000108322 001__ 108322
000108322 005__ 20240123091309.0
000108322 0247_ $$2doi$$a10.1016/j.quaint.2020.10.029
000108322 0248_ $$2sideral$$a121217
000108322 037__ $$aART-2021-121217
000108322 041__ $$aeng
000108322 100__ $$0(orcid)0000-0003-4280-3971$$aAlcolea, M.
000108322 245__ $$aDendro-anthracological tools applied to Scots type pine forests exploitation as fuel during the Mesolithic-Neolithic transition in the southern central pre-Pyrenees (Spain)
000108322 260__ $$c2021
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/MINECO/HAR2017-85023-P
000108322 540__ $$9info:eu-repo/semantics/closedAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000108322 590__ $$a2.454$$b2021
000108322 592__ $$a0.872$$b2021
000108322 593__ $$aEarth-Surface Processes$$c2021$$dQ1
000108322 594__ $$a5.5$$b2021
000108322 591__ $$aGEOGRAPHY, PHYSICAL$$b34 / 50 = 0.68$$c2021$$dQ3$$eT3
000108322 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b124 / 202 = 0.614$$c2021$$dQ3$$eT2
000108322 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
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__ $$g593–594 (2021), 332-345$$pQuat. int.$$tQuaternary International$$x1040-6182
000108322 8564_ $$s757817$$uhttps://zaguan.unizar.es/record/108322/files/texto_completo.pdf$$yVersión publicada
000108322 8564_ $$s2525153$$uhttps://zaguan.unizar.es/record/108322/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000108322 909CO $$ooai:zaguan.unizar.es:108322$$particulos$$pdriver
000108322 951__ $$a2024-01-23-09:07:32
000108322 980__ $$aARTICLE