Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-16T21:16:36.708Z Has data issue: false hasContentIssue false
  • English
  • Français

Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands)

Published online by Cambridge University Press:  01 April 2016

E. Wijnker ,
T.J. Bor ,
F.P. Wesselingh ,
D.K. Munsterman ,
H. Brinkhuis ,
A.W. Burger ,
H.B. Vonhof ,
K. Post ,
K. Hoedemakers  and
A.C. Janse
...Show all authors
E. Wijnker*
Affiliation:
Laboratory of Genetics, Wageningen University, Arboretumlaan 4, 6703 BD Wageningen, the Netherlands.
T.J. Bor
Affiliation:
Prinsenweer 54, 3363 JK Sliedrecht, the Netherlands.
F.P. Wesselingh
Affiliation:
Naturalis P.O. Box 9517, 2300 RA Leiden, the Netherlands.
D.K. Munsterman
Affiliation:
TNO B&O - National Geological Survey, P.O. Box 80015, 3508 TA Utrecht, the Netherlands.
H. Brinkhuis
Affiliation:
Palaeocecology, Inst. Environmental Biology, Laboratory of Pataeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands.
A.W. Burger
Affiliation:
P. Soutmanlaan 18, 1701 MC Heerhugowaard, the Nethertands.
H.B. Vonhof
Affiliation:
Faculty Earth and Life Sciences, Vrije Universiteit, de Boelelaan 1085, 1081 EH Amsterdam, the Netherlands.
K. Post
Affiliation:
Natuurmuseum Rotterdam P.O. Box 23452, 3001 KL Rotterdam, the Netherlands.
K. Hoedemakers
Affiliation:
Minervastraat 23, B 2640 Mortsel, Belgium.
A.C. Janse
Affiliation:
Gerard van Voornestraat 165, 3232 BE Brielle, the Netherlands.
N. Taverne
Affiliation:
Snipweg 14, 5451 VP Mill, the Netherlands.
*
*corresponding author. Email:[email protected]
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

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).

Keywords

Breda FormationMillMioceneNorth Sea BasinOosterhout FormationPliocene
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 87 , Issue 2 , August 2008 , pp. 165 - 180
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2008

References

Adams, C., Benson, R. Kidd, R. Ryan, W. & Wright, R., 1977. The Messinian salinity crisis and evidence of late Miocene eustatic changes in the world ocean. Nature 269: 383–386.CrossRefGoogle Scholar
Ahrens, H., 2003. Een kies van de mastodont Anancus arvemensis uit het Plioceen van Noord-Brabant (online). Available from: www.pleistocenemammals.com/nieuwsitems/anancus/anancus.htm (Accessed 28 September 2006).Google Scholar
Ahrens, H., 2004. Vier nieuwe fossielen van landzoogdieren uit Langenboom (online). Available from: www.pleistocenemammals.com/nieuwsitems/langenboom/langenboom.htm (Accessed 28 September 2006).Google Scholar
Ahrens, H., 2005. Weer een schedel van Protophocacena minima erbij! Cranium 22: 41–44.Google Scholar
Baldauf, J.G., Thomas, E., Clement, B., Takayama, T.., Weaver, P.P.E., Backman, J., Jenkins, G. Mudie, P.J. & Westberg-Smith, M.J., 1987. Magnetostratigraphic and biostratigraphic synthesis, Deep Sea Drilling Project, Leg 94. Initial Reports of the Deep Sea Drilling Project 94: 1159–1205.Google Scholar
Burger, A.W., 2006. Mollusken van groeve de Kuilen, Langenboom. Kbl. 45F coörd. 179.9/412.3 (online). Available from: www.wtkg.org/langenboom.htm (Accessed 28 September 2006).Google Scholar
Codée, M.C., 1988. Astarte trigonata ook in het Midden Plioceen. Afzettingen 9: 3–6.Google Scholar
De Schepper, S., Head, M.J., & Louwye, S., 2004. New dinoflagellate cyst and incertae sedis taxa from the Pliocene of northern Belgium, Southern North Sea Basin. Journal of Paleontology 78 (4): 625–644.2.0.CO;2>CrossRefGoogle Scholar
De Schepper, S., 2006, Plio-Pleistocene dinoflagellate cyst biostratigraphy and palaeoecology of the eastern North Atlantic and southern North Sea Basin. Unpublished PhD thesis. University of Cambridge: i–xvii + 306 pp.Google Scholar
De Vos, J. & Wijnker, E., 2006. A deer (Cervus rhenanus) from the Early Pliocene of Langenboom, Noord-Brabant (the Netherlands). Cainozoic Research 5: 107–110.Google Scholar
Doppert, J.W.C., Ruegg, G.H.J.. Van Staalduinen, C.J., Zagwijn, W.H. & Zandstra, J.G., 1975. Formaties van het Kwartair en Boven-Tertiair in Nederland. In: Zagwijn, W.H. & Van Staalduinen, C.J. (eds): Toelichting bij geologische overzichtskaarten van Nederland. Rijks Geologische Dienst (Haarlem): 11–56.Google Scholar
Ebbing, J.H.J. & De Lang, F.D., 2003. Formatie van Oosterhout. In: TNO-NITG. Lithostratigrafische nomenclator ondiepe ondergrond Nederland (online). Available from: www.nitg.tno.nl/nomenclatorShallow/start/start/introduction/index.html (Accessed 5 November 2006).Google Scholar
Faure, M., 2004. Le Sus strozzii du Pliocène final de Saint-Vallier (Drôme). Geobios 37: 189–190.CrossRefGoogle Scholar
Foekens, R., 2006. Ancient secrets from Mill disclosed. Determination of fossil periotics from Mio/Pliocene dolphins (Mammalia, Cetacea, Odontoceti) from the Dutch site Mill on family, genus and species level. MSc thesis, Leiden University. Leiden, the Netherlands: 51 pp.Google Scholar
Gladenkav, A.Y., Oleinik, A.E., Marincovich, L. Jr. & Barinov, K.B., 2002. A refined age for the earliest opening of Bering Strait. Palaeogeography, Palaeoclimatology, Palaeoecology 183; 321–328.CrossRefGoogle Scholar
Gliozzi, E., Abbozzi, L., Argenti, P., Azzardi, A., Caloi, L., Capasso Barbato, L. Di Stefano, G. Esu, D., Fitcarelli, G., Girotti, O., Kotsakis, T., Masini, F., Mazza, P., Mezzabotta, C., Palombo, M.R., Petronio, C., Rook, L., Sala, B., Sardella, R., Zanalda, E., & Torre, D., 1997. Biochronology of selected mammals, molluscs and ostracods from the middle Pliocene to the latest Pleistocene in Italy. The state of the art. Rivista Italiana di Paleontologia e Stratigrafia 103: 369–383.Google Scholar
Gradstein, F.M., Ogg, J.G. & Smith, A.G., 2004. A Geologic Time Scale 2004. Cambridge University Press: 589 pp.CrossRefGoogle Scholar
Grémare, A., Sardá, R., Medernach, L., Jordana, E., Pinedo, S., Amouraux, J.M., Martin, D., Nozais, C. & Charles, F., 1998. On the dramatic increase of Ditrupa arietina O.F. Muller (Annelida, Polychaeta) along both the French and Spanish Catalan coasts. estuarine, Coastal and Shelf Science 47: 447–457.CrossRefGoogle Scholar
Head, M.J. 1997. Thermophilic dinoflagellate assemblages from the mid Pliocene of eastern England. Journal of Paleontology 71: 165–193.CrossRefGoogle Scholar
Head, M.J., 1998. Marine environmental change in the Pliocene and early Pleistocene of eastern England: the dinoflagellate evidence reviewed. In: Van Kolfschoten, Th. & Gibbard, P.L.: The dawn of the Quaternary. Mededelingen NITG TNO 60: 199–226.Google Scholar
Head, M.J., 1999. The Late Pliocene St. Erth Beds of Cornwall: a review of the palynology and reappraisal of the dinoflagellates. In: Scourse, J. and Furze, M.F.A. (eds): The Quaternary of West Cornwall, Field guide. Quaternary Research Association (Durham): 88–92.Google Scholar
Head, M.J. & Norris, G., 2003. New species of dinoflagellate cysts and other palynomorphs from the latest Miocene and Pliocene of DSDP hole 603C, western North Atlantic. Journal of Paleontology 77: 1–15.2.0.CO;2>CrossRefGoogle Scholar
Hodell, D.A. & Kennett, J.P., 1986, Late Miocene- early Pliocene stratigraphy and paleoceanography of the South Atlantic and southwest Pacific Ocean: A synthesis. Paleoceanography 1: 285–311.CrossRefGoogle Scholar
Janse, A.C., 1985. Van de geologisch secretaris. Afzettingen 6: 99–101.Google Scholar
Johnson, A.L.A., Hickson, J.A., Swan, J., Brown, M.R.. Heaton, T.H.E., Chenery, S. & Balson, P.S., 2000. The Queen Scallop Aequipecten opercularis: a new source of information on late Cenozoic marine environments in Europe. In: Harper, E.M., Taylor, J.D. & Crame, J.A. (eds): The evolutionary biology of the Bivalvia, Geological Society special publication 177, The Geological society (London): 425–439.Google Scholar
Kim, S.T. & O’Neil, J.R., 1997. Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates. Geochimica et Cosmochimica Acta 61: 3461–3475.CrossRefGoogle Scholar
Kuhlmann, G., Langereis, C.G., Munsterman, D.K., van Leeuwen, R.-J., Verreussel, R.; Meulenkamp, J.E. & Wong, Th.E., 2006. Integrated chronostratigraphy of the Pliocene-Pleistocene interval and its relation to the regional stratigraphical stages in the southern North Sea region. Netherlands Journal of Geosciences 85: 19–35.CrossRefGoogle Scholar
Louwye, S., 2002. Dinoflagellate cyst biostratigraphy of Upper Miocene Deurne Sands (Diest Formation) of northern Belgium, southern North Sea Basin. Geological Journal 37: 55–67.CrossRefGoogle Scholar
Louwye, S., Head, M.J. & De Schepper, S., 2004. Dinoflagellate cyst stratigraphy and palaeoecology of the Pliocene in northern Belgium, southern North Sea Basin. Geological Magazine 141: 353–378.CrossRefGoogle Scholar
Louwye, S., De Schepper, S., Laga, P. & Vandenberghe, N., 2007. The Upper Miocene of the southern North Sea Basin (northern Belgium): a palaeoenvironmental and stratigraphical reconstruction using dinoflagellate cysts. Geological Magazine: 144(1): 33–52.CrossRefGoogle Scholar
Marincovich, L. Jr. & Gladenkov, A.Y., 20O1. New evidence for the age of the Bering Strait. Quaternary Science Reviews 20: 329–335.CrossRefGoogle Scholar
Marquet, R., 1998, De Pliocene gastropodenfauna van Kallo. Belgische Vereniging voor Paleontologie, publicatie 17 (Antwerpen): 246 pp.Google Scholar
Marquet, R., 2005. The Neogene Bivalvia (Heterodonta and Anomalodesmata) and Scaphopoda from Kallo and Doel (Oost-Vlaanderen, Belgium). Palaeontos 6: 1–142.Google Scholar
Meijer, H.J.M., 2004. The first record of birds from Mill (the Netherlands). www.palarch.nl, Vertebrate Palaeontology 1(2): 8–13.Google Scholar
Meijer, T., Cleveringa, P., Munsterman, D.K. & Verreussel, R.M.C.H., 2006. The Early Pleistocene Praetiglian and Ludhamian pollen stages in the North Sea Basin and their relationship to the marine isotope record. Journal of Quaternary Science 21: 307–310.CrossRefGoogle Scholar
Munsterman, D.K. & Brinkhuis, H., 2004. A southern North Sea Miocene dinoflagellate cyst zonation. Netherlands Journal of Geosciences 83: 267–285.CrossRefGoogle Scholar
Nolf, D., 1982. Otolithi Piscium. In: Schultze, H.P. (ed.): Handbook of Paleoichthyology 10. Fischer Verlag (Stuttgart-New York): 145 pp.Google Scholar
Half, D., 1978. Les otolithes des Téléostéens du Plio-Pleistocène belge. Géobios 11(4); 517–559.Google Scholar
Powell, A.J., 1992. Dinoflagellate cysts of the Tertiary System. In: Powell, A.J. (ed.): A stratigraphic index of dinoflagellate cysts. British Micropalaeontological Society Publication Series. Chapman and Hall (London): 155–272.CrossRefGoogle Scholar
Schokker, J., De Lang, F.D., Weerts, H.J.T. & Den Otter, C. 20O3. Formatie van Boxtel In: TNO-NITG. Lithostratigrafische nomenclator ondiepe ondergrond Nederland (online). Available from: www.nitg.tno.nl/nomenclatorShallow/nl/overig/boxtel/index.html (Accessed 5 November 2006).Google Scholar
Spaink, G., 1975. Zonering van het mariene Onder-Pleistoceen en Plioceen op grond van mollusken fauna’s. In: Zagwijn, W.H. & Van Staalduinen, C.J., (eds): Toelichting bij geologische overzichtskaarten van Nederland. Rijks Geologische Dienst (Haarlem): 118–122.Google Scholar
Van Rooijen, P., Klostermann, J., Doppen, J.W.Chr., Rescher, C.K., Verbeek, J.W., Sliggers, B.C. & Glasbergen, P., 1984. Stratigraphy and tectonics in the Peel-Venlo area as indicated by Tertiary sediments in the Broekhuizenvorst and Geldern T1 boreholes. Mededelingen RGD, 38(1): 1–27.Google Scholar
Vonhof, H.B., Wesselingh, F.P., Kaandorp, R.G.J., Davies, G.R., van Hinte, J.E., Guerrero, J., Räsänen, M., Romero-Pitmann, L., & Ranzi, A., 2003. Paleogeography of Miocene western Amazonia: isotopic composition of molluscan shells constrains the influence of marine incursions. Geological Society of America Bulletin 115: 983–993.CrossRefGoogle Scholar
Wesselingh, F., 1986. Najaarsexcursie. Afzettingen 7: 2–3.Google Scholar
Westerhoff, W.E., 2003. Formatie van Breda. In: TNO-NITG. Lithostratigrafische nomenclator ondiepe ondergrond Nederland (online). Available from: www.nitg.tno.nl/nomenclatorShallow/start/start/introduction/index.html (Accessed 5 November 2006).Google Scholar
Westerhoff, W.E. & Weerts, H.J.T., 2003a. Formatie van Beegden. In: TNO-NITG, Lithostratigrafische nomenclator ondiepe ondergrond Nederland (online). Available from: www.nitg.tno.nl/nomenclatorShallow/nl/fluviatiel/beegden/index.html (Accessed 5 November 2006).Google Scholar
Westerhoff, W.E. & Weerts, H.J.T.. 2003b. Formatie van Waalre, In: TNO-NITG. Lithostratigrafische nomenclator ondiepe ondergrond nederland (online). Available from: www.nitg.tno.nl/namenclatorShallow/nl/fluviatiel/waalre/index.html (Accessed 5 November 2006).Google Scholar
Wijnker, E., 2005. Miocene and Pliocene marine birds from Mill, the Netherlands. Unpublished MSc thesis, Wageningen University, Wageningen, the Netherlands: 125 pp.Google Scholar
Williams, G.L., Brinkhuis, H., Pearce, M.A., Fensome, R.A., & Weegink, J.W.. 2004. Southern Ocean and global dinoflagellate cyst events compared: index events for the Late Cretaceous-Neogene. In: Exon, N.F., Kennett, J.P., & Malone, M.J. (eds): Proceedings of the Ocean Drilling Program, Scientific Results, 189 (Online), Available from: www-odp.tamu.edu/publications/189_SR/107/107.htm (Accessed 24 November 2006).CrossRefGoogle Scholar
Wood, S.V., 1848. A monograph of the Crag Mollusca with descriptions of shells from the upper Tertiaries of the British Isles. Palaeontographical Society (London): 208 pp.Google Scholar
Zagwijn, W.H. & Hager, H., 1987. Correlations of continental and marine Neogene deposits in the south-eastern Netherlands and the Lower Rhine District. In: Janssen, A.W. (ed.): Proceedings of the third meeting of R.C.N.N.S. (Regional Committee on Northern Neogene Stratigraphy) at Leiden, the Netherlands 5–7 November 1986. Mededelingen van de werkgroep voor Tertiaire en Kwartaire Geologie 24: 59–78.Google Scholar
Ziegler, P., 1980. North Western Europe: Subsidence patterns of Post-Variscan basins. In: Cogné, J. & Slansky, M. (eds): Geology of Europe from the Precambrian to the Post-Hercynian Sedimentary Basis. Memoires du Bureau de recherches geologiques et minieres, 108: 249–280.Google Scholar