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The role of a proto-Schelde River in the genesis of the southwestern Netherlands, inferred from the Quaternary successions and fossils in Moriaanshoofd Borehole (Zeeland, the Netherlands)

Published online by Cambridge University Press:  24 March 2014

A.A. Slupik ,
F.P. Wesselingh ,
D.F. Mayhew ,
A.C. Janse ,
F.E. Dieleman ,
M. van Strydonck ,
P. Kiden ,
A.W. Burger  and
J.W.F. Reumer
A.A. Slupik*
Affiliation:
Natuurhistorisch Museum Rotterdam, Westzeedijk 345, 3015 AA Rotterdam, the Netherlands
F.P. Wesselingh
Affiliation:
Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, the Netherlands
D.F. Mayhew
Affiliation:
Natuurhistorisch Museum Rotterdam, Westzeedijk 345, 3015 AA Rotterdam, the Netherlands Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, the Netherlands
A.C. Janse
Affiliation:
Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, the Netherlands
F.E. Dieleman
Affiliation:
Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, the Netherlands
M. van Strydonck
Affiliation:
Koninklijk Instituut voor het Kunstpatrimonium, Jubelpark 1, 1000 Brussel, Belgium
P. Kiden
Affiliation:
TNO – Geological Survey of the Netherlands, P.O. Box 80015, 3508 AL Utrecht, the Netherlands
A.W. Burger
Affiliation:
P. Soutmanlaan 18, 1701 MC Heerhugowaard, the Netherlands
J.W.F. Reumer
Affiliation:
Natuurhistorisch Museum Rotterdam, Westzeedijk 345, 3015 AA Rotterdam, the Netherlands Department of Geosciences, Utrecht University, P.O. Box 80021, 3508 TA Utrecht, the Netherlands
*
Email: [email protected]
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Abstract

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We investigated the Quaternary lithological succession and faunas in a borehole near Moriaanshoofd (Province of Zeeland, SW Netherlands), in order to improve our understanding of the depositional context of classical Gelasian mammal faunas from the region. The fossils mostly derive from the base of a fossil-rich interval between 31 m and 36.5 m below the surface, that was initially interpreted as a Middle or Late Pleistocene interglacial marine unit, but turned out to be a Late Quaternary fluvial unit with large amounts of reworked fossils and sediments. Eocene mollusc taxa pinpoint Flanders (Belgium) as the source region for this river. Within the base of this paleo-Schelde River fossil material of various stratigraphic provenance became incorporated.

Keywords

PleistoceneEocenestratigraphyreworkingScheldemammalsmolluscs
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 92 , Issue 1 , April 2013 , pp. 69 - 86
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2013

References

Bosch, J.H.A, 1999. Standaard Boor Beschrijvingsmethode, versie 5. Internal report TNO, rapport NITG 98-205-A, 88 pp.Google Scholar
Briant, R.M., Bateman, M.D., Coope, G.R. & Gibbard, P.L., 2005. Climatic control on Quaternary fluvial sedimentology of a Fenland Basin river, England. Sedimentology 52: 1397–1423.Google Scholar
Busschers, F.S., 2008. Unravelling the Rhine. Response of a fluvial system to climate change, sea-level oscillation and glaciations. PhD thesis, Vrije Universiteit Amsterdam, 183 pp.Google Scholar
Busschers, F.S. & Weerts, H.J.T, 2003. Formatie van Kreftenheye. In: Lithostrati grafische Nomenclator van de Ondiepe Ondergrond. Retrieved 2013 from www.dinoloket.nl/formatie-van-kreftenheye.Google Scholar
Busschers, F.S., Kasse, C., Van Balen, R.T., Vandenberghe, J., Cohen, K.M., Weerts, H.J.T, Wallinga, J., Johns, C., Cleveringa, P. & Bunnik, F.P.M, 2007. Late Pleistocene evolution of the Rhine-Meuse system in the southern North Sea basin: imprints of climate change, sea-level oscillation and glacioisostacy. Quaternary Science Reviews 26: 3216–3248.Google Scholar
Cox, B.M. & Sumbler, M.G., 1999. Lithostratigraphy: principles and practice. In: Doyle, P. & Bennett, M.R. (eds): Unlocking stratigraphical record. Advances in modern stratigraphy. John Wiley & Sons Ltd: 11–27.Google Scholar
Dalrymple, R.W., 1994. Tidal depositional systems. In: Walker, R.G. (ed.): Facies models: response to sea level change. Geological Association of Canada: 195–218.Google Scholar
De Bruyne, R.H., De Graaf, A. & Hoeksema, D.F., 1987. Marine mollusks new for the Netherlands, washed ashore at the beaches of Ouddorp (GoereeOverflakkee, Province of Zuid-Holland), with some remarks on the occurrence of Alteneum dawsoni (Jeffreys, 1864). Basteria 51: 67–78.Google Scholar
De Mulder, E.F.J, Geluk, M.C., Ritsema, I., Westerhoff, W.E. & Wong, Th.E. (eds), 2003. De ondergrond van Nederland. Geologie van Nederland, deel 7. Nederlands Instituut voor Toegepaste Geowetenschappen TNO, 379 pp.Google Scholar
De Vos, J., Mol, D. & Reumer, J.W.F, 1995. Early Pleistocene Cervidae (Mammalia, Artiodactyla) from the Oosterschelde (the Netherlands), with a revision of the cervid genus Eucladoceros Falconer, 1868. Deinsea 2: 95–121.Google Scholar
De Vos, J., Mol, D. & Reumer, J.W.F, 1998. Early Pleistocene mammalian remains from the Oosterschelde or Eastern Scheldt (Province of Zeeland, the Netherlands). In: Van Kolfschoten, T. & Gibbard, P.L. (eds): The dawn of the Quaternary. Proceedings of the SEQS-EuroMam symposium 1996. Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO 60: 173–186.Google Scholar
Doppert, J.W.C, Ruegg, G.H.J, Van Staalduinen, C.J., Zagwijn, W.H. & Zandstra, J.G., 1975. Lithostratigrafie. 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
Du Four, L., Schelfaut, K., Vanheteren, S., Van Dijk, T. & Van Lancker, V., 2006. Geologie en sedimentologie van het Westerscheldemondingsgebied. In: Coosen, J., Mees, J., Seys, J. & Fockedey, N. (eds): Symposium: The Vlakte van de Raan van onder het stof gehaald. VLIZ Special Publication, 35 III. Vlaams Instituut voor de Zee (VLIZ) (Oostende), 135 pp.Google Scholar
Hijma, M.P., Cohen, K.M., Hoffmann, G., Van der Spek, A.J.F & Stouthamer, E., 2009. From river valley to estuary: the evolution of the Rhine mouth in the early to middle Holocene (western Netherlands, Rhine-Meuse delta). Netherlands Journal of Geosciences – Geologie en Mijnbouw 88(1): 13–53.Google Scholar
Hijma, M.P., Van der Spek, A.J.F & Van Heteren, S., 2010. Development of a midHolocene estuarine basin, Rhine-Meuse mouth area, offshore the Netherlands. Marine geology 271: 198–211.Google Scholar
Hijma, M.P. & Cohen, K.M., 2010. Timing and magnitude of the sea-level jump preluding the 8200 yr event. Geology 38: 275–278.Google Scholar
Hijma, M.P. & Cohen, K.M., 2011. Holocene transgression of the Rhine river mouth area, the Netherlands / Southern North Sea: palaeogeography and sequence stratigraphy. Sedimentology 58: 1453–1485.Google Scholar
Hijma, M.P., Cohen, K.M., Roebroeks, W., Westerhoff, W.E. & Busschers, F.S., 2012. Pleistocene Rhine-Thames landscapes: geological background for hominin occupation of the southern North Sea region. Journal of Quaternary Science 27(1): 17–39.Google Scholar
ICN/IUGS, 2009. Ratification of the definition of the base of Quaternary System/Period (and top of the Neogene System/Period), and redefinition of the base of the Pleistocene Series/Epoch (and top of the Pliocene Series/Epoch). www.stratigraphy.org.Google Scholar
Janssen, A.W., 1965. Mollusca uit de pleistocene ontsluiting te Zelzate. Mededelingen van de Werkgroep Tertiaire en Kwartaire Geologie 2: 24–37.Google Scholar
Johnson, H.D. & Baldwin, C.T., 1996. Shallow clastic seas. In: Reading, H.G. (ed.): Sedimentary environments: processes, facies and stratigraphy. Blackwell Publishing: 232–280.Google Scholar
Kiden, P., 1991. The Lateglacial and Holocene evolution of the Middle and Lower River Scheldt, Belgium. In: Starkel, L., Gregory, K.J. & Thornes, J.B., (eds): Temperate Palaeohydrology. John Wiley & Sons: 283–299.Google Scholar
Kiden, P., 2006. De evolutie van de Beneden-Schelde in België en ZuidwestNederland na de laatste ijstijd. Belgeo 2006/2003: 279–294.Google Scholar
Kiden, P., 2010. Formatie van Koewacht. In: Lithostratigrafische Nomenclator van de Ondiepe Ondergrond. Retrieved 2013 from www.dinoloket.nl/formatie-van-koewacht.Google Scholar
Mayhew, D.F. & Gibbard, P.L., 1998. Early Pleistocene small mammal remains and pollen flora from the Crag at Weybourne, Norfolk, England. In: Van Kolfschoten, T. & Gibbard, P.L. (eds): The dawn of the Quaternary. Proceedings of the SEQS-EuroMam symposium 1996. Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO 60: 263–269.Google Scholar
Mayhew, D.F. & Stuart, A.J., 1986. Stratigraphic and Taxonomic revision of the fossil vole remains (Rodentia, Microtinae) from the Lower Pleistocene deposits of Eastern England. Philosophical Transactions of The Royal Society B 312: 431–485.Google Scholar
Mayhew, D.F., De Vos, J. & Van Veen, J.C., 2008. First record of Trogontherium cuvieri (Rodentia, Castoridae) from the Oosterschelde. Deinsea 12: 17–22.Google Scholar
Meijer, T. & Cleveringa, P., 2009. Aminostratigraphy of Middle and Late Pleistocene deposits in the Netherlands and the southern part of the North Sea Basin. Global and Planetary Change 68: 326–345.Google Scholar
Nadeau, M.J., Grootes, P.M., Schleicher, M., Hasselberg, P., Rieck, A. & Bitterling, M., 1998. Sample throughput and data quality at the Leibniz-Labor AMS facility. Radiocarbon 40: 239–245.CrossRefGoogle Scholar
Pevzner, M., Tesakov, A.S. & Vangengeim, E., 1998. The position of the Tizdar locality (Taman peninsula, Russia) in the magnetochronological scale. Paludicola 2: 95–97.Google Scholar
Reading, H.G. & Collinson, J.D., 1996. Clastic coasts. In: Reading, H.G. (ed.): Sedimentary environments: processes, facies and stratigraphy. Blackwell Publishing: 154–231.Google Scholar
Reumer, J.W.F, Van Veen, J.C., Van der Meulen, A.J., Hordijk, L.W. & De Vos, J., 1998. The first find of small mammals (Desmaninae, Arvicolidae) from the Early Pleistocene Oosterschelde fauna in the Netherlands. Deinsea 4: 41–45.Google Scholar
Reumer, J.W.F, Mayhew, D.F. & Van Veen, J.C., 2005. Small mammals from the Late Pliocene Oosterschelde dredgings. Deinsea 11: 103–118.Google Scholar
Salvador, A. (ed.), 1994. International stratigraphic guide: a guide to stratigraphic classification, terminology and procedure. International subcommission on stratigraphic classification of IUGS international commission on stratigraphy. Geological Society of America (Boulder), 214 pp.Google Scholar
Schokker, J., 2003. Patterns and processes in a Pleistocene fluvio-aeolian environment. Roer Valley Graben, south-eastern Netherlands. Netherlands Geographical Studies 314, 142 pp.Google Scholar
Schokker, J., De Lang, F.D., Weerts, H.J.T, Den Otter, C. & Passchier, S., 2005. Formatie van Boxtel. In: Lithostratigrafische Nomenclator van de Ondiepe Ondergrond. Retrieved 2013 from www.dinoloket.nl/formatie-van-boxtel.Google Scholar
Schokker, J., Weerts, H.J.T, Westerhoff, W.E., Berendsen, H.J.A & Den Otter, C., 2007. Introduction of the Boxtel Formation and implications for the Quaternary lithostratigraphy of the Netherlands. Netherlands Journal of Geosciences – Geologie en Mijnbouw 86 (3): 197–210.Google Scholar
Slupik, A.A., Wesselingh, F.P., Janse, A.C. & Reumer, J.W.F, 2007. The stratigraphy of the Neogene-Quaternary succession in the southwest Netherlands from the Schelphoek borehole (42G4-11/42G0022) - a sequence-stratigraphic approach. Netherlands Journal of Geosciences - Geologie en Mijnbouw 86 (4): 317–332.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
Steurbaut, E. & Nolf, D., 1989. The stratotype of the Aalter sands (Eocene of SW Belgium): stratigraphy and calcareous nannoplankton. Mededelingen van de Werkgroep Tertiaire en Kwartaire Geologie 26 (1): 11–28.Google Scholar
Stuiver, M. & Polach, H.A., 1977. Discussion: Reporting of 14C Data. Radiocarbon 19(3): 355–363.Google Scholar
Tavernier, R., 1946. L'évolution du Bas Escaut au Pléistocène supérieur. Bulletin de la Société Belge de Géologie 65: 106–125.Google Scholar
Tavernier, R. & De Moor, G., 1974. L'évolution du Bassin de l'Escaut. In: Macar, P. (ed.): L'évolution des bassins fluviaux de la Mer du Nord méridionale. Colloque du Centenaire de la Société Géologique de Belgique, Liège: 159–231.Google Scholar
Tesakov, A.S., 1998. Voles of the Tegelen fauna. In: Van Kolfschoten, T. & Gibbard, P.L. (eds): The dawn of the Quaternary. Proceedings of the SEQS-EuroMam symposium 1996. Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO 60: 71–134.Google Scholar
Tesakov, A.S., 2004. Biostratigrafiya srednego pliotsena – eopleistotsena vostochnoi Evropy (Biostratigraphy of the Middle Pliocene-Eopleistocene of Eastern Europe). Russian Academy of Sciences, Transactions of the Geological Institute 554 Nauka (Moscow), 247 pp. (In Russian with English summary).Google Scholar
TNO, 2013. Lithostratigrafische Nomenclator van de Ondiepe Ondergrond, versie 2013. Retrieved 2013 from www.dinoloket.nl/nomenclator-ondiep.Google Scholar
Van den Berg, J.H., Boersma, J.R. & Van Gelder, A., 2007. Diagnostic sedimentary structures of the fluvial-tidal transition zone. Evidence from deposits of the Rhine and Meuse. Netherlands Journal of Geosciences – Geologie en Mijnbouw 86 (3): 287–306.Google Scholar
Van Kolfschoten, T., 1988. The Pleistocene mammalian fauna from the Zuurland borehole. In: Van Kolschoten, T. & De Boer, P.L. (eds): The Zuurland-2 borehole. Mededelingen van de Werkgroep voor Tertiaire en Kwartaire geologie / Contibutions to Tertiary and Quaternary geology 25 (1): 73–86.Google Scholar
Van Rummelen, F.F.F.E., 1965. Blad Zeeuwsch-Vlaanderen West en Oost. Toelichtingen bij de Geologische Kaart van Nederland 1: 50.000, Rijks Geologische Dienst (Haarlem), 79 pp.Google Scholar
Van Rummelen, F.F.F.E., 1970. Blad Schouwen-Duiveland. Toelichting bij de geologische kaart van Nederland 1: 50.000. Rijks Geologische Dienst (Haarlem), 116 pp.Google Scholar
Van Rummelen, F.F.F.E., 1978. Blad Beveland. Toelichting bij de geologische kaart van Nederland 1: 50.000. Rijks Geologische Dienst (Haarlem), 138 pp.Google Scholar
Van Strydonck, M. & Van der Borg, K., 1990–1991. The Construction of a preparation line for AMS-targets at the Royal Institute for Cultural Heritage Brussels. Bulletin Kon. Inst. v. h. Kunstpatrimonium 23: 228–234.Google Scholar
Van Voorthuysen, J.H., 1957. Algemeen geologisch overzicht tot een diepte van 40 m. In: De Ridder, N.A. (ed.): Agrohydrologische profielen van Zeeland. Ministerie van Landbouw, Staatsdrukkerij ('s-Gravenhage).Google Scholar
Vos, P.C., Bazelmans, J., Weerts, H.J.T & Van der Meulen, M.J. (eds.), 2011. Atlas van Nederland in het Holoceen (Amsterdam), 94 pp.Google Scholar
Weerts, H.J.T, 2003. Formatie van Naaldwijk. In: Lithostratigrafische Nomenclator van de Ondiepe Ondergrond. Retrieved 2013 from www.dinoloket.nl/formatie-van-naaldwijk.Google Scholar
Weerts, H.J.T, Cleveringa, P., Ebbing, J.H.J, De Lang, F.D. & Westerhoff, W.E., 2000. De lithostratigrafische indeling van Nederland: Formaties uit het Tertiair en Kwartair. TNO-rapport NITG 00-95-A, TNO-NITG (Utrecht).Google Scholar
Weerts, H.J.T. & Busschers, F.S., 2003. Formatie van Nieuwkoop. In: Lithostratigrafische Nomenclator van de Ondiepe Ondergrond. Retrieved 2013 from www.dinoloket.nl/formatie-van-nieuwkoop.Google Scholar
Westerhoff, W.E., Geluk, M.C. & De Mulder, E.F.J, 2003. Geschiedenis van de ondergrond. In: De Mulder, E.F.J, Geluk, M.C., Ritsema, I., Westerhoff, W.E. & Wong, T. (eds): De ondergrond van Nederland. Nederlands Instituut voor Toegepaste Geowetenschappen TNO: 119–246.Google Scholar