Mots-clés
Datation Th/U ; Datation isotopique ; Grotte ; Interglaciaire ; Israël ; Jérusalem ; Karst ; Oxygène 18 ; Paléoclimat ; Quaternaire ; Stalagmite ; Variation climatiqueCave ; Climatic variation ; Interglacial ; Isotope dating ; Israel ; Jerusalem ; Karst ; Oxygen 18 ; Palaeoclimate ; Quaternary ; Th/U datingContinental oxygen isotopic record of the last 170,000 years in Jerusalem
Auteurs :FRUMKIN, A.
FORD, D.C.
SCHWARCZ, H.P.
Description :
A long radiometrically dated oxygen isotopic record of continental climatic variations since the penultimate glaciation was obtained from a stalagmite deposited in a sealed cave in Jerusalem. This record shows that speleothems have the potential of assigning dates to long- and short-term climatic events, with possible refining of Milankovitch tuning of ice and marine records which themselves are not datable. Short-term (1000-yr) events are very significant in the region, reaching 50% of glacial/interglacial fluctuations. The Mediterranean Sea was the most probable source of local precipitation throughout the last glacial cycle.
Type de document :
Article de périodique
Source :
Quaternary research, issn : 0033-5894, 1999, vol. 51, n°. 3, p. 317-327, Collation : Illustration, Références bibliographiques : 60 ref.
Date :
1999
Editeur :
Pays édition : Etats-Unis, San Diego, CA, Elsevier
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)