Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/120340
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Type: Journal article
Title: A multi-dating approach to age-modelling long continental records: The 135 ka El Cañizar de Villarquemado sequence (NE Spain)
Author: Valero-Garcés, B.
González-Sampériz, P.
Gil Romera, G.
Benito, B.
Moreno, A.
Oliva-Urcia, B.
Aranbarri, J.
García-Prieto, E.
Frugone, M.
Morellón, M.
Arnold, L.
Demuro, M.
Hardiman, M.
Blockley, P.
Lane, C.
Citation: Quaternary Geochronology, 2019; OnlinePubl
Publisher: Elsevier
Issue Date: 2019
ISSN: 1871-1014
Statement of
Responsibility: 
B.L. Valero-Garcés, P. González-Sampériz, G. Gil Romera, B.M. Benito, A. Moreno, B. Oliva-Urcia, J. Aranbarri, E. García-Prieto, M. Frugone, M. Morellón, L.J. Arnold, M. Demuro, M. Hardiman, S.P.E. Blockley, C.S. Lane
Abstract: We present the multidisciplinary dating approach - including radiocarbon, Uranium/Thorium series (U/Th), paleomagnetism, single-grain Optical Stimulated Luminescence (OSL), Infrared Stimulated Luminescence (IRSL) and tephrochronology - used for the development of an age model for the Cañizar de Villarquemado sequence (VIL) for the last ca. 135 ka. We describe the protocols used for each technique and discuss the positive and negative results, as well as their implications for interpreting the VIL sequence and for dating similar terrestrial records. In spite of the negative results of some techniques, particularly due to the absence of adequate sample material or inaccurate analytical precision, the multi-technique strategy employed here is essential to maximize the chances of obtaining robust age models in terrestrial sequences. The final Bayesian age model for VIL sequence includes 16 AMS 14C ages, 9 OSL ages and 5 previously published IRSL ages, and the accuracy and resolution of the model are improved by incorporating information related to changes in accumulation rate, as revealed by detailed sedimentological analyses. The main paleohydrological and vegetation changes in the sequence are coherent with global Marine Isotope Stage (MIS) 6 to 1 transitions since the penultimate Termination, although some regional idiosyncrasies are evident, such as higher moisture variability than expected, an abrupt inception of the last glacial cycle and a resilient response of vegetation in Mediterranean continental Iberia in both Terminations.
Rights: Crown Copyright © 2019 Published by Elsevier B.V. All rights reserved.
RMID: 0030124729
DOI: 10.1016/j.quageo.2019.101006
Grant ID: http://purl.org/au-research/grants/arc/FT130100195
http://purl.org/au-research/grants/arc/DE160100743
Appears in Collections:Geology & Geophysics publications

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