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Meijer, T. (author), Pouwer, R. (author), Cleveringa, P. (author), de Wolf, H. (author), Busschers, F.S. (author), Wesselingh, F.P. (author)When dealing with stratigraphic successions in marginal basin settings, the geological record is often fragmented due to erosion and reworking processes. The North Sea Basin is an example: it has a fragmented Quaternary record; in particular, Middle Pleistocene intervals are poorly known. As a result, we have little insight into climate, marine...article 2021
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- Westerhoff, W.E. (author), Donders, T.H. (author), trabucho Alexandre, N. (author), Busschers, F.S. (author) article 2020
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van den Biggelaar, D.F.A.M. (author), Kluiving, S.J. (author), Bohncke, S.J.P. (author), van Balen, R.T. (author), Kasse, C. (author), Prins, M.A. (author), Kolen, J. (author)This paper presents a new perspective for the temporal variation of crop cultivation adoption during the period 6000-5400BP in Flevoland (central Netherlands) based on the spatial evolution of soils and hydrology. To determine the role of soil properties and groundwater level rise in the adoption of crop cultivation in wetlands, mapping of the...article 2015
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Slupik, A.A. (author), Wesselingh, F.P. (author), Mayhew, D.F. (author), Janse, A.C. (author), Dieleman, F.E. (author), van Strydonck, M. (author), Kiden, P. (author), Burger, A.W. (author), Reumer, J.W.F. (author)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...article 2013
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Deeben, J. (author), Hiddink, H. (author), Huisman, D.J. (author), Müller, A. (author), Schokker, J. (author), Wallinga, J. (author), TNO Bouw en Ondergrond (author)The original distribution pattern of Middle-Palaeolithic artefacts may be affected by tectonic movement, sedimentation and periglacial processes. This is e.g. the case in the coversand area of Limburg and Eastern Brabant (NL), where the occurrence of numerous finds in a SW-NE trending zone across the Roer Valley Graben is considered enigmatic....article 2010
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Berg, S. (author), Wagner, B. (author), Cremer, H. (author), Leng, M.J. (author), Melles, M. (author), TNO Bouw en Ondergrond (author)The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrounding shallow marine areas provide valuable archives for the reconstruction of the late Pleistocene and Holocene environmental and climatic history of the region. Two sediment records from two marine inlets of Rauer Group have been studied for...article 2010
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Eisma, D. (author), Mook, W.G. (author), Laban, C. (author)Salinity, temperature and age have been determined for Cardium edule shells, collected in the Southern Bight of the North Sea, from their isotopic composition. The results indicate that before c.8100 BP(probably between.10,000 and 8000 BP) a brackish-water tidal-flat area existed in the present Deep Water Channel (chlorinity c.13). Between c...bookPart 2009
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- TNO Bouw en Ondergrond (author), Berg, S. (author), Wagner, B. (author), White, D.A. (author), Cremer, H. (author), Bennike, O. (author), Melles, M. (author) article 2009
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Westerhoff, W.E. (author), Kemna, H.A. (author), Boenigk, W. (author), TNO Bouw en Ondergrond (author)The fluvial history of the northern Lower Rhine Embayment shows interplay of three main river systems: Rhine, Meuse and smaller rivers draining the central and northern part of Belgium. The Pliocene and Early Pleistocene (pre-)Rhine and Meuse river systems had their conjunction in the southern part of the Roer Valley Graben between Aachen and...article 2008
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Busschers, F.S. (author), Kasse, C. (author), van Balen, R.T. (author), van den Berghe, J. (author), Cohen, K.M. (author), Weerts, H.J.T. (author), Wallinga, J. (author), Johns, C. (author), Cleveringa, P. (author), Bunnik, F.P.M. (author), TNO Bouw en Ondergrond (author)High-resolution continuous core material, geophysical measurements, and hundreds of archived core descriptions enabled to identify 13 Late Pleistocene Rhine-Meuse sedimentary units in the infill of the southern part of the North Sea basin (the Netherlands, northwestern Europe). This sediment record and a large set of Optical Stimulated...article 2007
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Kemna, H.A. (author), Westerhoff, W.E. (author), TNO Bouw en Ondergrond (author)The chronostratigraphical subdivision of the Pliocene and Early Pleistocene as applied in terrestrial deposits of Central and NW-Europe largely relies on the pollen analytical investigations. This subdivision is almost entirely based on the interpretation of quantitative changes of the vegetational cover as recorded by the pollen content of...article 2007
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Meijer, T. (author), Cleveringa, P. (author), Munsterman, D.K. (author), Verreussel, R.M.C.H. (author), TNO Bouw en Ondergrond (author)In this paper, the currently accepted correlation of the Early Pleistocene Ludhamian stage of England with the Tiglian-A sub-stage of the Netherlands is challenged. Recent investigations of Early Pleistocene marine North Sea deposits from a borehole near Noordwijk (the Netherlands) yielded evidence from molluscs, dinoflagellate cysts and...article 2006
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TNO Bouw en Ondergrond (author), Kuhlmann, G. (author), Langereis, C.G. (author), Munsterman, D. (author), van Leeuwen, R.J. (author), Verreussel, R. (author), Meulenkamp, J.E. (author), Wong, Th.E. (author)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...article 2006
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TNO Bouw en Ondergrond (author), Busschers, F.S. (author), Weerts, H.J.T. (author), Wallinga, J. (author), Cleveringa, P. (author), Kasse, C. (author), Wolf, H.de (author), Cohen, K.M. (author)Eight continuous corings in the west-central Netherlands show a 15 to 25 m thick stacked sequence of sandy to gravelly channel-belt deposits of the Rhine-Meuse system. This succession of fluvial sediments was deposited under net subsiding conditions in the southern part of the North Sea Basin and documents the response of the Rhine-Meuse river...article 2005
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Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author), Jansen, H.S.M. (author), Huizer, J. (author), Dijkmans, J.W.A. (author), Mesdag, C. (author), van Hinte, J.E. (author)The geometry and depositional history of the Maassluis Formation is described from an East-West oriented transect located in the west-central Netherlands and P- and Q-blocks in the Dutch offshore area. The Late Pliocene to Early Pleistocene Maassluis Formation was deposited under near coastal marine conditions. Two distinct facies are...article 2004
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Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author), Jansen, H.S.M. (author), Huizer, J. (author), Dijkmans, J.W.A. (author), van Hinte, J.E. (author)87Sr/86Sr (Strontium) ratio analyses of shell material (mainly Arctica islandica) from 24 levels in the Maassluis Formation of boreholes Noordwijk, Zegveld and Terschelling suggest that the age of the formation ranges from 0.82 to 2.34 Ma (± 0.5 Ma), and that the Oosterhout Formation at Noordwijk could be as much as 2.5 Ma older than hitherto...article 2004
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Winthaegen, P.L.A. (author), Verweij, J.M. (author), Netherlands Institute of Applied Geoscience TNO, National Geological Survey, P.O. Box 80015, 3508 TA Utrecht, Netherlands (author)The application of the empirical Eaton method to calibrated sonic well information and 3D seismic interval velocity data in the southeastern part of the Central North Sea Graben, using the Japsen (Glob. Planet. Change 24 (2000) 189) normal velocitydepth trend, resulted in the identification of an undercompacted and overpressured zone within the...article 2003
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Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author), Gans, W.de (author), Beets, D.J. (author), Centineo, M.C. (author)During its maximum extension, the Saalian ice cap reached into the central Netherlands, where glacier tongues excavated over 100 m deep basins in the unconsolidated Middle and Early Pleistocene sediments. The basins are filled by relatively thick successions of Late Saalian, Eemian and Weichselian sediments. The fill of the Amsterdam glacial...article 2000
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Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author), Bosch, J.H.A. (author), Cleveringa, P. (author), Meijer, T. (author)A historical outline of the Eemian research in the Netherlands is presented as an introduction to recent research in the type area. At the end of the 19th and during the first part of the 20th century, Eemian sediments were recognized because of the presence of lusitanian and mediterranean mollusc species. From 1930 onwards, pollen analysis made...article 2000
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Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author), van Leeuwen, R.J.W. (author), Beets, D.J. (author), Bosch, J.H.A. (author), Burger, A.W. (author), Cleveringa, P. (author), van Harten, D. (author), Herngreen, G.F.W. (author), Kruk, R.W. (author), Langereis, C.G. (author), Meijer, T. (author), Pouwer, R. (author), de Wolf, H. (author)The Amsterdam glacial basin was a major sedimentary sink from late Saalian until late Eemian (Picea zone, E6) times. The basin's exemplary record makes it a potential reference area for the last interglacial stage. The cored Amsterdam-Terminal borehole was drilled in 1997 to provide a record throughout the Eemian interglacial. Integrated facies...article 2000
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