000129689 001__ 129689
000129689 005__ 20240319080953.0
000129689 0247_ $$2doi$$a10.1016/j.gloplacha.2022.103788
000129689 0248_ $$2sideral$$a128449
000129689 037__ $$aART-2022-128449
000129689 041__ $$aeng
000129689 100__ $$aEzquerro, Lope
000129689 245__ $$aLate Neogene to Early Quaternary climate evolution in southwestern Europe from a continental perspective
000129689 260__ $$c2022
000129689 5060_ $$aAccess copy available to the general public$$fUnrestricted
000129689 5203_ $$aPaleoclimate reconstructions are mostly based on continuous oceanic records, but continental records, controlled by global and regional conditions, are paramount in identifying long- and short-term climatic variability between regions and investigating forcing mechanisms. Here we present a high-resolution lacustrine log from a western Mediterranean intramountain basin; it is based on calcite oxygen isotope composition (d18Oc) and records detailed paleoclimatic information from the Late Miocene to the Early Pleistocene (9.8–1.8 Ma). Evidence is found for orbital forcing in the regional paleoclimate, with minimum and maximum eccentricity related to drier and wetter conditions respectively. Superimposed onto this variability, the long-term trend reflects the influence of global paleogeographic and climate change. Variations inferred in precipitation-evaporation (P–E) are related to SST in the North Atlantic, which evidences a connection between marine dynamics and continental climate in areas far from the coast in southwestern Europe and a relation between dry periods and high SST inland. It is proposed that the regional climate was impacted by the effect of the closure of the Central Atlantic Seaway and changes in the Atlantic Meridional Overturning Circulation (AMOC). Warmer/drier conditions were related to a more permanent, stable, high-pressure centre over the mid-Atlantic in a situation of strengthened AMOC, which would have blocked westerly winds, increasing aridity in southwestern Europe. The inferred warm/dry connection differs from other western Mediterranean records, supporting previous interpretations of a regional climate gradient in western Europe. As occurs at present, isolation from the influence of the humidity of the Mediterranean Sea during warm periods as a result of'' to the local orography could well have been the cause of regional differences. © 2022 Elsevier B.V.
000129689 536__ $$9info:eu-repo/grantAgreement/ES/AEI/PID2019-108705GB-I00$$9info:eu-repo/grantAgreement/ES/DGA/E32-20R
000129689 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000129689 590__ $$a3.9$$b2022
000129689 591__ $$aGEOGRAPHY, PHYSICAL$$b13 / 49 = 0.265$$c2022$$dQ2$$eT1
000129689 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b53 / 202 = 0.262$$c2022$$dQ2$$eT1
000129689 592__ $$a1.459$$b2022
000129689 593__ $$aOceanography$$c2022$$dQ1
000129689 593__ $$aGlobal and Planetary Change$$c2022$$dQ1
000129689 594__ $$a8.2$$b2022
000129689 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000129689 700__ $$0(orcid)0000-0001-5700-6495$$aMuñoz, Arsenio$$uUniversidad de Zaragoza
000129689 700__ $$0(orcid)0000-0002-9130-117X$$aLiesa, Carlos L.$$uUniversidad de Zaragoza
000129689 700__ $$0(orcid)0000-0003-1412-5245$$aSimón, José L.$$uUniversidad de Zaragoza
000129689 700__ $$0(orcid)0000-0002-8929-9429$$aLuzón, Aránzazu$$uUniversidad de Zaragoza
000129689 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000129689 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000129689 773__ $$g211 (2022), 103788 [19 pp]$$pGlob. planet. change$$tGLOBAL AND PLANETARY CHANGE$$x0921-8181
000129689 8564_ $$s1119874$$uhttps://zaguan.unizar.es/record/129689/files/texto_completo.pdf$$yPostprint
000129689 8564_ $$s1956199$$uhttps://zaguan.unizar.es/record/129689/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000129689 909CO $$ooai:zaguan.unizar.es:129689$$particulos$$pdriver
000129689 951__ $$a2024-03-18-13:19:30
000129689 980__ $$aARTICLE