Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)

Environmental magnetic proxies were analyzed in a relatively monotonous, ~25.3m thick alluvial sedimentary sequence drilled in the Añavieja Basin (NE Spain). Results from the core AÑ2 suggest that the concentrationdependent magnetic parameters mainly reflect variations in the content of detrital mag...

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Main Authors: Oliva-Urcia, Belén, Muñoz Jiménez, Arsenio, Larrasoaña Gorosquieta, Juan Cruz, Luzón Aguado, María Aránzazu, Pérez García, Antonio, González Rodríguez, Ángel, Jiang, Z., Qingsong, Liu, Román Berdiel, Teresa
Format: Other/Unknown Material
Language:English
Published: Universidad de Barcelona 2020
Subjects:
Online Access:https://hdl.handle.net/20.500.12468/377
https://doi.org/10.1344/GeologicaActa2016.14.2.4
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record_format openpolar
spelling ftcsic:oai:digital.csic.es:20.500.12468/377 2023-05-15T17:23:40+02:00 Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain) Oliva-Urcia, Belén Muñoz Jiménez, Arsenio Larrasoaña Gorosquieta, Juan Cruz Luzón Aguado, María Aránzazu Pérez García, Antonio González Rodríguez, Ángel Jiang, Z. Qingsong, Liu Román Berdiel, Teresa 2020-09-24T09:09:58Z https://hdl.handle.net/20.500.12468/377 https://doi.org/10.1344/GeologicaActa2016.14.2.4 en eng Universidad de Barcelona #PLACEHOLDER_PARENT_METADATA_VALUE# CGL2009-09165/BTE CGL2009-08969 FEDER UZ 2008-CIE-12 https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2016.14.2.4 Geológica Acta, v. 14, n.2, 139-154 1696-5728 http://hdl.handle.net/20.500.12468/377 https://doi.org/10.1344/GeologicaActa2016.14.2.4 open Añavieja Basin aluvial sequence magnetite environmental magnetism vegetation cover temperature NGRIP curve Postprint 2020 ftcsic https://doi.org/20.500.12468/377 https://doi.org/10.1344/GeologicaActa2016.14.2.4 2022-08-23T23:39:34Z Environmental magnetic proxies were analyzed in a relatively monotonous, ~25.3m thick alluvial sedimentary sequence drilled in the Añavieja Basin (NE Spain). Results from the core AÑ2 suggest that the concentrationdependent magnetic parameters mainly reflect variations in the content of detrital magnetite, sourced in the catchment rocks and soils of the basin, via changes in the dynamics of alluvial fans due to temperature changes in the northern hemisphere during the Late Pleistocene. The correspondence between the magnetic proxies and the temperature variations in the North Atlantic region (NGRIP curve) indicates that higher (lower) concentrations and finer (coarser) magnetite grains coincide with warm (cold) periods. We propose that during cold periods, a sparser vegetation cover favored the incoming of higher energy runoff bearing coarser sediments to the basin that are relatively impoverished in magnetite. In contrast, during warm periods, the wider distribution of the vegetation cover associated with the lower runoff energy lead to finer, magnetite-richer sediment input to the basin. Maghemite, presumably of pedogenic origin, appears to be present also in the studied alluvial sediments. Further studies are necessary to unravel its palaeoclimatic significance. Instituto Pirenaíco de Ecología, España Departamento de Geología y Geoquímica, Universidad Autónoma de Madrid, España Departamento de Ciencias de la Tierra, Universidad de Zaragoza, España Instituto Geológico y Minero de España, España Institut de Ciéncies de la Terra Jaume Almera, España Paleomagnetism and Geochronology Laboratory, Institute of Geology and Geophysics, Chinesse Academy of Sciences, China Function Laboratory for Marine Geology, National Oceanography Laboratory, China Programa Junta para la Ampliación de Estudios, Consejo Superior de Investigaciones Científicas, España Ministerio de Ciencia e Innovación, España Gobierno de Aragón, España Fondo Social Europeo, Unión Europea Other/Unknown Material NGRIP North Atlantic Digital.CSIC (Spanish National Research Council) Jaume ENVELOPE(-63.750,-63.750,-65.483,-65.483)
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Añavieja Basin
aluvial sequence
magnetite
environmental magnetism
vegetation cover
temperature
NGRIP curve
spellingShingle Añavieja Basin
aluvial sequence
magnetite
environmental magnetism
vegetation cover
temperature
NGRIP curve
Oliva-Urcia, Belén
Muñoz Jiménez, Arsenio
Larrasoaña Gorosquieta, Juan Cruz
Luzón Aguado, María Aránzazu
Pérez García, Antonio
González Rodríguez, Ángel
Jiang, Z.
Qingsong, Liu
Román Berdiel, Teresa
Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)
topic_facet Añavieja Basin
aluvial sequence
magnetite
environmental magnetism
vegetation cover
temperature
NGRIP curve
description Environmental magnetic proxies were analyzed in a relatively monotonous, ~25.3m thick alluvial sedimentary sequence drilled in the Añavieja Basin (NE Spain). Results from the core AÑ2 suggest that the concentrationdependent magnetic parameters mainly reflect variations in the content of detrital magnetite, sourced in the catchment rocks and soils of the basin, via changes in the dynamics of alluvial fans due to temperature changes in the northern hemisphere during the Late Pleistocene. The correspondence between the magnetic proxies and the temperature variations in the North Atlantic region (NGRIP curve) indicates that higher (lower) concentrations and finer (coarser) magnetite grains coincide with warm (cold) periods. We propose that during cold periods, a sparser vegetation cover favored the incoming of higher energy runoff bearing coarser sediments to the basin that are relatively impoverished in magnetite. In contrast, during warm periods, the wider distribution of the vegetation cover associated with the lower runoff energy lead to finer, magnetite-richer sediment input to the basin. Maghemite, presumably of pedogenic origin, appears to be present also in the studied alluvial sediments. Further studies are necessary to unravel its palaeoclimatic significance. Instituto Pirenaíco de Ecología, España Departamento de Geología y Geoquímica, Universidad Autónoma de Madrid, España Departamento de Ciencias de la Tierra, Universidad de Zaragoza, España Instituto Geológico y Minero de España, España Institut de Ciéncies de la Terra Jaume Almera, España Paleomagnetism and Geochronology Laboratory, Institute of Geology and Geophysics, Chinesse Academy of Sciences, China Function Laboratory for Marine Geology, National Oceanography Laboratory, China Programa Junta para la Ampliación de Estudios, Consejo Superior de Investigaciones Científicas, España Ministerio de Ciencia e Innovación, España Gobierno de Aragón, España Fondo Social Europeo, Unión Europea
format Other/Unknown Material
author Oliva-Urcia, Belén
Muñoz Jiménez, Arsenio
Larrasoaña Gorosquieta, Juan Cruz
Luzón Aguado, María Aránzazu
Pérez García, Antonio
González Rodríguez, Ángel
Jiang, Z.
Qingsong, Liu
Román Berdiel, Teresa
author_facet Oliva-Urcia, Belén
Muñoz Jiménez, Arsenio
Larrasoaña Gorosquieta, Juan Cruz
Luzón Aguado, María Aránzazu
Pérez García, Antonio
González Rodríguez, Ángel
Jiang, Z.
Qingsong, Liu
Román Berdiel, Teresa
author_sort Oliva-Urcia, Belén
title Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)
title_short Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)
title_full Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)
title_fullStr Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)
title_full_unstemmed Response of alluvial systems to Late Pleistocene climate changes recorded by environmental magnetism in the Añavieja Basin (Iberian Range, NE Spain)
title_sort response of alluvial systems to late pleistocene climate changes recorded by environmental magnetism in the añavieja basin (iberian range, ne spain)
publisher Universidad de Barcelona
publishDate 2020
url https://hdl.handle.net/20.500.12468/377
https://doi.org/10.1344/GeologicaActa2016.14.2.4
long_lat ENVELOPE(-63.750,-63.750,-65.483,-65.483)
geographic Jaume
geographic_facet Jaume
genre NGRIP
North Atlantic
genre_facet NGRIP
North Atlantic
op_relation #PLACEHOLDER_PARENT_METADATA_VALUE#
CGL2009-09165/BTE
CGL2009-08969
FEDER UZ 2008-CIE-12
https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2016.14.2.4
Geológica Acta, v. 14, n.2, 139-154
1696-5728
http://hdl.handle.net/20.500.12468/377
https://doi.org/10.1344/GeologicaActa2016.14.2.4
op_rights open
op_doi https://doi.org/20.500.12468/377
https://doi.org/10.1344/GeologicaActa2016.14.2.4
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