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Article Reference Mammals from the Paleocene-Eocene transition in Belgium (Tienen Formation, MP7): Paleobiogeographical and biostratigraphical implications
Located in Library / RBINS Staff Publications
Inproceedings Reference Mandibles from Palaeolithic dogs and Pleistocene wolves at Předmostí, the Czech Republic
Located in Library / RBINS Staff Publications
Proceedings Reference Mangrove Insect Project (MIP): Species discovery, inventroy and habitat assessment
Located in Library / RBINS Staff Publications
Article Reference MARS: multimedia archaeological research system
26. Semal P., Cornelissen E. & Cauwe N., 2004. MARS: multimedia archaeological research system. Notae Praehistoricae, 24 : 203-208.
Located in Library / RBINS Staff Publications
Article Reference Metapopulation processes affecting diversity and distribution of myrmecophiles associated with red wood ants.
Located in Library / RBINS Staff Publications
Article Reference Micro-computed tomography for natural history specimens: a handbook of best practice protocols
Micro-computed tomography (micro-CT or microtomography) is a non-destructive imaging technique using X-rays which allows the digitisation of an object in three dimensions. The ability of micro-CT imaging to visualise both internal and external features of an object, without destroying the specimen, makes the technique ideal for the digitisation of valuable natural history collections. This handbook serves as a comprehensive guide to laboratory micro-CT imaging of different types of natural history specimens, including zoological, botanical, palaeontological and geological samples.
Located in Library / RBINS Staff Publications 2019
Inproceedings Reference Microfacies analysis of a middle to upper Frasnian succession at the Lompret quarry (SW Belgium) documenting a transition from the Lion reef to deep marine Neuville and Matagne environments
Located in Library / RBINS Staff Publications 2018
Article Reference Microfossils in calculus demonstrate consumption of plants and cooked foods in Neanderthal diets (Shanidar III, Iraq; Spy I and II, Belgium).
The nature and causes of the disappearance of Neanderthals and their apparent replacement by modern humans are subjects of considerable debate. Many researchers have proposed biologically or technologically mediated dietary differences between the two groups as one of the fundamental causes of Neanderthal disappearance. Some scenarios have focused on the apparent lack of plant foods in Neanderthal diets. Here we report direct evidence for Neanderthalconsumption of a variety of plant foods, in the form of phytoliths and starch grains recovered from dental calculus of Neanderthal skeletons from Shanidar Cave, Iraq, and Spy Cave, Belgium. Some of the plants are typical of recent modern human diets, including date palms (Phoenix spp.), legumes, and grass seeds (Triticeae), whereas others are known to be edible but are not heavily used today. Many of the grass seed starches showed damage that is a distinctive marker of cooking. Our results indicate that in both warm eastern Mediterranean and cold northwestern European climates, and across their latitudinal range, Neanderthalsmade use of the diverse plant foods available in their local environment and transformed them into more easily digestible foodstuffs in part through cooking them, suggesting an overall sophistication in Neanderthal dietary regimes.
Located in Library / RBINS collections by external author(s)
Article Reference Microorganization of ovaries and oogenesis of Haplotaxis sp. (Clitellata: Haplotaxidae)
Located in Library / RBINS Staff Publications 2020
Article Reference Micropalaeontological dating of the Prémontré mammal fauna (MP10, Prémontré Sands, EECO, early late Ypresian, Paris Basin).
At their type locality the Prémontré Sands contain fairly well-diversified organic-walled microfossil assemblages attributable to the lower part of dinoflagellate cyst Zone D9 and indicating a transition from an estuarine to a lagoonal depositional regime, up-section as well as laterally. Identical assemblages have been recorded in the inner to mid-neritic Merelbeke Clay Member in Belgium, allowing the Prémontré Sands to be positioned within lower NP13 and early Chron C22r. The deposition of the MP10 Prémontré mammal fauna is estimated to postdate the onset of both NP13 and Chron C22r, which are nearly coincident, by about 200 to 300 kyr. The biostratigraphic dating refers this deposit to the early late Ypresian and to the final phase of the Early Eocene Climatic Optimum (EECO) at about 50.4 to 50.3 million years ago. The Prémontré Sands, as well as their distal equivalent the Merelbeke Clay Member, were deposited following a major sea-level rise, the highest of the late Ypresian in the southern North Sea Basin s.l. (including the Paris Basin). They are separated from the overlying “Glauconie grossière” (zone NP14; middle part of zone D9) by a hiatus of approximately 2.5 myr.
Located in Library / RBINS Staff Publications 2016