Revisión de los depósitos costeros del estadio isotópico marino 5e (MIS 5e) de Fuerteventura (islas Canarias)

  1. Martín-González, E. 1
  2. Galindo, I. 2
  3. Mangas, J. 3
  4. Romero, C. 4
  5. Sánchez, N. 2
  6. González-Rodríguez, A. 5
  7. Coello, J. J. 1
  8. Márquez, A. 6
  9. De Vera, A. 1
  10. Vegas, J. 7
  11. Melo, C. 8
  1. 1 Museo de Ciencias Naturales de Tenerife
  2. 2 Instituto Geológico y Minero de España (IGME)
  3. 3 Instituto de Oceanografía y Cambio Global. Universidad de Las Palmas de Gran Canaria
  4. 4 Departamento de Geografía. Universidad de La Laguna
  5. 5 Área de Paleontología, Facultad de Biología, Universidad de La Laguna.
  6. 6 Área de Geología. Universidad Rey Juan Carlos
  7. 7 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

  8. 8 Departamento de Geologia, Faculdade de Ciências, Universidade de Lisboa
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Journal:
Vieraea: Folia Scientarum Biologicarum Canariensium

ISSN: 0210-945X

Year of publication: 2019

Issue: 46

Pages: 667-688

Type: Article

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Abstract

Fossiliferous outcrops are golden gates for the study of past events. The Quaternary is a period marked by several oscillations of the sea level, resulting in several glacial and interglacial events. The Last Interglacial period, with the warmest interval occurring between ~128 ka to ~116 ka (Marine Isotopic Stage 5e (MIS 5e) had a mean global temperature 2ºC higher than today, resulting in a mean sea level (msl) ~8.67 m above present msl. Fuerteventura Island holds an extensive and well preserved fossiliferous record that urges to be studied and preserved. As part of Project ECLIPSA, that aims to study field evidences of past climates changes in the Canary islands, a survey has been preformed in Fuerteventura Island, being now presented the preliminary results, as well a complilation of previous works regarding the outcrops from this island.

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