El registro holoceno del estuario del Guadalquivir en el área de Sevillaaproximación geoarqueológica

  1. F. Borja 1
  2. M. Hunt 2
  3. J.L. Ubera 3
  4. C. Zazo 4
  5. C.J.Dabrio 5
  6. J.L. Goy 6
  7. M.A. Barral 1
  8. Y. Llergo López 3
  9. César Borja 2
  1. 1 Universidad de Huelva
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    Universidad de Huelva

    Huelva, España

    ROR https://ror.org/03a1kt624

    Geographic location of the organization Universidad de Huelva
  2. 2 Universidad de Sevilla
    info
    Universidad de Sevilla

    Sevilla, España

    ROR https://ror.org/03yxnpp24

    Geographic location of the organization Universidad de Sevilla
  3. 3 Universidad de Córdoba
    info
    Universidad de Córdoba

    Córdoba, España

    ROR https://ror.org/05yc77b46

    Geographic location of the organization Universidad de Córdoba
  4. 4 Consejo Superior de Investigaciones Científicas
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    Consejo Superior de Investigaciones Científicas

    Madrid, España

    ROR https://ror.org/02gfc7t72

    Geographic location of the organization Consejo Superior de Investigaciones Científicas
  5. 5 Universidad Complutense de Madrid
    info
    Universidad Complutense de Madrid

    Madrid, España

    ROR https://ror.org/02p0gd045

    Geographic location of the organization Universidad Complutense de Madrid
  6. 6 Universidad de Salamanca
    info
    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

    Geographic location of the organization Universidad de Salamanca
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Book:
Contribuciones al estudio del periodo cuaternario
  1. Lario Gómez, Javier (coord.)
  2. Silva, Pablo G. (coord.)

Publisher: Escuela Técnica Superior de Ingenieros Industriales de Madrid ; Universidad Politécnica de Madrid

ISBN: 978-84-7484-201-2

Year of publication: 2007

Pages: 101-102

Type: Book chapter

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Abstract

We study the sedimentary internal area filling of Guadalquivir estuary, near Seville. The sediment samples come from two cores drilled in San Fernando Street, located to the south of the historical town. They are separated about 200 m and they have deepened something more than 18 m, reaching the geologic formation of Margas Azules (late Miocene). Methodologically, we used sedimentology, palynology (twenty-two samples distributed between 2 m and 12.35 m of depth) and radiocarbon data (six samples spread between 4 m and 12 m of depth), as well as the analysis of the archaeological record. All it allows to establish a palaeogeographic sequence characterised by three great phases: marine transgression episode (Lower-middle Holocene vertical aggradation); alluvial episode with final progressive human influence (Middle-recent Holocene lateral progradation); and urban occupation episode with cyclic alluvial influence (Recent Holocene).

Data source: Dialnet