Holocene palaeoenvironmental evolution of Saltés Island, Tinto and Odiel estuary, SW Spain, during the Roman period, 1st century BC–5th century AD

  1. María L. González-Regalado 1
  2. Paula Gómez 1
  3. Francisco Ruiz 1
  4. Luis M. Cáceres 1
  5. María J. Clemente 1
  6. Joaquín Rodríguez-Vidal 1
  7. Antonio Toscano 1
  8. Guadalupe Monge 2
  9. Manuel Abad 1
  10. Tatiana Izquierdo 1
  11. Antonio M. Monge Soares 3
  12. Juan M. Campos 1
  13. Javier Bermejo 1
  14. Aranzazu Martínez-Aguirre 2
  15. Gloria I. López 4
  1. 1 Universidad de Huelva
    info

    Universidad de Huelva

    Huelva, España

    ROR https://ror.org/03a1kt624

  2. 2 Universidad de Sevilla
    info

    Universidad de Sevilla

    Sevilla, España

    ROR https://ror.org/03yxnpp24

  3. 3 Universidade de Lisboa
    info

    Universidade de Lisboa

    Lisboa, Portugal

    ROR https://ror.org/01c27hj86

  4. 4 Centro Nacional de Investigación sobre la Evolución Humana
    info

    Centro Nacional de Investigación sobre la Evolución Humana

    Burgos, España

    ROR https://ror.org/01nse6g27

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Revista:
Journal of iberian geology: an international publication of earth sciences

ISSN: 1886-7995,  1698-6180

Año de publicación: 2019

Volumen: 45

Número: 1

Páginas: 129-145

Tipo: Artículo

DOI: 10.1007/S41513-018-0089-8 DIALNET GOOGLE SCHOLAR

Otras publicaciones en: Journal of iberian geology: an international publication of earth sciences

Objetivos de desarrollo sostenible

Resumen

A multidisciplinary analysis of Holocene sediments from Saltés Island (Tinto-Odiel estuary, SW Spain) has allowed to differentiate eigth sedimentary facies, according to their textural characteristics, internal structure, paleontology and archaeological content. Its interpretation and the chronological datings carried out reconstruct a transition from a sandy tidal plain to a fnal occupation by a Roman salting (cetaria) between the 1st century BC to 5th century A. This evolution includes the deposit of washover fans derived from high-energy events between the 1st century BC to 3th century AD. The integration of these new data with others from previous research has allowed partially complete the palaeoenviromental reconstruction of the marine domain of the Tinto-Odiel estuary.

Fuente de los datos: Dialnet