000079151 001__ 79151
000079151 005__ 20200117221629.0
000079151 0247_ $$2doi$$a10.1016/j.quaint.2017.09.011
000079151 0248_ $$2sideral$$a107074
000079151 037__ $$aART-2018-107074
000079151 041__ $$aeng
000079151 100__ $$0(orcid)0000-0001-5379-5087$$aSauqué, V.
000079151 245__ $$aLos Batanes: A trap for the Pyrenean wild goat during the Late Pleistocene (Spain)
000079151 260__ $$c2018
000079151 5060_ $$aAccess copy available to the general public$$fUnrestricted
000079151 5203_ $$aLos Batanes cave (1025 m.a.s.l.) is a karstic system formed by pressure ducts, near the locality of Biescas in the Upper Gallego Valley (Huesca, Spain). Many fossil remains were retrieved from the cave sediments. The minimum sediment calendar age was determined to be 12.770 ± 60 BP. This date indicates that the deposit was formed before the Late Pleistocene-Early Holocene transition at the Pyrenees. Here we analyze the faunal assemblage of the site that is only conformed by remains of Pyrenean wild goat (Capra pyrenaica pyrenaica), which is a recently extinct subspecies of Iberian wild goat (C. pyrenaica). In the site, 1079 remains of Iberian wild goat have been recovered being one of the most numerous both in minimum number of individuals (MNI) and number of identified specimens (NISP) recovered until now in a natural trap in the Spanish Pyrenees. The population of Los Batanes shows a wide range of ages between juvenile and senile individuals and the MNI estimated from the number of right metatarsus is nine. The taphonomic features indicate that the cave acted as a trap for the goats which inhabited the vicinity of the cave. These goats probably stumbled and fell to the bottom of the pit and they could not get out, dying inside. Due to the origin of the accumulation numerous complete bones have been recovered. These fossil allow us to perform a biometric analysis that indicates that population of Los Batanes is in the range size of other goats from Late Pleistocene of Iberian Peninsula.
000079151 536__ $$9info:eu-repo/grantAgreement/ES/DGA/FSE$$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2012-38434-C03-01$$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2015-65387-C3-2-01
000079151 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000079151 590__ $$a1.952$$b2018
000079151 591__ $$aGEOGRAPHY, PHYSICAL$$b30 / 50 = 0.6$$c2018$$dQ3$$eT2
000079151 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b104 / 195 = 0.533$$c2018$$dQ3$$eT2
000079151 592__ $$a1.159$$b2018
000079151 593__ $$aEarth-Surface Processes$$c2018$$dQ1
000079151 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000079151 700__ $$aGarcía-González, R.
000079151 700__ $$aRabal-Garcés, R.
000079151 700__ $$aGalán, J.
000079151 700__ $$0(orcid)0000-0002-2882-6061$$aNúñez-Lahuerta, C.$$uUniversidad de Zaragoza
000079151 700__ $$aGisbert, M.
000079151 700__ $$0(orcid)0000-0001-5125-9651$$aCuenca-Bescós, G.$$uUniversidad de Zaragoza
000079151 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000079151 773__ $$g481 (2018), 75-90$$pQuat. int.$$tQuaternary International$$x1040-6182
000079151 8564_ $$s1079809$$uhttps://zaguan.unizar.es/record/79151/files/texto_completo.pdf$$yPostprint
000079151 8564_ $$s108226$$uhttps://zaguan.unizar.es/record/79151/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000079151 909CO $$ooai:zaguan.unizar.es:79151$$particulos$$pdriver
000079151 951__ $$a2020-01-17-21:58:50
000079151 980__ $$aARTICLE