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Article Reference The bats of the Congo and of Rwanda and Burundi Revisited (Mammalia: Chiroptera)
Located in Library / RBINS Staff Publications 2017
Article Reference The bee genus Colletes Latreille 1802 in Ethiopia (Hymenoptera: Apoidea: Colletidae)
Located in Library / RBINS Staff Publications
Book Reference The Belgian Quaternary mammals, a bibliography 1819- 1981
Located in Library / RBINS Staff Publications
Article Reference The boundary between the Middle Eocene Brussel Sand and the Lede Sand Formations in the Zaventem-Nederokkerzeel area (Northeast of Brussels, Belgium).
Located in Library / RBINS Staff Publications
Article Reference The cave bear (Ursus spelaeus) from Goyet, Belgium. The bear den in Chamber B (bone horizon 4)
Located in Library / RBINS Staff Publications
Article Reference The checklist of Northeast China's subfamily Prioninae and biological obeservation of Callipogon (Eoxenus) relictus Semenov-Tian-Shanskij, 1899 (Coleoptera, Cerambycidae, Prioninae)
Located in Library / RBINS Staff Publications
Article Reference The cicada genus karenia Distant, 1888 (Hemiptera : Cicadidae), with description of a new species
Located in Library / RBINS Staff Publications
Article Reference The composite Kortrijk section (W Belgium): a key reference for mid-Ypresian (Early Eocene) stratigraphy in the southern North Sea Basin.
The upper part of the Kortrijk Clay Formation (the Roubaix Clay and Aalbeke Clay Members of mid-Ypresian age) has been exposed in road and canal cuttings and clay quarries in the Kortrijk area (western Belgium), and penetrated by several cored boreholes. It is overlain disconformably by the Mont-Panisel Sand Member of the Hyon Sand Formation (upper middle Ypresian). The Roubaix Clay Member contains diverse and well-preserved calcareous nannofossils, dinoflagellate cysts, foraminifera, ostracods and other calcitic microfossils, and less well-preserved mollusc assemblages, while the Aalbeke Clay Member is secondarily decalcified. The calcareous nannofossil subdivision of upper NP11 and lower NP12 has been recognised in the Kortrijk area, and calibrated with the NW European mid-Ypresian dinoflagellate cyst, ostracod and planktonic foraminiferal zones and datums (e.g. Subbotina influx). Several medium-scale depositional sequences, with an estimated duration of 400 kyr or less, have been recorded. Their respective boundaries coincide with the resistivity maxima identified on the majority of the wireline log profiles of the Belgian Ypresian. Integrated biostratigraphic, magnetostratigraphic and sequence stratigraphic analysis enables correlation with other areas in Belgium, with the London Clay Formation of southern England, and with the standard chronostratigraphic scale. A marine erosion surface has been identified at the base of Unit 20 in the Kortrijk area (mid-Ypresian, early Biochron NP12, middle C24n.1n, ~ 52.8 Ma), corresponding to the first occurrence of estuarine channel-fill units in southern England. This indicates a brief but profound sea-level fall, either eustatically or tectonically controlled. The composite Kortrijk section is proposed as a reference section for the middle Ypresian in the southern North Sea Basin, and for similar settings in mid- to high-latitudes of the Northern Hemisphere (e.g. Kazakhstan and Crimea).
Located in Library / RBINS Staff Publications 2017
Book Reference The correlation of Famennian and Tournaisian deposits of the USSR and French-Belgian basin on conodonts
Located in Library / RBINS Staff Publications
Article Reference The cost of CO2 geological storage is more than a number
CO2 geological storage is the last stage in the CO2 capture and storage process which aims to reduce CO2 emissions into the atmosphere. The cost of storage has frequently been regarded as minor compared to the cost of the whole CCS process. There are however a multitude of cost parameters that will form a unique combination for each storage project, with costs projected from one to several tens of euros per tonne of CO2 stored. Several research efforts have lately been identifying the main cost drivers and relatively wide cost ranges. Reservoir type and location, geological uncertainty, injectivity and capacity are recognised as the main source of cost variation between potential storage projects.
Located in Library / RBINS Staff Publications