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dc.contributor.authorLópez González, F.
dc.contributor.authorGrandal-d'Anglade, Aurora
dc.contributor.authorVidal Romaní, Juan Ramón
dc.date.accessioned2010-01-22T13:26:19Z
dc.date.available2010-01-22T13:26:19Z
dc.date.issued1997
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1997, 22: 67-80 ISSN: 0213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6279
dc.description.abstract[Abstract] This paper deal with the biostratinomic processes and fossildiagenetic processes which affected the bone rest of Pleistocene age from the Liñares Sur carstic cave. AH show that the active processes was creepy remaining the fossil bones close ro the original situation of the animal and showing a distinctive intervention of rodents (rooth marks) inmediately after the death of those. The burial was produced by solifiuxion which includes bone remains in between clays and shales resulting from the decalcification ofthe hybrid limesrones that constitutes the cave. After this happened the bones were affected by edaphic processes becoming encrusted, patinated and tinged by Fe and Mn oxides.
dc.language.isospaes_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectTaphonomyes_ES
dc.subjectUpper Pleistocenees_ES
dc.subjectGaliciaes_ES
dc.titleAnálisis tafonómico de la muestra ósea de Liñares sur (Lugo, Galicia)es_ES
dc.title.alternativeTaphonomic study of the bone sample of Liñares sur (Lugo, Galicia)
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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