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

  1. Esther Martín González 1
  2. Inés Galindo Jiménez 2
  3. José Mangas Viñuela 3
  4. Carmen Romero Ruiz 4
  5. Nieves Sánchez Jiménez 2
  6. Alberto González Rodríguez 4
  7. Juan Jesús Coello Bravo 1
  8. Álvaro Márquez 5
  9. Alejandro de Vera 1
  10. Juana Vegas Salamanca 2
  11. Carlos Melo 6
  1. 1 Museo de Ciencias Naturales de Tenerife
  2. 2 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    GRID grid.421265.6

  3. 3 Universidad de Las Palmas de Gran Canaria
    info

    Universidad de Las Palmas de Gran Canaria

    Las Palmas de Gran Canaria, España

    GRID grid.4521.2

  4. 4 Universidad de La Laguna
    info

    Universidad de La Laguna

    San Cristobal de La Laguna, España

    GRID grid.10041.34

  5. 5 Universidad Rey Juan Carlos
    info

    Universidad Rey Juan Carlos

    Madrid, España

    GRID grid.28479.30

  6. 6 Universidade de Lisboa
    info

    Universidade de Lisboa

    Lisboa, Portugal

    GRID grid.9983.b

Journal:
Vieraea: Folia Scientarum Biologicarum Canariensium

ISSN: 0210-945X

Year of publication: 2019

Issue: 46

Pages: 667-688

Type: Article

Export: RIS
Institutional repository: lockOpen access postprint

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.