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El registro de la laguna de Taravilla (Alto Tajo, Sistema Ibérico) como sensor de cambios paleohidrológicos y paleoambientales

AuthorsValero-Garcés, Blas L. CSIC ORCID ; Navas Izquierdo, Ana CSIC ORCID ; Mata, M. Pilar; Machín Gayarre, Javier CSIC; Delgado Huertas, Antonio CSIC ORCID ; González-Sampériz, Penélope CSIC ORCID ; Schwalb, Antje; Moreno Caballud, Ana CSIC ORCID ; Edwards, R. Lawrence; González Barrios, A.
Keywordslake records
Iberian Range
Little Ice Age
Medieval Warm Period
Issue DateJul-2004
PublisherSociedad Geológica de España
CitationVI Congreso Geológico de España - Session: "“Registros de cambios climáticos durante el Cuaternario en la Península Ibérica”, coordinated by B. Valero-Garcés y F. Martínez-Ruíz" (Zaragoza, Spain. 11-17 July, 2004)
Abstract[EN] Lacustrine and travertine records from Laguna de Taravilla (Iberian Range, Guadalajara province, Spain, 40° 39’ N, 1° 59’ W, 1100 m have been analysed using sedimentological, mineralogical, geochemical and palynological techniques. A preliminary chronological framework is based on U/Th, 14C AMS, 210Pb and 137Cs dates. Phases of increased travertine growth occurred during the GlacialInterglacial transitions from isotope stage 6 to 5 and 2 to 1. Short lacustrine cores indicate a lake level and surface area increase after the XVth century, that can be correlated with the end of the Medieval Warm Period. Sandy facies related to flood events are more frequent during the interval ascribed to the Little Ice Age. The growth of littoral vegetation at the mouth of the inlet could have prevented more sandy sediments to reach the center of the lake during the last century.
Description9 Pag., 2 Fig., 1 Tabl.
Appears in Collections:(EEAD) Comunicaciones congresos

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