Articles producció científica> Història i Història de l'Art

Late Pliocene vegetation and orbital-scale climate changes from the western Mediterranean area

  • Datos identificativos

    Identificador: PC:352
    Handle: https://hdl.handle.net/20.500.11797/PC352
    Autores:
    Jiménez-Moreno, G.Burjachs, F.Expósito, I.Oms, O.Carrancho, T.Villalaín, J.J.Agustí, J.Campeny, G.Gómez de Soler, B.van der Made, J.
    Resumen:
    10.1016/j.gloplacha.2013.05.012

  • Otros:

    Autor según el artículo: Jiménez-Moreno, G. Burjachs, F. Expósito, I. Oms, O. Carrancho, T. Villalaín, J.J. Agustí, J. Campeny, G. Gómez de Soler, B. van der Made, J.
    Versión del articulo depositado: info:eu-repo/semantics/acceptedVersion
    Departamento: Història i Història de l'Art
    URL Documento de licencia: https://repositori.urv.cat/ca/proteccio-de-dades/
    Resumen: The Late Pliocene is a very interesting period as climate deteriorated from a warm optimum at ca. 3.3¿3.0 Ma to a progressive climate cooling. Simultaneously, the Mediterranean area witnessed the establishment of the Mediterranean-type seasonal precipitation rhythm (summer drought). These important climate changes produced significant vegetation changes, such as the extinction of several thermophilous and hygrophilous plant taxa from the European latitudes. Besides these long-term trends, climate was also characterized by cyclical variability (i.e., orbital changes) that forced vegetation changes (forested vs. open vegetation). In the Mediterranean area, cyclical changes in the vegetation were mostly forced by precession. In this study we analyzed pollen from a Late Pliocene maar lake core from NE Spain. An increase in aridity is observed as well as cyclic variations throughout the studied sequence. Cyclicity was mostly forced by precession but also by obliquity and eccentricity. Precipitation seems to be the main factor controlling these cycles. These data allowed estimating a sedimentary rate of ca. 0.19 mm/yr and the time duration covered by the studied core, close to 200 ka. The combination of biostratigraphy, palaeomagnetism and cyclostratigraphy allowed for a very precise dating of the sediments between ca. 3.3 and 3.1 Ma. Climate and paleobiogeographical implications are discussed within the context of the Late Pliocene Northern Hemisphere glacial intensification.
    Entidad: Universitat Rovira i Virgili.
    Año de publicación de la revista: 2013
    Acceso a la licencia de uso: https://creativecommons.org/licenses/by/3.0/es/
    ISSN: 0921-8181
    Página inicial: 15
    Página final: 28
    Volumen de revista: 108