Controles alogénicos sobre la ciclicidad en la sedimentación continental en la Cuenca de Guadix (Cordillera Bética, España) durante el Plioceno y Pleistoceno: estado del conocimiento

  1. César Viseras 1
  2. Sila Pla-Pueyo 2
  3. Jesús M. Soria 3
  4. Juan Fernández 1
  5. Fernando García-García 4
  6. Elizabeth Gierlowski-Kordesch 5
  7. Ian Candy 6
  8. Danielle Schreve 6
  1. 1 Universidad de Granada
    info

    Universidad de Granada

    Granada, España

    ROR https://ror.org/04njjy449

  2. 2 Heriot-Watt University
    info

    Heriot-Watt University

    Edimburgo, Reino Unido

    ROR https://ror.org/04mghma93

  3. 3 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

  4. 4 Universidad de Jaén
    info

    Universidad de Jaén

    Jaén, España

    ROR https://ror.org/0122p5f64

  5. 5 University of London
    info

    University of London

    Londres, Reino Unido

    ROR https://ror.org/04cw6st05

  6. 6 Ohio University
    info

    Ohio University

    Athens, Estados Unidos

    ROR https://ror.org/01jr3y717

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Journal:
Revista de la Sociedad Geológica de España

ISSN: 0214-2708

Year of publication: 2014

Volume: 27

Issue: 1

Pages: 223-238

Type: Article

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More publications in: Revista de la Sociedad Geológica de España

Abstract

The Guadix Basin (Betic Cordillera, S Spain) is the ideal scenario to study the auto- and allogenic processes controlling continental sedimentation in hydrologically closed-basins. The extension and the lateral and vertical continuity of the outcrops, together with abundant archaeological and palaeontological sites in the area, have allowed the interpretation of the evolution of the basin throughout the last 4 Ma and the factors controlling it. These studies become much more important due to their relation to the characterisation of palaeoenvironments inhabited by the first European hominins. In this work, we present a synthesis of the most significative stratigraphical, sedimentological, petrological and palaeoclimatic studies developed in the Guadix Basin in the last decade, and updated results regarding the allogenic factors that controlled the continental sedimentation in the basin.

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