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Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/19910
DC FieldValueLanguage
dc.contributor.authorPetit-Maire, Nicolees
dc.contributor.authorDelibrias, G.es
dc.contributor.authorMeco, J.es
dc.contributor.authorPomel, René-Simones
dc.contributor.authorRosso, Jean-Claudees
dc.date.accessioned2017-01-18T03:30:33Z-
dc.date.accessioned2018-06-18T06:45:37Z-
dc.date.available2017-01-18T03:30:33Z-
dc.date.available2018-06-18T06:45:37Z-
dc.date.issued1987es
dc.identifier.issn0168-6208es
dc.identifier.urihttp://hdl.handle.net/10553/19910-
dc.description.abstractFuerteventura, the most arid island in the Canary archipelago, due to its location about 100km off the Saharan coast of Morocco, holds important Quaternary deposits indicating recent climatic change. Three levels with Hymenoptera nests and terrestrial mollusk shells were observed in the fixation of the dunes by vegetation: they are radiocarbon dated at 23.600 ± 550 BP, 15.000 ± 200 BP and 9.800 ± 140 BP.en
dc.formatapplication/pdfes
dc.languageenges
dc.sourcePalaeoecology of Africa and the Surrounding Islands [ISSN 0168-6208], t. 18, p. 351-356es
dc.subject24 Ciencias de la vidaes
dc.subject2416 Paleontologíaes
dc.subject250205 Paleoclimatologíaes
dc.titlePaleoclimats de L´ile de Fuerteventura ( Archipel Canarien)es
dc.typeinfo:eu-repo/semantics/articlees
dc.typeArticlees
dc.identifier.absysnet218751es
dc.investigacionCienciases
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesses
dc.type2Artículoes
dc.identifier.ulpgcSíes
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.author.orcid0000-0001-7658-9956-
crisitem.author.fullNameMeco Cabrera, Joaquín Francisco-
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