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Age and significance of the Quaternary cemented deposits of the Duje Valley (Picos de Europa, Northern Spain)

Published online by Cambridge University Press:  20 January 2017

Elisa Villa ,
Heather Stoll ,
Pedro Farias ,
Luna Adrados ,
R. Lawrence Edwards  and
Hai Cheng
Elisa Villa*
Affiliation:
Departamento de Geología, Universidad de Oviedo, Oviedo, 33005, Spain
Heather Stoll
Affiliation:
Departamento de Geología, Universidad de Oviedo, Oviedo, 33005, Spain
Pedro Farias
Affiliation:
Departamento de Geología, Universidad de Oviedo, Oviedo, 33005, Spain
Luna Adrados
Affiliation:
Departamento de Geología, Universidad de Oviedo, Oviedo, 33005, Spain
R. Lawrence Edwards
Affiliation:
Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA
Hai Cheng
Affiliation:
Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA Institute of Global Environmental Change, Xian Jiaotong University, Xian 710049, China
*
*Corresponding author at: Universidad de Oviedo, Departamento de Geología, 33005 Oviedo, Spain. Fax: + 34 985103103. E-mail address:[email protected] (E. Villa).
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Abstract

Cemented calcareous breccias appear in the Picos de Europa (Cantabrian Mountains, Spain) resting on glacially abraded surfaces and covered by moraines. U/Th dating of the calcite coating the clasts was successful in two samples, the oldest one indicating that the breccias accumulated during or prior to Marine Isotope Stage (MIS) 11, and the youngest indicating later cementation during MIS 8. The former introduces a limit for the age of the glaciation preceding the breccias, which cannot correspond to an event younger than MIS 12. This is the oldest absolute age so far obtained for intercalated glacial/interglacial deposits of the Iberian Peninsula.

Keywords

Picos de EuropaQuaternary cemented depositsU/Th datingMIS 11MIS 12Mid-Pleistocene glaciation
Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 1 , January 2013 , pp. 1 - 5
Copyright
University of Washington

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References

Castañón, J.C., and Frochoso, M. Hugo Obermaier y el glaciarismo pleistoceno. Moure, A. El hombre fósil 80 años después. (1996). Universidad de Cantabria, Santander. 153–176.Google Scholar
Flor, G., and Baylon-Misioné, J.I. El glaciarismo cuaternario de los Puertos de Áliva (Macizo Oriental de los Picos de Europa, Occidente de Cantabria). Cuaternario y Geomorfología 3, (1989). 27–34.Google Scholar
Gale, S.J., and Hoare, P.G. The glacial history of the northwest Picos de Europa of northern Spain. Zeitschrift für Geomorphologie 41, (1997). 81–96.Google Scholar
Hughes, P.D., Woodward, J.C., Gibbard, P.L., Macklin, M.G., Gilmour, M.A., and Smith, G.R. The glacial history of the Pindus Mountains, Greece. Journal of Geology 114, (2006). 413–434.CrossRefGoogle Scholar
Hughes, P.D., Woodward, J.C., van Calsteren, P.C., Thomas, L.E., and Adamson, K.R. Pleistocene ice caps on the coastal mountains of the Adriatic Sea. Quaternary Science Reviews 29, (2010). 3690–3708.Google Scholar
Hughes, P.D., Woodward, J.C., van Calsteren, P.C., and Thomas, L.E. The glacial history of the Dinaric Alps, Montenegro. Quaternary Science Reviews 30, (2011). 3393–3412.CrossRefGoogle Scholar
Lang, N., and Wolff, E.W. Interglacial and glacial variability from the last 800 ka in marine, ice and terrestrial archives. Climate of the Past 7, (2011). 361–380.Google Scholar
Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A.C.M., and Levrard, B. A long-term numerical solution for the insolation quantities of the Earth. Astronomy and Astrophysics 428, (2004). 261–285.CrossRefGoogle Scholar
Moreno, A., Valero-Garcés, B.L., Jiménez-Sánchez, M., Domínguez-Cuesta, M.J., Mata, M.P., Navas, A., González-Sampériz, P., Stoll, H., Farias, P., Morellón, M., Corella, J.P., and Rico, M. The last deglaciation in the Picos de Europa National Park (Cantabrian Mountains, northern Spain). Journal of Quaternary Science 25, (2010). 1076–1091.CrossRefGoogle Scholar
Obermaier, H. Estudio de los glaciares de los Picos de Europa. Trabajos del Museo Nacional de Ciencias Naturales. Serie Geológica 9, (1914). (41 pp.)Google Scholar
Ogando, E. Picos de Europa. Exploraciones Verticales. Boletín Cántabro de Espeleología 16, (2007). 43–51.Google Scholar
Penck, A. Die Picos de Europa und das Kantabrische Gebirge. Geographische Zeitschrift Leipzig (1897). 278–281.Google Scholar
Prokopenko, A.A., Bezrukova, E.V., Khursevich, G.K., Solotchina, E.P., Kuzmin, M.I., and Tarasov, P.E. Climate in continental interior Asia during the longest interglacial of the past 500,000 yr: the new MIS 11 records from Lake Baikal, SE Siberia. Climate of the Past 6, (2010). 31–48.Google Scholar
Serrano, E., González-Trueba, J.J., and González-García, M. Mountain glaciation and paleoclimate reconstruction in the Picos de Europa (Iberian Peninsula, SW Europe). Quaternary Research 78, (2012). 303–314.CrossRefGoogle Scholar
Smart, P.L. Origin and development of gacio-karst closed depressions in the Picos de Europa, Spain. Zeitschrift für Geomorphologie 30, (1986). 423–443.Google Scholar
Vaks, A., Gutareva, O.S., Breitenbach, S.F.M., Erdenedalai, A., Osinzev, A.V., and Henderson, G.M. A history of permafrost in Siberia and aridity in Mongolia during the last 500 ka. (2011). 126 (Abstract KR6) Google Scholar
Vidal Romaní, J.R., Fernández Mosquera, D., Marti, K., and De Brum Ferreira, A. Nuevos datos para la cronología glaciar pleistocena en el NW de la Península Ibérica. Cuadernos del Laboratorio Xeolóxico de Laxe 24, (1999). 7–29.Google Scholar
Voelker, A.H.L., Rodrigues, T., Billups, K., Oppo, D., McManus, J., Stein, R., Hefter, J., and Grimalt, J.O. Variations in mid-latitude north Atlantic surface water properties during the mid-Brunhes (MIS 9–14) and their implications for the thermohaline circulation. Climate of the Past 6, (2010). 531–552.CrossRefGoogle Scholar