Asociaciones palinológicas del tránsito Rhaetiense-Hettangiense en Asturias (España)

  1. Barrón, Eduardo
  2. Pieren Pidal, Agustín
  3. Goy Goy, Antonio
  4. Gómez Fernández, Juan José
Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Año de publicación: 2005

Título del ejemplar: XV Congreso Nacional de Sedimentología y IV Coloquio de Estratigrafía y Paleogeografía del Pérmico y Triásico de España

Número: 8

Páginas: 133-136

Tipo: Artículo

Otras publicaciones en: Geotemas (Madrid)

Resumen

The palynological study of 49 successive samples collected from the Vilorteo and Cantavieyo Diamond Drill Holes, drilled in the La Camocha Mine area, near Gijón (Asturias), allowed the characterization of three palynological assemblages. The oldest assemblages (PA1) is characteristic of the Rhaetian. A precise age for the middle assembalges (PA2) cannot be assigned, due to the scarce productivity of the samples. The youngest (PA3) is characteristic of the Hettangian. Consequently the Triassic-Jurassic boundary (TJB) is located within the upper part of the carbonate succession of the Solís Mb. Two palynozones, Rhaetipollis germanicus Zone and Krausselisporite reissingeri Zone, have been established. Their boundary nearly coincides with the TJB. A quantitative analysis reveals an increase in the proportion of hygrophilous and warmer taxa near the TJB, compatible with a global climatic change probably related with the end-Triassic mass extinction.