Please use this identifier to cite or link to this item: http://earsiv.odu.edu.tr:8080/xmlui/handle/11489/5208
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dc.contributor.authorBiltekin, Demet-
dc.contributor.authorBurjachs, Francesc-
dc.contributor.authorVallverdu, Josep-
dc.contributor.authorSharp, Warren D.-
dc.contributor.authorMertz-Kraus, Regina-
dc.contributor.authorGema Chacon, M.-
dc.contributor.authorSaladie, Palmira-
dc.contributor.authorBischoff, James L.-
dc.contributor.authorCarbonell, Eudald-
dc.date.accessioned2024-03-26T06:48:52Z-
dc.date.available2024-03-26T06:48:52Z-
dc.date.issued2019-
dc.identifier.citationBiltekin, D., Burjachs, F., Vallverdú, J., Sharp, WD., Mertz-Kraus, R., Chacón, MG., Saladié, P., Bischoff, JL., Carbonell, E. (2019). Vegetation and climate record from Abric Romani (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d-3). Quat. Sci. Rev., 220, 154-164. https://doi.org/10.1016/j.quascirev.2019.07.035en_US
dc.identifier.issn0277-3791-
dc.identifier.urihttp://dx.doi.org/10.1016/j.quascirev.2019.07.035-
dc.identifier.urihttps://www.webofscience.com/wos/woscc/full-record/WOS:000487565700009-
dc.identifier.urihttp://earsiv.odu.edu.tr:8080/xmlui/handle/11489/5208-
dc.descriptionWoS Categories: Geography, Physical; Geosciences, Multidisciplinaryen_US
dc.descriptionWeb of Science Index: Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)en_US
dc.descriptionResearch Areas: Physical Geography; Geologyen_US
dc.description.abstractThis study addresses the pollen record of Abric Romani archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of Artemisia steppes during the second part of the MIS 5a indicates that the degree of continentality can be related to the low winter temperatures and precipitation. During MIS 4, a colder and dryer climate enabled the development of open vegetation (dominated by Artemisia with Poaceae and other Asteraceae) around the study site. (C) 2019 Elsevier Ltd. All rights reserved.en_US
dc.description.sponsorshipScientific and Technological Research Council of Turkey (TUBITAK); Government of Catalonia [2009 SGR 813]; TUBITAKen_US
dc.language.isoengen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD-OXFORDen_US
dc.relation.isversionof10.1016/j.quascirev.2019.07.035en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectPollen analysis, Tufas, Palaeoclimatology, Palaeovegetation, NE Iberian Peninsulaen_US
dc.subjectGRANDE DI MONTICCHIO, POLLEN RECORD, LAST, NEANDERTHAL, HOLOCENE, SPAIN, PADUL, CAVE, PALEOENVIRONMENT, RECONSTRUCTIONen_US
dc.titleVegetation and climate record from Abric Romani (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d-3)en_US
dc.typearticleen_US
dc.relation.journalQUATERNARY SCIENCE REVIEWSen_US
dc.contributor.departmentOrdu Üniversitesien_US
dc.contributor.authorID0000-0002-3177-3263en_US
dc.contributor.authorID0000-0003-2976-0321en_US
dc.contributor.authorID0000-0002-1730-8461en_US
dc.identifier.volume220en_US
dc.identifier.startpage154en_US
dc.identifier.endpage164en_US
Appears in Collections:Deniz Bilimleri ve Teknolojisi

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