000151044 001__ 151044
000151044 005__ 20251017144630.0
000151044 0247_ $$2doi$$a10.1016/j.gloplacha.2022.103813
000151044 0248_ $$2sideral$$a128735
000151044 037__ $$aART-2022-128735
000151044 041__ $$aeng
000151044 100__ $$aBenito-Calvo, A.
000151044 245__ $$aTowards the steady state? A long-term river incision deceleration pattern during Pleistocene entrenchment (Upper Ebro River, Northern Spain)
000151044 260__ $$c2022
000151044 5060_ $$aAccess copy available to the general public$$fUnrestricted
000151044 5203_ $$aPleistocene fluvial incision acceleration resulting in narrow and deeply entrenched valleys has been widely described and is generally attributed to uplift rate increase or greater climatic severity. In this paper, the long-term downcutting pattern of the Upper Ebro River and driving mechanisms are assessed, and we reconstruct the valley incision recorded by an outstanding sequence of 22 river terraces. Dating of 8 fluvial levels by means of the ESR, TCN, and OSL techniques, spanning the last 1.2 Ma, reveals a long-term incision deceleration pattern. The estimated age-incision model indicates a decrease in the incision rates, showing a long-term deceleration during the final Early Pleistocene (from 0.42 to 0.18 m/ka), and a tendency towards a steady state or base level stabilization from the Middle Pleistocene (0.15–0.03 m/ka) to the Late Pleistocene (0.03 m/ka). This incision pattern does not support climate change as a long-term incision-acceleration driver by itself, demonstrating the need for base level lowering effects to have operated. Upper Ebro deceleration incision is explained by the headward attenuation of the incision wave induced by the opening of the Ebro Cenozoic Basin in a geodynamic context characterized by an absence of significant uplift over the last million years. This trend could have changed the aggressor-victim roles of the rivers involved in fluvial captures at the drainage divide. The documented incision deceleration pattern differs from that reported for other valleys in the Iberian Peninsula, suggesting that the degree of maturity of the fluvial systems depends on their relative position with respect to the capture point, in addition to tectonic and lithostructural factors. In the Late Pleistocene-Holocene, a short-lived incision rate increase is recorded, corresponding to the last terrace dissection phase, during the transition from the last glacial MIS 2 to the interglacial MIS 1.
000151044 536__ $$9info:eu-repo/grantAgreement/ES/MICINN/CGL2017-85045-P$$9info:eu-repo/grantAgreement/ES/MINECO/PGC2018-093925-B-C31
000151044 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
000151044 590__ $$a3.9$$b2022
000151044 591__ $$aGEOGRAPHY, PHYSICAL$$b13 / 49 = 0.265$$c2022$$dQ2$$eT1
000151044 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b53 / 202 = 0.262$$c2022$$dQ2$$eT1
000151044 592__ $$a1.459$$b2022
000151044 593__ $$aOceanography$$c2022$$dQ1
000151044 593__ $$aGlobal and Planetary Change$$c2022$$dQ1
000151044 594__ $$a8.2$$b2022
000151044 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000151044 700__ $$aMoreno, D.
000151044 700__ $$aFujioka, T.
000151044 700__ $$aLópez, G. I.
000151044 700__ $$aMartín-González, F.
000151044 700__ $$aMartínez-Fernández, A.
000151044 700__ $$aHernando-Alonso, I.
000151044 700__ $$aKarampaglidis, T.
000151044 700__ $$aBermúdez de Castro, J. M.
000151044 700__ $$0(orcid)0000-0002-5407-940X$$aGutiérrez, F.$$uUniversidad de Zaragoza
000151044 7102_ $$12000$$2427$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Externa
000151044 773__ $$g213 (2022), 103813 [18 pp.]$$pGlob. planet. change$$tGLOBAL AND PLANETARY CHANGE$$x0921-8181
000151044 8564_ $$s15319867$$uhttps://zaguan.unizar.es/record/151044/files/texto_completo.pdf$$yVersión publicada
000151044 8564_ $$s2489271$$uhttps://zaguan.unizar.es/record/151044/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000151044 909CO $$ooai:zaguan.unizar.es:151044$$particulos$$pdriver
000151044 951__ $$a2025-10-17-14:26:06
000151044 980__ $$aARTICLE