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   <subfield code="a">Geochemical compositional changes at the Pliocene-Pleistocene transition in fluviodeltaic deposits in the Tegelen-Reuver area (southeastern Netherlands)</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[D. J. Huisman, G. T. Klaver, A. Veldkamp, B. J. H. van Os]</subfield>
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   <subfield code="a">2: O contents, which can be attributed to the Alpine source supplying fresh, sodic plagioclase-rich material instead of the local, strongly weathered sediments. Increasing K2O/Al2O3 can be attributed to a similar decrease in degree of weathering. However, this trend is disturbed by the loss of K from clay minerals during weathering in organic-rich layers. Local high TiO2 anomalies, caused by preferential sorting and concentration, are found in most Pliocene sections, but they are absent in the Upper Pliocene and Lower Pleistocene Alpine-derived deposits. This change is probably due to a change in the energy of the fluvial system. Finally, (pyrite-) S contents drop (siderite-) Fe contents rise. Micromorphological observations indicate that the Pliocene pyrite was formed when freshwater deposits were flooded with seawater during short-term events. The decrease in S, and the increase in siderite-Fe, can be attributed to decreasing marine influence, as a result of the marine regression at the Pliocene-Pleistocene transition.</subfield>
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   <subfield code="u">Wageningen Agricultural University, Laboratory for Soil Science and Geology, P.O. Box 37, NL-6700 AA Wageningen, The Netherlands Tel.: +31-30-2534162 Fax: +31-23-2535121 e-mail: h.huisman@nitg.tno.nl, NL</subfield>
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