Hostname: page-component-78c5997874-m6dg7 Total loading time: 0 Render date: 2024-11-19T16:26:54.620Z Has data issue: false hasContentIssue false

Reply to the comment by M.P. Hijma & K.M. Cohen on the paper by Van de Plassche et al. (2010)

Published online by Cambridge University Press:  24 March 2014

B. Makaske
Affiliation:
Alterra, Wageningen Universityand Research Centre, P.O. Box 47, 6700 AA Wageningen, the Netherlands. Email: [email protected]
W.Z. Hoek
Affiliation:
Department of Physical Geography, Faculty of Geosciences, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, the Netherlands
Rights & Permissions [Opens in a new window]

Extract

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.

First of all, we want to stress that this reply to the comment by Hijma & Cohen on the paper by Van de Plassche et al. (2010) reflects our personal view and not necessarily the opinion of the first author of the paper under discussion, Orson van de Plassche. After a long career dedicated to sea-level research, Orson passed away on May 4, 2009, and left us with the Vlaardingen data set and his explicit wish to publish this material, which ultimately led to the Van de Plassche et al. (2010) paper. In the present paper we will: (1) give some background information on the Vlaardingen data set and the special circumstances under which the Van de Plassche et al. (2010) paper was written; (2) reply to the comment on the construction of our revised mean sea-level curve (MSL-R2); (3) reply to the comment on our suggestion that the palaeoriver-gradient might influence sea-level jump magnitude calculations.

The paper by Van de Plassche et al. (2010) is primarily based on the Vlaardingen data set that was collected by Orson van de Plassche in the mid-1980s, in a sequel to his PhD project (Van de Plassche, 1982). Soon after the start of the Vlaardingen project Orson became busily occupied with sea-level research in North America, leaving the Vlaardingen data set virtually unpublished (some data were published in Van de Plassche (1995)).

Type
Correspondence
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2011

References

Berendsen, H.J.A., Makaske, B., Van de Plassche, O., Van Ree, M.H.M., Das, S., Van Dongen, M., Ploumen, S. & Schoenmakers, W., 2007. New groundwater-level rise data from the Rhine-Meuse delta; implications for the reconstruction of Holocene relative mean sea-level rise and differential land-level movements. Netherlands Journal of Geosciences – Geologie en Mijnbouw 86: 333354.Google Scholar
Hijma, M.P. & Cohen, K.M., 2010. Timing and magnitude of the sea-level jump preluding the 8200 yr event. Geology 38: 275278.Google Scholar
Van de Plassche, O., 1982. Sea-level change and water-level movements in the Netherlands during the Holocene. Mededelingen Rijks Geologische Dienst 36: 193.Google Scholar
Van de Plassche, O., 1995. Periodic clay deposition in a fringing peat swamp in the lower Rhine-Meuse river area, 5400-3400 cal BC. In: Finkl Jnr, C.W. (ed.): Holocene cycles: climate, sea levels and sedimentation. Journal of Coastal Research Special Issue 17: 95102.Google Scholar
Van de Plassche, O., Makaske, B., Hoek, W.Z., Konert, M. & Van der Plicht, J., 2010. Mid-Holocene water-level changes in the lower Rhine-Meuse delta (western Netherlands): implications for the reconstruction of relative mean sea-level rise, palaeoriver-gradients and coastal evolution. Netherlands Journal of Geosciences – Geologie en Mijnbouw 89: 320.Google Scholar
Van der Molen, J. & De Swart, H.E., 2001. Holocene tidal conditions and tide-induced sand transport in the southern North Sea. Journal of Geophysical Research 106 (C5): 93399362.Google Scholar
Van Dijk, G.J., Berendsen, H.J.A. & Roeleveld, W., 1991. Holocene water-level development in the Netherlands' river area; implications for sea-level reconstruction. Geologie en Mijnbouw 70: 311326.Google Scholar