Please use this identifier to cite or link to this item:
https://hdl.handle.net/10316/113324
DC Field | Value | Language |
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dc.contributor.author | Turu, Valenti | - |
dc.contributor.author | Peña-Monné, Jose Luís | - |
dc.contributor.author | Cunha, Pedro P. | - |
dc.contributor.author | Jalut, Guy | - |
dc.contributor.author | Buylaert, Jan-Pieter | - |
dc.contributor.author | Murray, Andrew S. | - |
dc.contributor.author | Bridgland, David R. | - |
dc.contributor.author | Faurschou-Knudsen, Mads | - |
dc.contributor.author | Oliva, Marc | - |
dc.contributor.author | Carrasco, Rosa M. | - |
dc.contributor.author | Ros, Xavier | - |
dc.contributor.author | Turu-Font, Laia | - |
dc.contributor.author | Ventura Roca, Josep | - |
dc.date.accessioned | 2024-02-15T11:01:12Z | - |
dc.date.available | 2024-02-15T11:01:12Z | - |
dc.date.issued | 2023 | - |
dc.identifier.issn | 0033-5894 | pt |
dc.identifier.issn | 1096-0287 | pt |
dc.identifier.uri | https://hdl.handle.net/10316/113324 | - |
dc.description.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. | pt |
dc.language.iso | eng | pt |
dc.publisher | Cambridge University Press | pt |
dc.relation | UID/MAR/04292/2020 | pt |
dc.relation | SFRH/BSAB/150395/2019 | pt |
dc.rights | openAccess | pt |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | pt |
dc.subject | End moraines | pt |
dc.subject | Penultimate glacial cycle | pt |
dc.subject | Last glacial cycle | pt |
dc.subject | SW Europe | pt |
dc.subject | Luminescence dating methods | pt |
dc.title | Glacial–interglacial cycles in the south-central and southeastern Pyrenees since ~180 ka (NE Spain–Andorra–S France) | pt |
dc.type | article | - |
degois.publication.firstPage | 1 | pt |
degois.publication.lastPage | 28 | pt |
degois.publication.title | Cambridge University Press | pt |
dc.peerreviewed | yes | pt |
dc.identifier.doi | 10.1017/qua.2022.68 | pt |
degois.publication.volume | 113 | pt |
dc.date.embargo | 2023-01-01 | * |
uc.date.periodoEmbargo | 0 | pt |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.fulltext | Com Texto completo | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
crisitem.author.researchunit | CNC - Center for Neuroscience and Cell Biology | - |
crisitem.author.orcid | 0000-0002-3814-6289 | - |
crisitem.author.orcid | 0000-0001-5559-1862 | - |
crisitem.project.grantno | MARE-Marine and Environmental Sciences Centre | - |
Appears in Collections: | FCTUC Ciências da Terra - Artigos em Revistas Internacionais I&D MARE - Artigos em Revistas Internacionais |
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File | Description | Size | Format | |
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Glacialinterglacial-cycles-in-the-southcentral-and-southeastern-Pyrenees-since-180-ka-NE-SpainAndorraS-FranceQuaternary-Research-United-States.pdf | 4.18 MB | Adobe PDF | View/Open |
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This item is licensed under a Creative Commons License