{"refrec":{"BRefID":10707,"RR":"<b>Westerhoff, W.E.; Cleveringa, P.</b> (1990). Sea-level rise and coastal sedimentation in central Noord-Holland (The Netherlands) around 5000 BP: a case study of changes in sedimentation dynamics and sediment distribution patterns, <b><i>in</i></b>: Beukema, J.J. <i>et al.</i> (Ed.) <i>Expected effects of climatic change on marine coastal ecosystems. Developments in Hydrobiology,</i> 57: pp. 133-138","BEntID":10707,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Beukema, J.J. <i>et al.</i> <i>Expected effects of climatic change on marine coastal ecosystems. Developments in Hydrobiology,</i> 57: pp. 133-138","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Westerhoff, W.E.; Cleveringa, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Westerhoff, W.E.; Cleveringa, P.","Englishabstract":"The coastal development of the central part of the present province of Noord-Holland during the Atlantic and Subboreal led to a change in sedimentary environments, which ranged from lagoonal, via a tidal-flat-like depositional system, to a coast where prograding barriers predominated. The sedimentation pattern in the coastal plain is determined not only by rising of the sea-level but also by the pre-existing relief, the supply of sediments, and the hydrodynamic setting. 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