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dc.contributor.authorLeira, M.
dc.contributor.authorFernández Mosquera, Daniel
dc.date.accessioned2010-01-25T09:33:55Z
dc.date.available2010-01-25T09:33:55Z
dc.date.issued1998
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1998, 23: 251-261 ISSN: 00213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6382
dc.description.abstract[Abstract] Profiles of percent carbon, nitrogen and phosphorus, carbon/nitrogen (C/N) ratios, percent organic matter and carbonates, and stable carbon (δ13C) and nitrogen (δ15N) from a 176 cm core were used to reconstruct environments of deposition in the Amboromena basin (Madagascar)during last 12,000 yr BP. From these profiles three distinctively different stages in the basin evolution were apparent, which could have been result from the response to changes in the climatic conditions. Similar changes has been observed in other works about climate evolution in Madagascar and the African Tropics during the Late Quaternary.
dc.language.isoenges_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectMadagascares_ES
dc.subjectAndringitra Massifes_ES
dc.subjectStable isotopeses_ES
dc.subjectδ13Ces_ES
dc.subjectδ15Nes_ES
dc.subjectLate Quaternaryes_ES
dc.subjectPaleoenvironmentales_ES
dc.subjectReconstructiones_ES
dc.titleA 12,000 yr δ13C and δ15N isotopic record from Amboromena, Andringitra Massif, in Madagascares_ES
dc.title.alternativeRegistro isotópico de δ13 C y δ15 N de 12.000 años de antigüedad de Amboromena (Macizo de Andringitra, Madagascar)
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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