Caracterización, significado e implicaciones paleoclimáticas de los paleosuelos ferralíticos de la Formación Frontada (Berriasiense superior, Grupo Campóo, Cuenca Vasco-Cantábrica)

  1. J.Mª Hernández 1
  2. V. Pujalte 2
  3. S. Robles 2
  1. 1 Fundación Cristina Enea, San Sebastián, Gipuzkoa
  2. 2 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info

    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 2019

Zenbakien izenburua: Comunicaciones presentadas en la LXVI Sesión Científica / Leioa (Bilbao), 24 de mayo de 2019

Zenbakia: 66

Orrialdeak: 23-26

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

The Frontada Formation (Campóo Group) presents an important amount of structures related to the migration and precipitation of iron in its alluvial floodplain sedimentary record. These pedogenical features are associated with processes of intense chemical weathering of the substrate and establishment of hydromorphic soils. The analysis of these structures has allowed us to deduce how they were generated, as well as to propose a genetic model to explain their origin. This model suggests a context of high climatic humidity and temperature, similar to the nowadays equatorial climate, under which the ferricretization processes occurred.

Datuen iturria: Dialnet