Luminiscencia frente a quimismo elemental en inocerámidos (Bivalvia) de facies profunda (Formación de Plentzia, Santóniense del Arco Vasco). (Parte I)

Inoceramid shells (four individuals) from deep facies sediments of the Plentzia Formation) (Santonian, Basque Arc) have been analysed to determine their elemental chemistry (Mg2*, Sr2*, Na+, Ba2*, Fe2* and Mn2*) using the electronic pròbe' microanalyse'r. Relationships between the...

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Detalles Bibliográficos
Autores: Jiménez Berrocoso, A., Zuluaga, María Cruz, Elorza, Javier
Tipo de recurso: artículo
Fecha de publicación:2003
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/9062
Acceso en línea:http://hdl.handle.net/10272/9062
Access Level:acceso abierto
Palabra clave:Inoceramids
Luminescence
Elemental chemistry
Deep burial diagenesis
Santonian
Basque Arc
Descripción
Sumario:Inoceramid shells (four individuals) from deep facies sediments of the Plentzia Formation) (Santonian, Basque Arc) have been analysed to determine their elemental chemistry (Mg2*, Sr2*, Na+, Ba2*, Fe2* and Mn2*) using the electronic pròbe' microanalyse'r. Relationships between the luminescent behaviour of the selected inoceramids and their elemental chemistry (obtained from eight transects with a ¡total of 1235 ana:iyses) have been established. Results, indicate that Mg2*'and Sr2* keep higher values tat the medium shell layer, where luminescènce isj,ess intense. By contrast, Fe2+ and Mn-* are considerably higher at both the outer andJnner shell layer and inter-prismatic zones, where luminescence exhibits the highest colour intensity (bright-yellowish). On the other hand, Na* and Ba2* do not show a clear relationship with the luminescent behaviour of the analysed inoceramids, as their variations along the transects do not follow the luminescent changes of the shells. Therefore, it is suggested that in spite of the deep burial suffered by the sediments, which deeply overprinted the elemental chemistry of the shells, Na* and Ba2* profiles could still preserve patterns close to the originals