000118979 001__ 118979
000118979 005__ 20240319081013.0
000118979 0247_ $$2doi$$a10.1007/s12665-022-10547-x
000118979 0248_ $$2sideral$$a130165
000118979 037__ $$aART-2022-130165
000118979 041__ $$aeng
000118979 100__ $$0(orcid)0000-0003-4067-8222$$aPeña Monné, José Luis$$uUniversidad de Zaragoza
000118979 245__ $$aLate Quaternary palaeoenvironmental controls on concentric talus evolution in the Central Ebro Basin (NE Spain)
000118979 260__ $$c2022
000118979 5060_ $$aAccess copy available to the general public$$fUnrestricted
000118979 5203_ $$aThe polyphasic evolution of the testimonial buttes in the central area of the Ebro basin (Los Monegros) is analysed. This is a semiarid area that favours high erosion rates. An evolutionary model of the Jubierre hills is presented that shows the environmental cycles represented by aggradational and degradative processes on the slopes that resulted in the present arrangement of talus flatiron rings. In the four studied cases, talus relicts are composed of detritic material from a disappeared caprock pediment. Four slope stages (S4 to S1) that formed under stable climate conditions are identified. Older stages (S4 and S3) are estimated by comparison with other talus flatirons in the region. The S2 stage contains Bronze Age archaeological remains and the radiocarbon age obtained was 1608-1446 years cal BC (2 sigma), while S1 is younger. A palaeoenvironmental interpretation was made for these aggradational stages (S4 to S1). The active erosion of these hills led to a relief inversion, and talus flatirons remain as the only features revealing the presence of the relict hills and past human occupations.
000118979 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/HAR2014-59042-P$$9info:eu-repo/grantAgreement/ES/MINECO/HAR2015-65620-P
000118979 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000118979 590__ $$a2.8$$b2022
000118979 592__ $$a0.599$$b2022
000118979 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b95 / 202 = 0.47$$c2022$$dQ2$$eT2
000118979 593__ $$aSoil Science$$c2022$$dQ2
000118979 591__ $$aWATER RESOURCES$$b45 / 103 = 0.437$$c2022$$dQ2$$eT2
000118979 593__ $$aEarth-Surface Processes$$c2022$$dQ2
000118979 591__ $$aENVIRONMENTAL SCIENCES$$b162 / 275 = 0.589$$c2022$$dQ3$$eT2
000118979 593__ $$aGeology$$c2022$$dQ2
000118979 593__ $$aWater Science and Technology$$c2022$$dQ2
000118979 593__ $$aPollution$$c2022$$dQ2
000118979 593__ $$aEnvironmental Chemistry$$c2022$$dQ3
000118979 593__ $$aGlobal and Planetary Change$$c2022$$dQ3
000118979 594__ $$a5.2$$b2022
000118979 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000118979 700__ $$aSampietro Vattuone, María Marta
000118979 700__ $$0(orcid)0000-0002-4726-819X$$aPicazo Millán, Jesús, V.$$uUniversidad de Zaragoza
000118979 7102_ $$13006$$2430$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Geografía Física
000118979 7102_ $$13000$$2695$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Antigüed.$$cÁrea Prehistoria
000118979 773__ $$g81, 422 (2022), 19$$pEnviron. earth sci.$$tEnvironmental Earth Sciences$$x1866-6280
000118979 8564_ $$s15498261$$uhttps://zaguan.unizar.es/record/118979/files/texto_completo.pdf$$yVersión publicada
000118979 8564_ $$s2525431$$uhttps://zaguan.unizar.es/record/118979/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000118979 909CO $$ooai:zaguan.unizar.es:118979$$particulos$$pdriver
000118979 951__ $$a2024-03-18-15:18:04
000118979 980__ $$aARTICLE