000108322 001__ 108322 000108322 005__ 20230526092850.0 000108322 0247_ $$2doi$$a10.1016/j.quaint.2020.10.029 000108322 0248_ $$2sideral$$a121217 000108322 037__ $$aART-2020-121217 000108322 041__ $$aeng 000108322 100__ $$aAlcolea, M. 000108322 245__ $$aDendro-anthracological tools applied to Scots type pine forests exploitation as fuel during the Mesolithic-Neolithic transition in the southern central pre-Pyrenees (Spain) 000108322 260__ $$c2020 000108322 5060_ $$aAccess copy available to the general public$$fUnrestricted 000108322 5203_ $$aThis work focuses on the reconstruction of fuelwood procurement during the Mesolithic-Neolithic transition in the southern central Pre-Pyrenees (Spain). The study combines wood charcoal identification with the application of dendro-anthracological approaches in the archaeological sequence of Esplugón (9.4–6.8 kyr cal BP) (Sabiñanigo, Huesca). Scots type pine (Pinus sylvestris tp.) reaches in this record around 90% of exploited firewood in line with its abundance in the inner Iberia mountainous areas during the onset of the Holocene. The classification of pine wood fragments in anthraco-groups is based on the combination of different dendro-anthracological tools: i) pith location tool and wood diameter estimation based on the trigonomethric method tool (ADmodel), ii) the study of growth rate based on the annual tree-ring width measurements, and iii) a modern dendrological dataset. There are hardly any differences observed in firewood procurement between the last hunter-gatherers and the first farmers in the long sequences from rock-shelters with recurrent human occupations. First results from this site point to the exploitation of whole trees but a high use of small pine branches probably from the gathering of branch shedding. 000108322 536__ $$9info:eu-repo/grantAgreement/ES/MICINN/Vacios y ocupaciones en la Prehistoria de la Cuenca del Ebro$$9info:eu-repo/grantAgreement/ES/MINECO/HAR2017-85023-P 000108322 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/ 000108322 590__ $$a2.13$$b2020 000108322 591__ $$aGEOGRAPHY, PHYSICAL$$b36 / 50 = 0.72$$c2020$$dQ3$$eT3 000108322 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b125 / 198 = 0.631$$c2020$$dQ3$$eT2 000108322 592__ $$a0.927$$b2020 000108322 593__ $$aEarth-Surface Processes$$c2020$$dQ1 000108322 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion 000108322 700__ $$aDufraisse, A. 000108322 700__ $$aRoyo, M.$$uUniversidad de Zaragoza 000108322 700__ $$0(orcid)0000-0001-5506-8510$$aMazo, C.$$uUniversidad de Zaragoza 000108322 700__ $$0(orcid)0000-0002-7585-3636$$ade Luis, M.$$uUniversidad de Zaragoza 000108322 700__ $$0(orcid)0000-0002-9558-1308$$aLongares, L.A.$$uUniversidad de Zaragoza 000108322 700__ $$0(orcid)0000-0002-9181-9833$$aUtrilla, P.$$uUniversidad de Zaragoza 000108322 700__ $$aFábregas, R. 000108322 7102_ $$13006$$2430$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Geografía Física 000108322 7102_ $$13000$$2695$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Antigüed.$$cÁrea Prehistoria 000108322 773__ $$g593–594 (2020), 332-345$$pQuat. int.$$tQuaternary International$$x1040-6182 000108322 8564_ $$s757822$$uhttps://zaguan.unizar.es/record/108322/files/texto_completo.pdf$$yPostprint 000108322 8564_ $$s2524986$$uhttps://zaguan.unizar.es/record/108322/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint 000108322 909CO $$ooai:zaguan.unizar.es:108322$$particulos$$pdriver 000108322 951__ $$a2023-05-26-08:12:56 000108322 980__ $$aARTICLE