000169154 001__ 169154
000169154 005__ 20260220162133.0
000169154 0247_ $$2doi$$a10.1177/09596836221095992
000169154 0248_ $$2sideral$$a136041
000169154 037__ $$aART-2022-136041
000169154 041__ $$aeng
000169154 100__ $$0(orcid)0000-0003-4280-3971$$aAlcolea, Marta
000169154 245__ $$aA southern refugium for temperate tree species in the Mediterranean mountains of El Port massif (NE Iberia): Charcoal analysis at Cova Del Vidre
000169154 260__ $$c2022
000169154 5060_ $$aAccess copy available to the general public$$fUnrestricted
000169154 5203_ $$aThis study focuses on the analysis of wood charcoal from Cova del Vidre (Roquetes, Tarragona, Spain). This cave, located at an altitude of 1000 m a.s.l., is a key site for understanding the transition from hunting and gathering to farming in a mountainous region of north-eastern Iberia so far unexplored by archaeobotany. The anthracological study is based on four archaeological levels from the Epipalaeolithic to the Early Neolithic dated between 12.9 and 6.8 kyr cal BP, that is, from the Late Glacial period to the Middle Holocene. During the Younger Dryas, the record is dominated by a little varied spectrum of cryophilous pines ( Pinus tp. sylvestris) and thorny shrubs revealing an open landscape where Prunus may prefigure the spread of temperate taxa. In the Early Holocene, a significant change in temperature and precipitation is evidenced, which promoted successional changes in plant communities, with a decline of pine and the sudden rise of temperate/Mediterranean taxa, such as Prunus and Quercus coccifera/ilex. During the Middle Holocene, other temperate taxa appear, such as Quercus deciduous, Buxus sempervirens and Taxus baccata, with yew finally dominating the anthracological record. The appearance and early development of temperate or Mediterranean species as early as the Younger Dryas and the Early Holocene periods, in a mountain context that had long been favourable for Scots pine, allows us to argue the local existence of a glacial refugium. Differences with the nearby sites in the lowlands demonstrate that altitudinal differences in vegetation were already established in the Holocene. Furthermore, the site helps to define the palaeodistribution of Taxus baccata, Abies alba and Fagus sylvatica in southern Europe.
000169154 540__ $$9info:eu-repo/semantics/openAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000169154 590__ $$a2.4$$b2022
000169154 591__ $$aGEOGRAPHY, PHYSICAL$$b27 / 49 = 0.551$$c2022$$dQ3$$eT2
000169154 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b113 / 202 = 0.559$$c2022$$dQ3$$eT2
000169154 592__ $$a1.025$$b2022
000169154 593__ $$aArcheology (arts and humanities)$$c2022$$dQ1
000169154 593__ $$aEarth-Surface Processes$$c2022$$dQ1
000169154 593__ $$aPaleontology$$c2022$$dQ1
000169154 593__ $$aEcology$$c2022$$dQ1
000169154 593__ $$aGlobal and Planetary Change$$c2022$$dQ2
000169154 594__ $$a5.3$$b2022
000169154 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000169154 700__ $$aChabal, Lucie
000169154 700__ $$aBosch-Arguilagós, Josep
000169154 700__ $$aPiqué, Raquel
000169154 773__ $$g32, 8 (2022), 794-806$$pHolocene$$tHolocene$$x0959-6836
000169154 8564_ $$s431045$$uhttps://zaguan.unizar.es/record/169154/files/texto_completo.pdf$$yPostprint
000169154 8564_ $$s2106201$$uhttps://zaguan.unizar.es/record/169154/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000169154 909CO $$ooai:zaguan.unizar.es:169154$$particulos$$pdriver
000169154 951__ $$a2026-02-20-14:54:02
000169154 980__ $$aARTICLE