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1. Introduction In the course of the last two centuries, the subsurface of the Antwerp area has received a lot of attention from geologists and paleontologists who were attracted by the large number of glauconiferous marine sediments yielding incredibly high numbers of well-preserved fossils that could be documented, sampled and studied whenever construction works reached into its shallowly buried Neogene deposits. Unfortunately, construction works are always temporary in nature, thus creating major pitfalls for the research on these deposits. In far too many cases, important outcrops remained undocumented or were only observed by a too limited number of researchers, hampering the advance of the understanding of the stratigraphy, sedimentology and paleontology of the Antwerp area Neogene. Although the Miocene and Pliocene geology of the Antwerp area is relatively well documented, insights in the upper Miocene Deurne Member of the Diest Formation have largely been hampered by the low number of temporary outcrops reported in the literature, in particular since Glibert & de Heinzelin de Braucourt (1955a, 1955b) summarized a century of observations on their ‘Sables de Deurne’. The current insights in the stratigraphy of the Antwerp area Neogene root for large parts in the works of four students of the KU Leuven Geology Lab in the late 60s and early 70s of the 20th century: Frans De Meuter, Piet Laga, Adolf Ringele and Karel Wouters. The stratigraphic framework published by De Me

geologica belgica (printed)/geologica belgica (online)

The upper Miocene Deurne Member of the Diest Formation revisited: unexpected results from the study of a large temporary outcrop near Antwerp International Airport, Belgium