Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands)
| Autor: | Erik Wijnker, Henk Brinkhuis, Hubert B. Vonhof, K. Hoedemakers, A.C. Janse, N. Taverne, T.J. Bor, A.W. Burger, F.P. Wesselingh, Dirk K. Munsterman, K. Post |
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| Přispěvatelé: | TNO Bouw en Ondergrond, Sedimentology |
| Rok vydání: | 2008 |
| Předmět: |
Piacenzian
Pliocene sequence stratigraphy Benelux Teleostei 010502 geochemistry & geophysics 01 natural sciences palaeozoology North Sea Basin Atlantic Ocean Chondrichthyes Netherlands Geology fossil record Europe Breda formation Mill Benthic zone Mammalia Laboratory of Genetics biostratigraphy North Sea upper miocene north-sea basin Aves Geosciences skeletal remains geology 010506 paleontology Pleistocene tektoniek Western Europe Context (language use) Biostratigraphy Laboratorium voor Erfelijkheidsleer Neogene bering strait dinoflagellate cyst noord-brabant Dinophyceae Paleontology geologie tectonics Sequence stratigraphy Oosterhout formation 0105 earth and related environmental sciences Zanclea paleozoölogie belgium Miocene age Mollusca Eurasia North Brabant pleistocene Quaternary |
| Zdroj: | Scopus-Elsevier Netherlands Journal of Geosciences = Geologie en Mijnbouw, 87(2), 165-180. Koninklijk Nederlands Geologisch Mijnbouwkundig Genootschap Geologie en Mijnbouw/Netherlands Journal of Geosciences, 2, 87, 165-180 Geologie en Mijnbouw, 87(2), 165-180 Geologie en Mijnbouw 87 (2008) 2 Wijnker, E, Bor, T J, Wesselingh, F P, Munsterman, D K, Brinkhuis, H, Burger, A W, Vonhof, H B, Post, K, Hoedemakers, K, Janse, A C & Taverne, N 2008, ' Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands) ', Netherlands Journal of Geosciences = Geologie en Mijnbouw, vol. 87, no. 2, pp. 165-180 . https://doi.org/10.1017/S0016774600023209 |
| ISSN: | 1573-9708 0016-7746 |
| DOI: | 10.1017/s0016774600023209 |
| Popis: | The locality of Langenboom (eastern Noord-Brabant, the Netherlands), also known as Mill, is famous for its Neogene molluscs, shark teeth, teleost remains, birds and marine mammals. The stratigraphic context of the fossils, which have been collected from sand suppletions, was hitherto poorly understood. Here we report on a section which has been sampled by divers in the adjacent flooded sandpit ‘De Kuilen’ from which the Langenboom sands have been extracted. The studied section covers part of the marine Miocene Breda Formation and Pliocene Oosterhout Formation, and is topped by fluvial Quaternary deposits of presumably the Beegden Formation. The Breda Formation (15 – 18 m below lake surface) in this section is, based on organic walled dinoflagellate cysts, of an early-middle Tortonian age. The Oosterhout Formation (7 – 15 m below lake surface) comprises two depositional sequences, the lower of which (12 – 15 m below lake surface) presumably is the source of most Langenboom fossils. Combined dinoflagellate cyst and benthic mollusc indicators point to an early Zanclean - early Piacenzian age for this lower cycle. Its basal transgressive lag and (to lesser extent) top comprise reworked Tortonian taxa as well, Dinoflagellate cysts and a single benthic mollusc point to a Piacenzian age for the upper Oosterhout Formation sequence (7 – 12 m below lake surface). |
| Databáze: | OpenAIRE |
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