Search publications of the members of the Royal Belgian institute of natural Sciences
-
Faunal remains from some Transbaikal sites: an analysis of bone representation and bone modification in the early Upper Palaeolithic of Eastern Siberia
-
Faunal remains from Kamenka, Buryatia: an analysis of the spatial distribution, bone representation and bone modification in the Early Upper Palaeolithic of Eastern Siberia
-
L’origine paléolithique du chien
-
« Messages d’os »
-
La faune pléistocène de Goyet
-
Le rôle de l’environnements dans les comportements des chasseurs-cueilleurs préhistoriques
-
"WARD, P.D.: The call of distant mammoths. Why the Ice Age mammals disappeared. Copernicus, Springer-Verlag, New York, 1997"
-
Van mens tot mens
-
Van mensen en mammoeten
-
Het leven tijdens de ijstijden
-
De mammoetfauna van noordelijk Eurazië
-
Archaeozoological investigations of Upper Palaeolithic sites from Northern Eurasia.
-
Complementary contribution to the study of the entomological fauna of Borneo island with the description of a new subspecies in the genus Aegosoma Audinet-Serville, 1832 (Coleoptera, Cerambycidae, Prioninae)
-
The Asaila depression, an archaeological landscape in Qatar
-
A mid-Holocene candidate tsunami deposit from the NW Cape (Western Australia)
-
Tsunami deposits of the Caribbean – Towards an improved coastal hazard assessment
-
New Sediment Cores Reveal Environmental Changes Driven by Tectonic Processes at Ancient Helike, Greece
- According to various historical sources an earthquake and an associated tsunami wiped out the Greek city of Helike on the Gulf of Corinth in 373 B.C. This study combines stratigraphical data from a new series of sediment cores with archaeological findings of the Helike Project to better assess the fate of Helike. Abrupt lithological changes, for example, from coarse-grained littoral facies at the base to fine-grained lagoonal deposits, in three of the new cores suggest sudden formation of lagoonal or lacustrine conditions in the central delta during tectonic events of subsidence due to fault-slip. These events date before c. 2550 B.C., before 348 cal. B.C.–64 cal. A.D. (probably 373 B.C.), and before 1437–1634 cal. A.D. (probably A.D. 1402). Vertically displaced isochronic surfaces between two neighboring cores may be related to active faulting of the fan-delta north of the Western Helike Fault Zone in 373 B.C. and A.D. 1402. Although the Helike Project reported possible tsunami evidence in earlier cores and trenches, no unequivocal sedimentary traces of a tsunami were identified in the Classical horizons of the new cores.
-
Typhoon Haiyan's sedimentary record in coastal environments of the Philippines and its palaeotempestological implications
-
Life and death after super typhoon Haiyan
-
Block and boulder transport in Eastern Samar (Philippines) during Supertyphoon Haiyan
