Valenti Turu
Glacial–interglacial cycles in the south-central and southeastern Pyrenees since ~180 ka (NE Spain–Andorra–S France)
Turu, Valenti; Peña-Monné, Jose Luís; Cunha, Pedro P.; Jalut, Guy; Buylaert, Jan-Pieter; Murray, Andrew S.; Bridgland, David; Faurschou-Knudsen, Mads; Oliva, Marc; Carrasco, Rosa M.; Ros, Xavier; Turu-Font, Laia; Ventura Roca, Josep
Authors
Jose Luís Peña-Monné
Pedro P. Cunha
Guy Jalut
Jan-Pieter Buylaert
Andrew S. Murray
Professor David Bridgland d.r.bridgland@durham.ac.uk
Professor
Mads Faurschou-Knudsen
Marc Oliva
Rosa M. Carrasco
Xavier Ros
Laia Turu-Font
Josep Ventura Roca
Abstract
This 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 closenested 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.
Citation
Turu, V., Peña-Monné, J. L., Cunha, P. P., Jalut, G., Buylaert, J.-P., Murray, A. S., Bridgland, D., Faurschou-Knudsen, M., Oliva, M., Carrasco, R. M., Ros, X., Turu-Font, L., & Ventura Roca, J. (2023). Glacial–interglacial cycles in the south-central and southeastern Pyrenees since ~180 ka (NE Spain–Andorra–S France). Quaternary Research, 113, 1-28. https://doi.org/10.1017/qua.2022.68
Journal Article Type | Article |
---|---|
Acceptance Date | Nov 17, 2022 |
Online Publication Date | Jan 26, 2022 |
Publication Date | 2023-05 |
Deposit Date | Mar 7, 2023 |
Publicly Available Date | Apr 24, 2023 |
Journal | Quaternary Research |
Print ISSN | 0033-5894 |
Electronic ISSN | 1096-0287 |
Publisher | Academic Press |
Peer Reviewed | Peer Reviewed |
Volume | 113 |
Pages | 1-28 |
DOI | https://doi.org/10.1017/qua.2022.68 |
Public URL | https://durham-repository.worktribe.com/output/1178735 |
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Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Copyright Statement
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence
(https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
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