Reconstrucción paleoambiental del último ciclo glacial-interglacial en la Iberia continentalla secuencia del Cañizar de Villarquemado (Teruel)

  1. González Sampériz, Penélope 3
  2. García-Prieto, E. 3
  3. Aranbarri Erkiaga, Josu 3
  4. Valero Garcés, Blas Lorenzo 3
  5. Moreno, A. 3
  6. Gil Romera, Graciela 3
  7. Sevilla Callejo, Miguel 3
  8. Santos, L. 4
  9. Morellón, Mario 5
  10. Mata Campo, María Pilar 6
  11. Andrade Olalla, Antonia 1
  12. Carrión García, José Sebastián 2
  1. 1 Universidad de Alcalá
    info

    Universidad de Alcalá

    Alcalá de Henares, España

    ROR https://ror.org/04pmn0e78

  2. 2 Universidad de Murcia
    info

    Universidad de Murcia

    Murcia, España

    ROR https://ror.org/03p3aeb86

  3. 3 Instituto Pirenaico de Ecología
    info

    Instituto Pirenaico de Ecología

    Zaragoza, España

    ROR https://ror.org/039ssy097

  4. 4 Universidade da Coruña
    info

    Universidade da Coruña

    La Coruña, España

    ROR https://ror.org/01qckj285

  5. 5 Swiss Federal Laboratories for Materials Science and Technology
    info

    Swiss Federal Laboratories for Materials Science and Technology

    Dübendorf, Suiza

    ROR https://ror.org/02x681a42

  6. 6 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

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Revista:
Cuadernos de investigación geográfica: Geographical Research Letters

ISSN: 0211-6820,  1697-9540

Año de publicación: 2013

Volumen: 39

Número: 1

Páginas: 49-76

Tipo: Artículo

DOI: 10.18172/CIG.1999 DIALNET GOOGLE SCHOLAR lock_openDialnet editor

Otras publicaciones en: Cuadernos de investigación geográfica: Geographical Research Letters

Resumen

La secuencia de El Cañizar de Villarquemado (NE Península Ibérica) constituye un registro excepcional que cubre los últimos ca. 130 000 años de historia ambiental. Los análisis multidisciplinares que se han realizado hasta el momento incluyen un análisis palinológico preliminar y otros indicadores sedimentológicos, como susceptibilidad magnética, análisis geoquímicos de fluorescencia de rayos X (XRF), mineralogía y contenido en carbono orgánico e inorgánico (TOC/TIC). El modelo cronológico se ha realizado combinando dataciones AMS 14C en los 20 m superiores de sedimento y OSL (Luminiscencia Óptica Estimulada) en los 54 m restantes. La secuencia sedimentaria está esencialmente formada por la alternancia de fases con mayor desarrollo de humedales y turberas, con otras de depósitos distales de abanicos aluviales y episodios de lago carbonatado. Los resultados obtenidos hasta el momento confirman que el registro del Cañizar de Villarquemado responde a unas condiciones relativamente húmedas durante un probable MIS6-MIS5, con variaciones en la vegetación regional (esencialmente dominada por Juniperus) que aparecen siempre muy determinadas por la continentalidad de la zona, y que resultan atípicas para lo esperable durante un episodio interglacial como el Eemiense. De todos modos, los márgenes de error adscritos al modelo de edad impiden ciertas precisiones y aseveraciones al respecto. Durante el MIS3 se registra el periodo más árido de toda la secuencia, como confirman los resultados sedimentológicos y los polínicos de algunos intervalos ya disponibles. Sin embargo el MIS2 presenta una gran variabilidad tanto a nivel local, como indican las distintas asociaciones de facies y la vegetación acuática, como a nivel regional, como se deduce de la cubierta vegetal general. El comienzo del Holoceno se registra de manera muy abrupta en cuanto a cambios paleohidrológicos, pero mostrando de nuevo cierta resiliencia de la vegetación, dominada esta vez por pinos y no por Juniperus como en la base de la secuencia, y muy adaptada a las condiciones de extrema continentalidad. El posterior desarrollo de quercíneas junto con la presencia de pinos, apunta situaciones climáticas muy diferentes entre un posible MIS5 y el MIS1.

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Fuente de los datos: Dialnet