Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)

This is a study of an extremely good outcrop of 1745 varves in the Villarroya Pliocene Basin (Spain). We have used the periodogram approach for estimating power spectra and periodicities of about 1 2, 6-7 and 2-3 years have been obtained. The light layers of the varves record the run-off of gastropo...

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Main Authors: Muñoz Jiménez, Arsenio, Sánchez Valverde, B.
Format: Article in Journal/Newspaper
Language:Spanish
Published: Sociedad Geológica de España 2001
Subjects:
Online Access:http://hdl.handle.net/10272/9580
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spelling ftunivhuelva:oai:rabida.uhu.es:10272/9580 2023-05-15T17:33:40+02:00 Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja) Palaeoclimatic interpretation of pliocene varves of the Villarroya Basin (Cameros Range, La Rioja, Spain) Muñoz Jiménez, Arsenio Sánchez Valverde, B. 2001 http://hdl.handle.net/10272/9580 spa spa Sociedad Geológica de España http://hdl.handle.net/10272/9580 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ info:eu-repo/semantics/openAccess CC-BY-NC-ND Pliocene Varves Sunspot El Niño/Southern Oscillation (ENSO) North-Atlantic Oscillation (NAO) Quasi-biennial Oscillation (QBO) info:eu-repo/semantics/article 2001 ftunivhuelva 2021-08-11T19:38:47Z This is a study of an extremely good outcrop of 1745 varves in the Villarroya Pliocene Basin (Spain). We have used the periodogram approach for estimating power spectra and periodicities of about 1 2, 6-7 and 2-3 years have been obtained. The light layers of the varves record the run-off of gastropods, ostracods and charophytes from seasonal productivity cycle, and are generated during late summer and autumn. It seems clear that the climatic information provided by these cycles corresponds mainly to summer time, which would be translated into a variation of the light layer thickness due to a more or less, intense development of the flora and fauna, being thicker in years of higher temperatures and thinner in years of lower temperatures. Considering the results, we would suggest that the sedimentation of these materials in the Pliocene was driven by solar activity or/and ENSO, NAO, and QBO phenomena. Nowadays these phenomena produce rainfall and temperature changes with the cyclicities shown In this study and we think they could have operated in the same way in Pliocene times Article in Journal/Newspaper North Atlantic North Atlantic oscillation Universidad de Huelva: Arias Montano
institution Open Polar
collection Universidad de Huelva: Arias Montano
op_collection_id ftunivhuelva
language Spanish
topic Pliocene
Varves
Sunspot
El Niño/Southern Oscillation (ENSO)
North-Atlantic Oscillation (NAO)
Quasi-biennial Oscillation (QBO)
spellingShingle Pliocene
Varves
Sunspot
El Niño/Southern Oscillation (ENSO)
North-Atlantic Oscillation (NAO)
Quasi-biennial Oscillation (QBO)
Muñoz Jiménez, Arsenio
Sánchez Valverde, B.
Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)
topic_facet Pliocene
Varves
Sunspot
El Niño/Southern Oscillation (ENSO)
North-Atlantic Oscillation (NAO)
Quasi-biennial Oscillation (QBO)
description This is a study of an extremely good outcrop of 1745 varves in the Villarroya Pliocene Basin (Spain). We have used the periodogram approach for estimating power spectra and periodicities of about 1 2, 6-7 and 2-3 years have been obtained. The light layers of the varves record the run-off of gastropods, ostracods and charophytes from seasonal productivity cycle, and are generated during late summer and autumn. It seems clear that the climatic information provided by these cycles corresponds mainly to summer time, which would be translated into a variation of the light layer thickness due to a more or less, intense development of the flora and fauna, being thicker in years of higher temperatures and thinner in years of lower temperatures. Considering the results, we would suggest that the sedimentation of these materials in the Pliocene was driven by solar activity or/and ENSO, NAO, and QBO phenomena. Nowadays these phenomena produce rainfall and temperature changes with the cyclicities shown In this study and we think they could have operated in the same way in Pliocene times
format Article in Journal/Newspaper
author Muñoz Jiménez, Arsenio
Sánchez Valverde, B.
author_facet Muñoz Jiménez, Arsenio
Sánchez Valverde, B.
author_sort Muñoz Jiménez, Arsenio
title Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)
title_short Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)
title_full Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)
title_fullStr Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)
title_full_unstemmed Interpretación paleoclimàtica de las varvas pliocenas de la Cuenca de Villarroya (Sierra de Cameros, La Rioja)
title_sort interpretación paleoclimàtica de las varvas pliocenas de la cuenca de villarroya (sierra de cameros, la rioja)
publisher Sociedad Geológica de España
publishDate 2001
url http://hdl.handle.net/10272/9580
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation http://hdl.handle.net/10272/9580
op_rights Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY-NC-ND
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