000169072 001__ 169072
000169072 005__ 20260218135106.0
000169072 0247_ $$2doi$$a10.1016/j.revpalbo.2020.104240
000169072 0248_ $$2sideral$$a117728
000169072 037__ $$aART-2020-117728
000169072 041__ $$aeng
000169072 100__ $$aAranbarri, J.
000169072 245__ $$aHolocene history of Aleppo pine (Pinus halepensis Mill.) woodlands in the Ebro Basin (NE Spain): Climate-biased or human-induced?
000169072 260__ $$c2020
000169072 5060_ $$aAccess copy available to the general public$$fUnrestricted
000169072 5203_ $$aThis paper reviews the past distribution of Aleppo pine woodlands in the Ebro Basin, Northeastern Iberia, from the Mesolithic to Modern times based on wood charcoal data. The aim is to detail the chronological timing and the drivers explaining the long-term presence of Aleppo pine woodlands and associated thermophilous flora. The available charcoal data support the early spread of Pinus halepensis during the Mesolithic (ca. 9000 cal BP) accompanied by Mediterranean trees and shrubs like Quercus sp. evergreen, Juniperus sp., Arbutus unedo, Pistacia lentiscus, Rhamnus/Phillyrea, Cistaceae, and Rosmarinus officinalis, as a local response to global climate change in the Early Holocene. During the arrival and the propagation of the Neolithic culture (ca. 7500–5500 cal BP), anthracological records, as well as regional palynological sequences, demonstrate the progressive replacement of an conifer-dominated open parkland by both Quercus sp. deciduous and evergreen woodlands in response to the Middle Holocene rise in temperature and humidity. This evidence, however, converges with the general idea that the presence and the spread of Pinus halepensis and associated scrubland have usually been attributed to the onset of landscape anthropization. The frequency of xero-thermophilous open scrubland and the use of Aleppo pine for fuel and woodcrafting progressively increased during the Bronze and Iron Ages, and especially in Ibero-Roman and Medieval/Islamic times, when the vegetation landscape in the Middle Ebro Basin was largely deforested as a consequence of increasing demographic pressure, grazing and the establishment of proto-urban centers.
000169072 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/DINAMO 2 CGL2012-33063$$9info:eu-repo/grantAgreement/ES/MINECO/DINAMO 3 CGL2015-69160-R$$9info:eu-repo/grantAgreement/ES/MINECO/HAR2016-78277-R$$9info:eu-repo/grantAgreement/ES/MINECO/HAR2017-85023-P
000169072 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
000169072 590__ $$a1.94$$b2020
000169072 591__ $$aPLANT SCIENCES$$b116 / 235 = 0.494$$c2020$$dQ2$$eT2
000169072 591__ $$aPALEONTOLOGY$$b18 / 54 = 0.333$$c2020$$dQ2$$eT2
000169072 592__ $$a0.737$$b2020
000169072 593__ $$aPaleontology$$c2020$$dQ1
000169072 593__ $$aEcology, Evolution, Behavior and Systematics$$c2020$$dQ1
000169072 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000169072 700__ $$0(orcid)0000-0003-4280-3971$$aAlcolea, M.
000169072 700__ $$aBadal, E.
000169072 700__ $$aVila, S.
000169072 700__ $$aAllué, E.
000169072 700__ $$aIriarte-Chiapusso, M.J.
000169072 700__ $$0(orcid)0000-0002-7646-0826$$aSebastián, M.$$uUniversidad de Zaragoza
000169072 700__ $$aMagri, D.
000169072 700__ $$0(orcid)0000-0002-5097-1468$$aGonzález-Sampériz, P.$$uUniversidad de Zaragoza
000169072 7102_ $$14013$$2210$$aUniversidad de Zaragoza$$bDpto. Didácticas Específicas$$cÁrea Didáctica Ciencias Socia.
000169072 7102_ $$12000$$2427$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Externa
000169072 773__ $$g279 (2020), 104240 [15 pp.]$$pRev. palaeobot. palynol.$$tReview of Palaeobotany and Palynology$$x0034-6667
000169072 8564_ $$s495010$$uhttps://zaguan.unizar.es/record/169072/files/texto_completo.pdf$$yPostprint
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000169072 951__ $$a2026-02-18-12:23:41
000169072 980__ $$aARTICLE