Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/1617
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dc.contributor.authorSala, Nohemi-
dc.contributor.authorPablos Fernández, Adrián-
dc.contributor.authorGómez-Olivencia, Azier-
dc.contributor.authorSanz-Royo, Alicia-
dc.contributor.authorVillalba, Mónica-
dc.contributor.authorPantoja-Pérez, Ana-
dc.contributor.authorLaplana, César-
dc.contributor.authorArsuaga, Juan Luis-
dc.contributor.authorAlgaba, Milagros-
dc.date.accessioned2019-12-
dc.date.accessioned2019-12-05T14:45:51Z-
dc.date.issued2020-01-
dc.identifier.citationQuaternary Science Reviews, 2020, 228, 106027es_ES
dc.identifier.issn0277-3791-
dc.identifier.issn1873-457X-
dc.identifier.urihttp://hdl.handle.net/20.500.12136/1617-
dc.description.abstractThe environmental conditions that existed during the period between 45 and 30 ka are of vital importance for addressing the transition between the Middle and Upper Paleolithic. It seems to be a hiatus of Paleolithic populations, a “no (hu)man’s land” in Central Iberia, coinciding with the mid part of Marine Isotope Stage (MIS) 3, between 42 and 28 cal kyr BP. This break in the archaeological record makes it difficult to address this period paleoecologically. Here we present a new cave site, Portalón del Tejadilla (Segovia), dated to a period roughly between ∼34.2 and 40.4 cal kyr BP in which cold-adapted faunas, such as woolly rhinoceros and giant deer, have been recovered in a hyena den site context. This site is located in Central Iberia, and more specifically, on the southern edge of the northern Plateau, an unexpected region for the presence of these faunas during the MIS 3. These new findings extend the geographical distribution of several species, including Coelodonta antiquitatis and Megaloceros giganteus. Furthermore, they document a climatic deterioration (colder and dryer) during the mid MIS 3 in Central Iberia in one of the coldest and driest episodes of the Late Pleistocene. Portalón del Tejadilla fills this temporal gap and provides valuable paleoecological information about the transition between the Middle to Upper Paleolithic.es_ES
dc.description.sponsorshipN-S is supported by a Juan de la Cierva Incorporación postdoctoral contract (IJCI-2017-32804). AP-P received a Fundación Atapuerca research fellowship in 2017. AGO is funded by a Ramón y Cajal fellowship (RYC-2017-22558) and also receives support from Research Group IT1044-16 from the Eusko Jaurlaritza-Gobierno Vasco and Group PPG17/05 from Universidad del País Vasco-Euskal Herriko Unibertsitatea.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectPaleobiogeographyes_ES
dc.subjectPaleoecologyes_ES
dc.subjectTundra-steppees_ES
dc.subjectPortalón del Tejadillaes_ES
dc.subjectCoelodonta antiquitatises_ES
dc.subjectMegaloceros giganteouses_ES
dc.subjectTaphonomyes_ES
dc.titleCentral Iberia in the middle MIS 3. Paleoecological inferences during the period 34–40 cal kyr BPes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quascirev.2019.106027-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quascirev.2019.106027es_ES
dc.date.available2019-12-05T14:45:51Z-
Appears in Collections:Paleobiología
Colecciones, Conservación y Restauración
Arqueomagnetismo



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