Evolución paleoambiental de una turbera finiholocena en el sector suroccidental del Parque Nacional de Doñana (S.O. España)

  1. Manuel Abad de los Santos 1
  2. Adolfo Francisco Muñoz Rodríguez 2
  3. María Luz González-Regalado Montero 2
  4. Francisco Ruiz Muñoz 2
  5. Joaquín Rodríguez Vidal 2
  6. Luis Miguel Cáceres Puro 2
  7. María Isabel Carretero León 3
  8. Guadalupe Monge Gómez 3
  9. Manuel Pozo Rodríguez 4
  10. M. Isabel Prudêncio 5
  11. María Isabel Dias 5
  12. R. Marqués González 5
  13. Tatiana Izquierdo 1
  14. Josep Tosquella Angrill 2
  15. Verónica Romero Aguilar 2
  1. 1 Universidad de Atacama, Chile
  2. 2 Universidad de Huelva, España
  3. 3 Universidad de Sevilla, España
  4. 4 Universidad Autónoma de Madrid, España
  5. 5 Universidad de Lisboa, Portugal
Journal:
Estudios geológicos

ISSN: 0367-0449

Year of publication: 2019

Volume: 75

Issue: 1

Type: Article

DOI: 10.3989/EGEOL.43417.514 DIALNET GOOGLE SCHOLAR lock_openOpen access editor

More publications in: Estudios geológicos

Metrics

Cited by

  • Scopus Cited by: 2 (19-02-2024)
  • Dialnet Métricas Cited by: 1 (18-02-2024)
  • Web of Science Cited by: 2 (18-10-2023)
  • Dimensions Cited by: 5 (14-12-2023)

JCR (Journal Impact Factor)

  • Year 2019
  • Journal Impact Factor: 0.577
  • Journal Impact Factor without self cites: 0.5
  • Article influence score: 0.183
  • Best Quartile: Q4
  • Area: GEOLOGY Quartile: Q4 Rank in area: 43/47 (Ranking edition: SCIE)

SCImago Journal Rank

  • Year 2019
  • SJR Journal Impact: 0.243
  • Best Quartile: Q4
  • Area: Geology Quartile: Q4 Rank in area: 183/301

Scopus CiteScore

  • Year 2019
  • CiteScore of the Journal : 0.9
  • Area: Geology Percentile: 26

Journal Citation Indicator (JCI)

  • Year 2019
  • Journal Citation Indicator (JCI): 0.23
  • Best Quartile: Q4
  • Area: GEOLOGY Quartile: Q4 Rank in area: 47/61

Dimensions

(Data updated as of 14-12-2023)
  • Total citations: 5
  • Recent citations (2 years): 3
  • Field Citation Ratio (FCR): 1.43

Abstract

The multidisciplinary analysis of a profile discovered by the winter storms on the coast of the Doñana National Park has allowed us to reconstruct the evolution of its western sector during the Late Holocene. Three phases have been defined, which reflect the transition from a brackish water marsh (FA-1) to a freshwater lagoon transformed into peat bog (FA-2), to end with the deposit of dune systems (FA-3).

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