{"refrec":{"BRefID":64310,"RR":"<b>Wartel, S.; de Meuter, F.; Ringele, A.</b> (1983). Note concerning the origin of Scheldt estuary bottom sediments (Belgium, The Netherlands). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 55(1)</i>: 15 pp.","BEntID":60799,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 55(1)</i>: 15 pp.","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":1,"BrackishFlag":1,"TerrestrialFlag":0,"Authorstring":"Wartel, S.; de Meuter, F.; Ringele, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wartel, S. <i>et al.</i>","Englishabstract":"The analyses of gravels, shells and foraminifera of bottom sediments in the Scheldt estuary reveal a correlation between these sediments and the substratum. This is particularly so for the foraminifera assemblages. The results indicate on the one hand an erosion of Tertiary and Quaternary deposits and, on the other hand, a prevailing downstream sediment transport between the river Rupel and Antwerp and an up- as a downstream sediment transport as well in the river Western-Scheldt.","AbstractOtherLang":"L'analyse des graviers, mollusques et foraminifères des sédiments du fond de l'estuaire de l'Escaut montre une correlation entre les sédiments récents et le substratum. Ceci est particulièrement le cas pour les foraminifères. Les résultats indiquent d'une part une érosion des dépôts Tertiaires et Quaternaires. 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