Distribución estratigráfica y consideraciones evolutivas sobre Scyphosphaera en el Mioceno Superior-Plioceno Inferior de la cuenca neógena de Alicante-Cartagena (Cordillera Bética Oriental). Parte III: Grupo S. campanula-S. turris

  1. C. Lancis 1
  2. J.A. Flores
  1. 1 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Año de publicación: 2004

Título del ejemplar: VII Congreso Geológico de España

Número: 7

Páginas: 247-250

Tipo: Artículo

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Otras publicaciones en: Geotemas (Madrid)

Resumen

The first specimens of Scyphosphaera are recorded during the Early Eocene, but during the Late Miocene it is observed an increase in diversity. Although these taxa have reduced biostratigraphic significance, it is an excellent paleoenvironmental marker relatively abundant in shallow and warm waters. This fact determines abundant record in several basins, whereas in other, are almost absent. In fact, most of the 50 identified species have been described in three sedimentary basins. In the Alicante-Cartagena basin, during the Messinian, we observed a high diversity. This is the third chapter of a series of four where we show the stratigraphic distribution as well as an attempt of evolutionary trend of the most characteristic groups of Scyphosphaera.

Fuente de los datos: Dialnet