evolution of life.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference264 articles.

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2. First record of Ordovician (Upper Arenigian, Acritarchs) beds in Bakony Mts., Hungary;Albani R.;Neues Jahrbuch für Geologie und Paläontologie Abhandlungen,1985

3. Pre-Alpine evolution of a segment of the North-Gondwanan margin: Geochronological and geochemical evidence from the central Serbo-Macedonian Massif

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5. Antonović, A., Popović, R. and Stojanović-Kuzenko, S. 1966. Ordoviziumska trilobitska fauna na Stogovo [Ordovician trilobite fauna from Stogovo]. In: Stračkov, M., Ivanov, T. and Stojanov, R. (eds) Referati 6th kongresa geologa Jugoslavije, Тom 1 [Proceedings of the 6th Geological Congress of Yugoslavia, Ohrid, Volume 1], 370–372 [in Macedonian].

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