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Tributaries of the Elbe Palaeovalley: Features of a Hidden Palaeolandscape in the German Bight, North Sea

  • Daniel A. HeppEmail author
  • Ursula Warnke
  • Dierk Hebbeln
  • Tobias Mörz
Chapter
Part of the Coastal Research Library book series (COASTALRL, volume 20)

Abstract

Prior to postglacial global sea-level rise in the present North Sea area, Mesolithic hunters and gatherers were able to settle in the coastal lowland landscape between England, Germany and Denmark, commonly known as Doggerland. Regarding the reconstruction of this now drowned palaeolandscape, the German exclusive economic zone (EEZ) sector is still ‘terra incognita’. Recent discoveries of two ancient fluvial systems, both of which were tributaries of the Elbe Palaeovalley, give new insights into the formation of the Mesolithic Doggerland landscape in the German EEZ. One of these fluvial systems developed during the last glaciation and connected the Dogger Hills with the Elbe Palaeovalley. The second river structure discovered in the south seems to be slightly younger and can be identified as the drowned extension of the modern Ems River.

Keywords

Doggerland Drowned Rivers Elbe Palaeovalley Tributaries 

Notes

Acknowledgments

We gratefully acknowledge Sebastian Feldmann, Lukasz Socko, Mike Belasus and Vanessa Wahlers for their excellent technical and scientific operation on board LEV Taifun and for assistance with the data processing onshore. We thank Mark Coughlan for his suggested improvements to the text, and Henk Weerts and Dimitris Sakellariou for constructive reviews that improved our manuscript. This study was funded through DFG-Research Center/Cluster of Excellence ‘MARUM – The Ocean in the Earth System’ in cooperation with the project ‘Bedrohtes Bodenarchiv Nordsee’ funded by the Federal Ministry of Education and Research (Germany). The study was further supported with data from several anonymous industry partners.

References

  1. Berendsen HJA, Stouthamer E (2000) Late Weichselian and Holocene palaeogeography of the Rhine-Meuse delta, the Netherlands. Palaeogeogr Palaeoclimatol Palaeoecol 161:311–335CrossRefGoogle Scholar
  2. Cohen KM, Gibbard PL, Weerts HJT (2014) North Sea palaeogeographical reconstructions for the last 1 Ma. Neth J Geosci 93:7–29Google Scholar
  3. Coles BJ (1998) Doggerland: a speculative survey. Proc Prehist Soc 64:45–81CrossRefGoogle Scholar
  4. Coles BJ (2000) Doggerland: the cultural dynamics of a shifting coastline. In: Pye K, Allen SRL (eds) Coastal and estuarine environments: sedimentology, geomorphology and geoarchaeology, vol 175. Geological Society of London, Special Publication, London, pp 393–401Google Scholar
  5. Figge K (1980) Das Elbe-Urstromtal im Bereich der Deutschen Bucht (Nordsee). Eiszeit Gegenw 30:203–211Google Scholar
  6. Fitch S, Gaffney VL, Ramsey E, Kitchen E (2011) West coast palaeolandscapes survey, final report. Visual and Spatial Technology Centre and University of Birmingham, BirminghamGoogle Scholar
  7. Fitch S, Thomson K, Gaffney V (2005) Late Pleistocene and Holocene depositional systems and the paleogeography of the Dogger Bank, North Sea. Quat Res 64:185–196CrossRefGoogle Scholar
  8. Gaffney VL, Fitch S, Smith D (2009) Europe’s lost world: the rediscovery of Doggerland. CBA research report 160. Council for British Archaeology, YorkGoogle Scholar
  9. Gaffney VL, Thomson K, Fitch S (eds) (2007) Mapping Doggerland: the Mesolithic landscapes of the southern North Sea. Archaeopress, OxfordGoogle Scholar
  10. Hijma MP (2009) From river valley to estuary: the early-mid Holocene transgression of the Rhine-Meuse valley, The Netherlands. PhD thesis, University of UtrechtGoogle Scholar
  11. Kiden P (1989) The late Holocene evolution of the perimarine part of the river Scheldt. In: Henriet JP, De Moor G, De Batist M (eds) The quaternary and tertiary geology of the southern bight North Sea. Belgian Geological Survey, Brussels, pp 173–184Google Scholar
  12. Kiden P (1991) The late glacial and Holocene evolution of the middle and lower river Scheldt, Belgium. In: Starkel L, Gregory KJ, Thornes JB (eds) Temperate palaeohydrology: fluvial processes in the temperate zone during the last 15000 years. Wiley, Chichester, pp 283–299Google Scholar
  13. Leopold LB, Wolman MG, Miller JP (1964, reprinted 1995) Fluvial processes in geomorphology. Dover Publication, New YorkGoogle Scholar
  14. Spinney L (2008) The lost world. Nature 454:151–153CrossRefGoogle Scholar
  15. Törnqvist TE (1993) Holocene alternation of meandering and anastomosing fluvial systems in the Rhine-Meuse Delta (Central Netherlands) controlled by sea-level rise and subsoil erodibility. J Sediment Res 63:683–693Google Scholar
  16. Van Heteren S, Meekes JAC, Bakker MAJ, Gaffney V, Fitch S, Gearey BR, Paap BF (2014) Reconstructing North Sea palaeolandscapes from 3D and high-density 2D seismic data: an overview. Neth J Geosci 93:31–42Google Scholar
  17. Vink A, Steffen H, Reinhardt L, Kaufmann G (2007) Holocene relative sea-level change, isostatic subsidence and the radial viscosity structure of the mantle of Northwest Europe (Belgium, the Netherlands, Germany, southern North Sea). Quat Sci Rev 26:3249–3275CrossRefGoogle Scholar
  18. Ward I, Larcombe P, Firth A, Manders M (2014) Practical approaches to management of the marine prehistoric environment. Neth J Geosci:1–12Google Scholar
  19. Zeiler M, Schulz-Ohlberg J, Figge K (2000) Mobile sand deposits and shoreface sediment dynamics in the inner German bight (North Sea). Mar Geol 170:363–380CrossRefGoogle Scholar

Copyright information

© Springer International Publishing AG 2017

Authors and Affiliations

  • Daniel A. Hepp
    • 1
    Email author
  • Ursula Warnke
    • 2
  • Dierk Hebbeln
    • 1
  • Tobias Mörz
    • 1
  1. 1.MARUM – Center for Marine Environmental SciencesUniversity of BremenBremenGermany
  2. 2.German Maritime Museum – Institute of the Leibniz-Association (Deutsches Schiffahrtsmuseum – Institut der Leibniz-Gemeinschaft)BremerhavenGermany

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