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Note on the taxonomy of the Microtus (Iberomys) (Arvicolinae, Rodentia) from the Late Pleistocene of Gruta do Caldeirao (Tomar, Portugal) and paleoclimatic interpretation of the rodent assemblage

Journal

ESTUDIOS GEOLOGICOS-MADRID
Volume 76, Issue 1, Pages -

Publisher

CONSEJO SUPERIOR INVESTIGACIONES CIENTIFICAS-CSIC
DOI: 10.3989/egeol.43622.542

Keywords

Microtus (Iberomys) cabrerae; Middle to Upper Paleolithic; Paleoclimatic reconstruction; Last Glacial Maximum; Western Iberia

Categories

Funding

  1. Jose Castillejo project of the Spanish Ministry of Science, Innovation and Universities [CAS18/00095]
  2. Ramon y Cajal contract [RYC-2016-19386]
  3. Spanish Ministry of Science, Innovation and Universities
  4. project Archaeology and Evolution of Early Humans in the Western Facade of Iberia - FCT (Fundacao para a Ciencia e a Tecnologia, Portugal) [PTDC/HAR-ARQ/30413/2017]
  5. Fundação para a Ciência e a Tecnologia [PTDC/HAR-ARQ/30413/2017] Funding Source: FCT

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Gruta do Caldeirao is an archaeological cave site located in Tomar (Portugal, western Iberian Peninsula), which contains an important Late Pleistocene sequence from Middle Paleolithic (Mousterian) to Upper Paleolithic (Solutrean-Magdalenian), including lithic tools, human remains, and other large- and small-vertebrate remains. Our revision and interpretation of the rodent assemblage previously published in the 1990s leads to three important conclusions: 1) the only species of the subgenus Iberomys present in the sequence is the current endemic Iberian vole species Microtus (Iberomys) cabrerae (Cabrera's vole); 2) the rodent assemblage is dominated throughout by open-forest species, such as the long-tailed field mouse (Apodemus sylvaticus), and species associated with open-humid areas such as the Mediterranean and Lusitanian pine voles (Microtus (Terricola) spp.), with the notable presence of an extinct hamster (Allocricetus bursae) in layer K, and three vole species not currently found in the vicinity of the cave (Microtus arvalis [the common vole], M. agrestis [the field vole], and Chionomys nivalis [the European snow vole]) also in the assemblage; 3) the bioclimatic model, which is used to reconstruct climatic parameters on the basis of the rodent association, corroborates the proposal that the Solutrean occupation from layers H to Fa took place during a cold period equated to the Last Glacial Maximum (LGM), as indicated by the available radiocarbon dates and supported by the magnetic susceptibility data.

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