Search publications of the members of the Royal Belgian institute of natural Sciences
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Importance and restriction of the otolith-based fossil record of Gadiform and Ophidiiform fishes.
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Evidence from otoliths for establishing relationships within Gadiforms.
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De steenkoolverkenningsboring Gruitrode-Ophoventer-heide (Boring 172 van het Kempens Bekken) Kaartblad Opoeteren, 63E224.
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The first fossil mysid statolith (Crustacea) to be described from western Europe.
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The stratotype of the Aalter Sands (Eocene of NW Belgium) : stratigraphy and calcareous nannoplankton.
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De boringen van Ursel en Maldegem (Kaartblad Knesselare 39W nrs. 212 en 213). Bijdrage tot de kennis van het Eoceen in Noordwest-België.
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The Ypresian in its type-area : a summary.
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Stratigraphie de l' Eocène en Flandre Occidentale et dans les régions limitrophes.
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Découverte de poissons bathyaux d'âge oligocène inférieur à Pizzocorno, près de Voghera.
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Oupeye/Hermalle-sous-Argenteau: fouilles de prévention d'un champs d'urnes
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Calcareous nannoplankton assemblages from the Tertiary in the Knokke borehole.
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Der nördlichen Wiking-graben im Känozoicum. Seismiche Daten und Bohrungen dokumentierten eine wechselvolle Ablagerungs-geschichte.
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Ypresian calcareous nannoplankton biostratigraphy and palaeogeography of the Belgian Basin.
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Oupeye/Hermalle-sous-Argenteau : évaluation archéologique et étude géologique du lieu-dit "Au Buisson".
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The Paleogene of the Paris and Belgian Basins. Standard-Stages and regional stratotypes.
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Integrated stratigraphic analysis of Lower Rupelian deposits (Oligocene) in the Belgian Basin.
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Ypresian Teleost otoliths from Belgium and Northern France.
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The Ypresian Stratotype.
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Holocene palaeoecology and human environmental interactions at the coastal Black Sea Lake Durankulak, northeastern Bulgaria
- The environmental changes (vegetation history, human impact and land use, influence of the Black Sea) in the area of Lake Durankulak, northeastern Bulgaria, were reconstructed and synthesized for the last ca. 8000 years. The palaeoecological information derived from various proxies (pollen, plant macrofossils, molluscs, sediments) was compared on a regional scale with the evidence from the nearby coastal lakes ShablaeEzeretz and Bolata. The Early Holocene xerothermic steppe vegetation, dominated by Chenopodiaceae, Artemisia and Poaceae species, and accompanied by stands of trees in moister habitats, was transformed after 6000 cal. BP into a forest-steppe, comprising oak woods with Carpinus betulus, Ulmus, Tilia, Acer. This vegetation pattern has been periodically modified, depleted and replaced by arable land or xerothermic herbaceous communities enriched with anthropophytes and ruderals, particularly after the intensification of human activities since 3300 cal. BP. The archaeobotanical evidence from the region has provided valuable information about the occupation phases and subsistence strategy of the local people since the Late Neolithic (5300 cal. BC/7250 cal. BP). Periods with cultivation of cereals (Triticum, Hordeum) and/or stock-breeding activity were interrupted by abandonment of the settlements and the arable land due to unfavourable environmental changes. The periodical connection/isolation of Lake Durankulak with the Black Sea and the periods of marine influence were recorded by changes in the composition of the fossil molluscan fauna and the lithology of the sediments, and chronologically confirmed by radiocarbon dates. The development of the coastal lakes throughout the largest part of the Holocene has been also considerably influenced by the fluctuations of the Black Sea level.
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Testing models of Eemian sea level variability, using estuarine deposits from the North Sea basin
