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Integrated chronostratigraphy of the Pliocene-Pleistocene interval and its relation to the regional stratigraphical stages in the southern North Sea region

Published online by Cambridge University Press:  01 April 2016

G. Kuhlmann ,
C.G. Langereis ,
D. Munsterman ,
R.-J. van Leeuwen ,
R. Verreussel ,
J.E. Meulenkamp  and
Th.E. Wong
G. Kuhlmann
Affiliation:
Faculty of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands TNO Built Environment and Geosciences - National Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB Utrecht, the Netherlands
C.G. Langereis*
Affiliation:
Faculty of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands
D. Munsterman
Affiliation:
TNO Built Environment and Geosciences - National Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB Utrecht, the Netherlands
R.-J. van Leeuwen
Affiliation:
TNO Built Environment and Geosciences - National Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB Utrecht, the Netherlands
R. Verreussel
Affiliation:
TNO Built Environment and Geosciences - National Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB Utrecht, the Netherlands
J.E. Meulenkamp
Affiliation:
Faculty of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands
Th.E. Wong
Affiliation:
Faculty of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands TNO Built Environment and Geosciences - National Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB Utrecht, the Netherlands
*
**Corresponding author. Email:langer@geo.uu.nl
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Abstract

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Time-stratigraphic interpretations of Late Pliocene to Early Pleistocene sediments from onshore locations and from marginal marine settings of the North Sea Basin often refer to the subdivision of the Dutch and British ’Quaternary’ regional stratigraphic stages. Since age control for these stages and their stage boundaries are based on relative dating methods, in this study pollen, dinoflagellate cysts and foraminiferal assemblages were investigated to correlate the regional stratigraphic stages independently to the global chronostratigraphy and the paleomagnetic timescale. The data were obtained from eight boreholes located in the depocentre setting of the Late Pliocene North Sea Basin comprising a 1000 m thick sedimentary succession. The British Gedgravian and Waltonian stages, the Dutch Reuverian to Brunssumian as well as published foraminiferal zones (NSB 14, FB and the lower part of the FA2 zone) fall within the Zanclean and Piacenzian. The lower boundaries of the Pre-Ludhamian and Pretiglian stages and of the NSB 14 to 15 zones are close to the paleomagnetic Gauss-Matuyama boundary. The Pre-Ludhamian, Ludhamian, Thurnian and the Pretiglian, Tiglian A and Tiglian B stages presumably cover the marine isotope stages 103 to 95. It is proposed that the Ludhamian, Thurnian and the Tiglian A were short lasting, warm, periods during which sea level highstand facilitated sedimentary deposition at the marginal areas of the North Sea Basin. The lower boundary of the paleomagnetic Olduvai subchron is situated in the Tiglian Cl-4b stage while the TC4c stage is found within the Olduvai subchron. Foraminiferal NSB 15 and NSB 16 zone as well as the upper part of the FA2 and FA1 zone fall within the Gelasian and cover the Matuyama chron as well as the lower part of the Olduvai subchron. Comparison with formerly dated North Sea sediments shows a good agreement between foraminiferal zonations on a broader scale but significant differences in absolute ages occur. Strontium isotope values indicate approximately 1 Ma younger ages as expected from our chronostratigraphic model. This discrepancy is explained by the dominance of freshwater from river discharge contributing high amounts of eroded material to the basin, leading to an increase of the 87Sr/86Sr ratio in the shelf-sea water.

Keywords

North Seadinoflagellate cystsforaminiferspollenPliocenePleistoceneregional stratigraphychronostratigraphy
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 85 , Issue 1 , March 2006 , pp. 19 - 35
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2006

References

Aguirre, E. & Pasini, G., 1985. The Pliocene - Pleistocene boundary. Episodes 8 (2): 116–120.Google Scholar
Beck, R.B, Funnell, B.M. & Lord, A.R., 1972. Correlation of the Lower Pleistocene Crag at depth in Suffolk. Geological Magazine 109: 137–139.Google Scholar
Berggren, W.A., Hilgen, F.J., Langereis, C.G., Kent, D.V., Obradovitch, J.D., Raffi, I., Raymo, M. & Shackelton, N.J., 1995a. Late Neogene chronology: New perspectives in high-resolution stratigraphy. Bulletin of the Geolical Society of America 107 (11): 1272–1287.Google Scholar
Berggren, W.A., Kent, D.V., Swisher, C.C. & Aubry, M-P., 1995b. A revised Cenozoic geochronology and chronostratigraphy. Geochronology time scales and global stratigraphic correlation, Society for Sedimentary Geology (SEPM) special publication 54: 129–212.Google Scholar
Bijlsma, S., 1981. Fluvial sedimentation from the Fennoscandian area into the Nortwest European Basin during the Late Cenozoic. Geologie en Mijnbouw 60: 337–345.Google Scholar
Boenigk, W., Koci, A. & Brunnacker, K., 1979. Magnetostratigraphie im Pliozaen der Niederrheinischen Bucht. Neues Jahrbuch fuer Geologie und Palaeontologie 9: 513–528.Google Scholar
Cameron, T.D.J., Bonny, A.P., Gregory, D.M. & Harland, R., 1984. Lower Pleistocene dinoflagellate cyst, forminiferal and pollen assemblages in four boreholes in the Southern North Sea. Geological Magazine 121 (2): 85–97.Google Scholar
Cande, S.C. & Kent, D.V., 1995. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic. Journal of Geophysical Research 100 (B4): 6093–6095.Google Scholar
De Jong, J., 1988. Climatic variability during the past three million years, as indicated by vegetational evolution in northwest Europe and with emphasis on data from the Netherlands. Philosophical Transactions of the Royal Society of London, B318: 603–617.Google Scholar
De Vernal, A., Londeix, I., Mudie, P.J., Harland, R., Morzadec-Kerfourn, M.T., Turon, J.I. & Wrenn, J.H., 1992. Quaternary organic-walled dinoflagellate cysts of the North Atlantic Ocean and adjacent seas: eco-stratigraphy and biostratigraphy. In: Head, M.J. & Wrenn, J.H. (eds): Neogene and Quaternary Dinoflagellate Cysts and Acritarchs. American Association of Stratgraphic Palynologists Foundation (Dallas): 289–328.Google Scholar
Doppert, J.W.C., 1980. Lithostratigraphy and biostratigraphy of marine Neogene deposits in the Netherlands. Mededelingen Rijks Geologische Dienst 32-16: 255–311.Google Scholar
Eidvin, T., Riis, F. & Rundberg, Y., 1999. Upper Cainozoic stratigraphy in the central North Sea (Ekofisk and Sleipner fields). Geologisk Tidsskrift 79: 97–128.Google Scholar
Farrell, J.W., Clemens, S.C. & Gromet, L.P., 1995. Improved chronostratigraphic reference curve of late Neogene seawater 87Sr/86Sr. Geology 23 (5): 403–406.2.3.CO;2>CrossRefGoogle Scholar
Funnel, B., 1996. Global sea-level and the (pen-)insularity of late Cenzoic Britain. In: Island Britain: a Qaternary perspective, Preece, R.C. (ed.), Special Publication of the Geological Society 96: 3–13.Google Scholar
Glennie, K.W., 1990. Introduction to the petroleum geology of the North Sea. Blackwell (Oxford): 402 pp.Google Scholar
Gibbard, P.L., West, R.G., Zagwijn, W.H., Balson, P.S., Burger, A.W., Funnel, B.M., Jeffery, D.H., de Jong, J., van Kolfschoten, T., Loster, A.M., Meijer, T., Norton, P.E.P., Treece, R.C., Rose, J., Stuart, A.J., Whiteman, C.A. & Zalasiewicz, J.A., 1991. Early and Early Middle Pleistocene Correlations in the southern North Sea Basin. Quaternary Science Reviews 10: 23–52.Google Scholar
Gradstein, F. & Backström, S., 1996. Cainozoic biostratigraphy and palaeo-bathymetry, northern North Sea and Haltenbanken. Norsk Geologisk Tidskrift 76: 3–32.Google Scholar
Gradstein, F.M., Ogg, J.G., & Smith, A.G. (eds), 2004. A Geologic Time Scale 2004. Cambridge University Press: 589 pp.Google Scholar
Hallam, D.F. S Maher, B.A., 1994. A record of reversed polarity carried by the iron sulphide greigite in British early Pleistocene sediments. Earth and Planetary Science Letters 121: 71–80.Google Scholar
Harland, R., 1979. Dinoflagellate biostratigraphy of Neogene and Quaternary sediments at Holes 400/400A in the Bay of Biscay (Deep Sea Drilling Project Leg 8). In: Montadert, L., Roberts, D.G. et al. (eds). Initial Reports of the Deep Sea Drilling Project, 48. U.S. Government Printing Office (Washington): 531–545.Google Scholar
Harland, R., Bonny, A.P., Hughes, M.J. & Morigi, A.H., 1991. The lower Pleistocene stratigraphy of the Ormesby Borehole, Norfolk, England. Geological Magazine 128: 647–660.Google Scholar
Harland, R., 1992. Dinoflagellate cysts of the Quaternary system. In: Powell, A.J. (ed.). A stratigraphic index of dinoflagellate cysts. Chapman and Hall (London): 253–280.Google Scholar
Head, M.J., 1994. Morphology and paleoenvironmental significance of the Cenozoic dinoflagellata genera Habibacysta and Bitectatodinium. Micropaleontology 40: 289–321.Google Scholar
Head, M.J., 1996. Late Cenozoic dinoflagellates from the Royal Society Borehole at Ludham, Norfolk, Eastern England. Journal of Paleontology 70: 543–570.CrossRefGoogle Scholar
Head, M.J., 1997. Thermophilic dinoflagellate assemblages from the mid Pliocene of eastern England. Journal of Paleontology 71: 165–193.Google Scholar
Head, M.J., 1998a. Marine environmental change in the Pliocene and early Pleistocene of eastern England: the dinoflagellate evidence reviewed. Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO 60: 199–225.Google Scholar
Head, M.J., 1998b. Pollen and dinoflagellates from the Red Crag at Walton-on-the-Naze, Essex: evidence for a mild climatic phase during the early Late Pliocene of eastern England. Geological Magazine 135: 803–817.Google Scholar
Huuse, M., 2002. Late Cenozoic palaeogeography of the estern North Sea Basin: climate vs. tectonic forcing of basin margin uplift and deltaic progradation. Bulletin of the Geological Society of Denmark 49: 145–170.Google Scholar
Kasse, C., 1996. Paleomagnetic dating and effects of Weichselian periglacial processes on the magnetization of early Pleistocene deposits (southern Netherlands, northern Belgium). Geologie en Mijnbouw 75: 19–31.Google Scholar
King, C., 1983. Cainozoic micropalaeontological biostratigraphy of the North Sea. Report Institute Geological Sciences 82: 1–40: 6 pl.Google Scholar
King, C., 1989. Cenozoic of the North Sea. In: Jenkins, D.G. & Murray, J.W. (eds) Stratigraphical atlas of fossil Foraminifera. Chichester, Ellis Horwood: 418–489.Google Scholar
Konradi, P.B., 1996. Foraminiferal biostratigraphy of the post-mid Miocene in the Danish Central Trough, North Sea. In: De Batist, M.P.J., (ed), Geology of siliclastic shelf seas. Geol. Soc. Spec. Publ. 117: 15–22.Google Scholar
Kuhlmann, G., 2004. High resolution stratigraphy and paleoenvironmental changes in the southern North Sea during the Neogene - An integrated study of Late Cenozoic marine deposits from the northern part of the Dutch offshore area. Ph.D. thesis, Utrecht University, Geologica Ultraiectina, Mededelingen van de Faculteit Aardwetenschappen 245: 205 pp.Google Scholar
Laursen, G.V., 1995. Foraminiferal analyses of Tertiary deposits in the North Sea area: Stratigraphy, palaeoecology and taxonomy. Ph.D. thesis, University of Aarhus: 267 pp.Google Scholar
Lourens, L.J., Hilgen, F.J., Zachariasse, W.J., Van Hoof, A.A.M., Antonarakou, A. & Vergnaud-Grazzini, C., 1996. Evaluation of the Pliocene to early Pleistocene astronomical time scale, Paleoceanography 11: 391–413.Google Scholar
Matthiessen, J. & Brenner, W., 1996. Dinoflagellate cyst ecostratigraphy of Pliocene-Pleistocen sediments from the Yermak Plateau (Arctic Ocean, Hole 911A). In: Thiede, H., Myhre, A.M., Firth, J.V., Johnson, G.L. & Ruddiman, W.F. (eds): Proceedings of the Ocean Drilling Program, Scientific Results 151: College Station, TX (Ocean Drilling Program): 243–253.Google Scholar
Mauz, B., 1998. The onset of the Quaternary: A review of new findings in the Pliocene-Pleistocene chronostratigraphy. Quaternary Science Reviews 17 (4-5): 357–364.Google Scholar
McArthur, J.M., Howarth, R.J. & Bailey, T.R., 2001. Strontium Isotope Stratigraphy: LOWESS Version 3: Best Fit to the Marine Sr-Isotope Curve for 0 - 509 Ma and Accompanying Look-up Table for Deriving Numerical Age. The Journal of Geology 109: 155–170.Google Scholar
Mudie, P.J., 1989. Palynology and dinocyst biostratigraphy of the late Miocene to Pleistocene, Norwegian Sea ODP Leg 104, Sites 642 to 644. In: Eldholm, O., Thiede, J., Tayler, E., et al. (eds): Proceedings of the Ocean Drilling Program, College Station, Texas: 568 pp.Google Scholar
Oakley, K.P., 1949. The Plio-Pleistocene boundary. Proceedings of the International Geological Congress, 18th session, 1948: Section H. Geological Magazine 86: 18–21.Google Scholar
Palmer, M.R. & Edmond, J.M., 1989. The strontium isotope budget of the modern ocean. Earth and Planetary Science Letters 92: 11–26.Google Scholar
Poulsen, N.E., Manum, S.B., Williams, G.L. & Ellegaard, M., 1996. Tertiary dinoflagellate biostratigraphy of Sites 907, 908 and 909 in Norwegian-Greenland Sea. In: Thiede, J., Myhre, A.M., Firth, J.V., Johnson, G.L. & Ruddiman, W.F. (eds): Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program): 255–287.Google Scholar
Smelror, M., 1999. Plio-Pleistocene and redeposited dinoflagellate cysts from the western Svalbard margin (Site 986): biostratigraphy, paleoenvironment and sediment provenance. In: Raymo, M.E., Jansen, E., Blum, P. & Herbert, T.D. (eds): Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program): 83–97.Google Scholar
Sørensen, J.C., Gregersen, U., Breiner, M. & Michelsen, O., 1997. High-frequency sequence stratigraphy of Upper Cenozoic deposits in the central and southeastern North Sea areas. Marine and Petroleum Geology 14 (2): 99–123.Google Scholar
Urban, B., 1978. The interglacial of Frechen/Rheinland - a section of the Tiglian A-type. Geologie en Mijnbouw 57: 401–406.Google Scholar
Van Adrichem Boogaert, H.A. & Kouwe, W.F.P. (eds), 1997. Stratigraphic nomenclature of the Netherlands, revision and update by RGD and N0GEPA, Section Tertiary (Lower, Middle and Upper North Sea Groups). Mededelingen Rijks Geologische Dienst 50 (I): 1–39, 6 annexes.Google Scholar
Van den Berg, M.W. & Van Hoof, A.A.M., 2001. The Maas terrace sequence at Maastricht, SE Netherlands: evidence for 200 m of late Neogene and Quaternary surface uplift. In: Maddy, D., Macklin, M.G. & Woodward, J.C. (eds): River Basin Sediment Systems: Archives of Environmental Change. A.A. Balkema Publishers (Lisse): 45–86.Google Scholar
Van der Vlerk, I.M. & Florschütz, F., 1950. Nederland in het ijstijdvak. Utrecht: 287 pp.Google Scholar
Van Montfrans, H.M., 1971. Paleomagnetic dating in the North Sea Basin. Earth and Planetary Science Letters 11: 226–235.Google Scholar
Van Voorthuysen, J.H., Toering, K. & Zagwijn, W.H., 1972. The Plio-Pleistocene boundary in the North Sea Basin; revision of its position in the marine beds. Geologie en Mijnbouw 51 (6): 627–639.Google Scholar
Versteegh, G.J.M., 1995. Paleoenvironmental changes in the Mediterranean and North Atlantic in relation to the onset of Northern Hemisphere glaciations - a palynological approach. Published thesis, University of Utrecht, Ponsen en Looijen (Wageningen): 134 pp.Google Scholar
Versteegh, G.J.M., 1997. The onset of major Northern Hemisphere glaciations and their impact on dinoflagellate cysts and acritarchs from the Singa section, Calabria (southern Italy) and DSDP Holes 607/607A (North Atlantic). Marine Micropaleontology 30: 319–343.Google Scholar
Vinken, R., 1988. The North West European Tertiary Basins. Results of the International Geological Correlation Programme, Project No. 124, Geologisches Jahrbuch 100: 508 pp.Google Scholar
Weaver, P.P.E. & Clement, B.M., 1986. Synchronicity of Pliocene planktonic foraminiferal datums in the North Atlantic. Marine Micropalaeontology 10: 295–307.Google Scholar
Weaver, P.P.E., 1987. Magnetobiostratigraphy of planktonic foraminiferal datums, DSDP Leg 94, North Atlantic. In: Ruddiman, W.F., Kidd, R.B., Thomas, E., et al., Initial Reports of the DSDP, 94: Washington, 815–829.Google Scholar
West, R.G., 1961. Vegetational history of the Early Pleistocene of the Royal Society Borehole at ludham, Norfolk. Proceedings of the Royal Society of London, B155: 437–453.Google Scholar
Westerhoff, W.E., Cleveringa, P., Meijer, T., van Kolfschoten, T. & Zagwijn, W.H., 1998. The Lower Pleistocene fluvial (clay) deposits in the Maalbeek pit near Tegelen, the Netherlands. In: Van Kolfschoten, T. & Gibbard, P.L. (eds): The Dawn of the Quaternary, Proceedings of the SEQS-EuroMam symposium., Mededelingen NITG-TNO 60: 35–69.Google Scholar
Zagwijn, W.H., 1957. Vegetation, climate and time-correlations in the Early Pleistocene of Europe. Geologie en Mijnbouw 19: 233–244.Google Scholar
Zagwijn, W.H., 1960. Aspects of the Pliocene and Early Pleistocene vegetation of the Netherlands. Mededelingen Geologische Stichting C III-I, 5: 78 pp.Google Scholar
Zagwijn, W.H., 1963. Pollen-analytic investigations in the Tiglian of the Netherlands. Mededelingen Geologische Stichting 16: 49–72.Google Scholar
Zagwijn, W.H., 1974. The paleogeographic evolution of the Netherland during the Quarternary. Geologie en Mijnbouw 53 (6): 369–385.Google Scholar
Zagwijn, W.H., 1985. An outline of the Quaternary stratigraphy of the Netherlands. Geologie en Mijnbouw 64: 17–24.Google Scholar
Zagwijn, W.H., 1992. The beginning of the Ice Age in Europe and its major subdivisions. Quaternary Science Reviews 11 : 583–591.Google Scholar
Zagwijn, W.H., 1998. Borders and boundaries; a century of stratigraphical research in the Tegelen-Reuver area of Limburg (the Netherlands). In: The dawn of the Quaternary; proceedings of the SEQS-EuroMam symposium 1996: Van Kolfschoten, Th. & Gibbard, P.L. (eds): Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO 60: 19–34.Google Scholar
Zagwijn, W.H. & Doppert, J.W.C., 1978. Upper Cenozoic of the southern North Sea Basin: Palaeoclimatic and Palaeogeographic evolution. Geologie en Mijnbouw 57 (4): 577–588.Google Scholar
Zalasiewicz, J.A., Mathers, S.J., Gibbard, P.L. Peglar, S.M, Funnell, B.M., Catt, J.A., Harland, R., Long, P.E. & Austin, T.J.F., 1991. Age and relationship of the Chillesford Clay (early Pleistocene: Suffolk, England). Philosphical Transactions of the Royal Society of London 333: 81–100.Google Scholar
Ziegler, P., 1990. Geological atlas of Western and Central Europe. 3rd edition, Shell International Petroleum Maatschappij B.V.: 239 ppGoogle Scholar