000124447 001__ 124447
000124447 005__ 20241125101150.0
000124447 0247_ $$2doi$$a10.1017/qua.2022.68
000124447 0248_ $$2sideral$$a132821
000124447 037__ $$aART-2023-132821
000124447 041__ $$aeng
000124447 100__ $$aTuru, V.
000124447 245__ $$aGlacial–interglacial cycles in the south-central and southeastern Pyrenees since ~180 ka (NE Spain–Andorra–S France)
000124447 260__ $$c2023
000124447 5060_ $$aAccess copy available to the general public$$fUnrestricted
000124447 5203_ $$aThis study uses luminescence and 14C accelerator mass spectrometry procedures to date relevant glaciofluvial and glacial deposits from the south-central and southeastern Pyrenees (Andorra–France–Spain). We distinguish two types of end-moraine complexes: (1) those in which at least a far-flung moraine exists beyond a frequently nested end-moraine complex (the most common) and (2) those in which a close-nested end moraine encompasses at least two glacial cycles. Both types formed within six distinctive glacial intervals: (1) A penultimate glacial cycle during Marine Oxygen Isotope Stage (MIS) 6 and older glaciofluvial terraces occurred beyond the range of the luminescence dating method. (2) An early glacial advance in MIS 5d (~97 −15/+19 ka) was followed by glacial retreat during MIS 5c (< 91 ± 9 ka). (3) The last maximum ice extent (LMIE) was in early MIS 4 (~74 ± 4.5 ka). (4) Unexpectedly, glaciers thinned during the second half of MIS 3 (~39 −6/+11 ka). (5) During the MIS 3–2 transition, glaciers subsequently fluctuated behind the LMIE limits. (6) The global last glacial maximum (LGM) started as early as ~26.6 ± 0.365 ka b2k, and the corresponding end moraines were built behind the LMIE limits or merged with it, forming close-nested moraines.
000124447 536__ $$9info:eu-repo/grantAgreement/ES/AEI/PID2020-117685GB-I00$$9info:eu-repo/grantAgreement/ES/DGA/H14-23R
000124447 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000124447 590__ $$a1.7$$b2023
000124447 592__ $$a0.787$$b2023
000124447 591__ $$aGEOGRAPHY, PHYSICAL$$b38 / 65 = 0.585$$c2023$$dQ3$$eT2
000124447 593__ $$aArts and Humanities (miscellaneous)$$c2023$$dQ1
000124447 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b155 / 254 = 0.61$$c2023$$dQ3$$eT2
000124447 593__ $$aEarth-Surface Processes$$c2023$$dQ1
000124447 593__ $$aEarth and Planetary Sciences (miscellaneous)$$c2023$$dQ1
000124447 594__ $$a4.7$$b2023
000124447 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000124447 700__ $$0(orcid)0000-0003-4067-8222$$aPeña-Monné, J. L.$$uUniversidad de Zaragoza
000124447 700__ $$aCunha, P. P.
000124447 700__ $$aJalut, G.
000124447 700__ $$aBuylaert, J. P.
000124447 700__ $$aMurray, A. S.
000124447 700__ $$aBridgland, D.
000124447 700__ $$aFaurschou-Knudsen, M.
000124447 700__ $$aOliva, M.
000124447 700__ $$aCarrasco, R. M.
000124447 700__ $$aRos, X.
000124447 700__ $$aTuru-Font, L.
000124447 700__ $$aVentura Roca, J.
000124447 7102_ $$13006$$2430$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Geografía Física
000124447 773__ $$g113 (2023), [28 pp.]$$pQuat. res.$$tQuaternary Research (United States)$$x0033-5894
000124447 8564_ $$s4283903$$uhttps://zaguan.unizar.es/record/124447/files/texto_completo.pdf$$yVersión publicada
000124447 8564_ $$s2886207$$uhttps://zaguan.unizar.es/record/124447/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000124447 909CO $$ooai:zaguan.unizar.es:124447$$particulos$$pdriver
000124447 951__ $$a2024-11-22-12:06:14
000124447 980__ $$aARTICLE