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dc.contributor.authorAlvarez Vena, Adrian
dc.contributor.authorBallesteros Posada, Daniel 
dc.date.accessioned2023-06-15T11:42:27Z
dc.date.available2023-06-15T11:42:27Z
dc.date.issued2023-03-01
dc.identifier.citationA. Álvarez-Vena et al. Mammalian turnover as an indicator of climatic and anthropogenic landscape modification: A new Meghalayan record (Late Holocene) in northern Iberia. Palaeogeography, Palaeoclimatology, Palaeoecology 616 (2023) 111476[https://doi.org/10.1016/j.palaeo.2023.111476]es_ES
dc.identifier.urihttps://hdl.handle.net/10481/82508
dc.descriptionAcknowledgements AB.M-A. developed part of this research as part of the ERC Consoli- dator Grant (SUBSILIENCE ref. 818299). We thank J.A. Delgado for his technical work on studying macromammal assemblage. Financial sup- port was provided by the Bilbao Port Authority (Autoridad Portuaria de Bilbao) within the project “Estabilizaci´on del sector occidental de la Cantera de Punta Lucero en el Puerto de Bilbao”. We are also grateful to Juan Manuel L´opez-García and the anonymous reviewer for their sug- gestions and comments that strongly improved the manuscript.es_ES
dc.descriptionSupplementary data to this article can be found online at https://doi.org/10.1016/j.palaeo.2023.111476es_ES
dc.description.abstractThe Punta Lucero III cave is a natural trap where abundant vertebrate remains were accumulated during the Meghalayan (Late Holocene). To better understand the paleoenvironmental conditions in which this record was accumulated, the micromammal assemblage, comprising a minimum number of 1396 individuals belonging to 19 taxa, was studied using the Mutual Ecogeographic Range and the Habitat Weighting Method. Throughout ~2600 years, the micromammal community's quick turnover reflected a shift from patchy forests and humid meadows to open, shrubbier grasslands. The Late Holocene Thermal Maximum's humid and mild climatic conditions underwent a cooling and aridification phase, coeval with the Iron Age Cold Epoch. These concluded in a slight temperature rising, coeval with the Roman Warm Period. Macromammals experienced a shift from wild populations to domestic herds. Therefore, this work discusses a broader context for this mammalian turnover from a human cultural perspectivees_ES
dc.description.sponsorshipERC Consolidator Grant (SUBSILIENCE ref. 818299)es_ES
dc.description.sponsorshipBilbao Port Authority (Autoridad Portuaria de Bilbao)es_ES
dc.description.sponsorshipEstabilización del sector occidental de la Cantera de Punta Lucero en el Puerto de Bilbaoes_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsAtribución 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectClimatic changees_ES
dc.subjectChalcolithices_ES
dc.subjectBronze age es_ES
dc.subjectIron age es_ES
dc.subjectMicromys minutuses_ES
dc.subjectMus musculuses_ES
dc.titleMammalian turnover as an indicator of climatic and anthropogenic landscape modification: A new Meghalayan record (Late Holocene) in northern Iberiaes_ES
dc.typejournal articlees_ES
dc.rights.accessRightsopen accesses_ES
dc.identifier.doi10.1016/j.palaeo.2023.111476
dc.type.hasVersionVoRes_ES


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