The environmental and climatic conditions of the Late Pleistocene of Southern Belgium are here determined for the final part of Marine Isotope Stage 3 (MIS 3) and for MIS 2 on the basis of a study of rodent assemblages. This paper provides a synthesis of several sets of environmental and climatic data from Late Pleistocene sites, all of which are located in southern Belgium. One has previously been published (Caverne Marie-Jeanne), and seven are unpublished (Cavernes de Goyet, Trou des Nutons, Trou du Frontal, Trou de Chaleux, Grotte la Chefalize, Trou du Chˆene, and Trou du Sureau). The habitat weighting and quantified ecology methods are applied to rodent material housed in the Royal Belgian Institute of Natural Sciences (RBINS, Brussels), and previous radiocarbon dates are updated, in order to reconstruct past environments. Among all the sites under analysis, the quantified ecology method shows that Trou de Chaleux corresponds to the coldest temperatures and lowest precipitation. Trou de Chaleux, with a chronology between ca. 15,964–14,014 cal yr B.P., could probably be placed in Greenland Stadial 2 (GS2) or Heinrich Event 1 (HE1). It has a rodent assemblage associated with a predominance of open dry and rocky formations, the most abundant species being the collared lemming and the narrow-headed vole. These data are found to coincide with previous studies carried out on the large-mammal, herpetofaunal, and avifaunal associations of the site, as well as on small-mammal associations from other sites in southern Belgium with similar chronology, such as Grotte Walou. Taken together, this indicates that these latest Pleistocene intervals in southern Belgium were characterized by harsh climatic and environmental conditions. In contrast, the other assemblages under study yielded much more heterogeneous results, frequently inconsistent with an attribution to the Pleistocene. This is likely to be a result of their admixture with Holocene material due to recent intrusions.
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RBINS Staff Publications 2023
In this contribution, we describe a tooth of Otodus obliquus Agassiz, 1843, found in sand supplementation material on the beach of Dishoek, Walcheren (The Netherlands). Even though this species has a broad distribution in Paleocene and early Eocene successions in Western Europe, in the Netherlands it was thus far only known to occur reworked in younger strata in the subsurface of the northern part of the country, and has never been described from sand supplementation material. The described specimen was found in material dredged up from the Middeldiep, a trough in the Zeeuwse Banken area. The associated mollusk fauna suggests that the material is derived from the mid-Pleistocene to early Holocene Kreftenheye Formation, in which the described early Eocene tooth likely occurred as reworked. Potentially, it was originally derived from the early Eocene Tielt Formation, outcropping to the south of Brugge, Belgium, and transported by local rivers to the Zeeuwse Banken area during the Pleistocene. Alternatively, flint and chalk material present in the sand supplementation material suggests that the described specimen could also be originated across the North Sea, derived from the early Eocene Harwich and London Clay deposits exposed in Kent and Essex (England) and transported eastwards by the paleo-Thames.
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RBINS Staff Publications 2021
