Reconocimiento de acumulaciones travertínicas fósiles en la Fm. Aguilar (Kimmeridgiense-Berriasiense de Palencia y Burgos). Implicaciones paleoecológicas y paleohidrológicas
Fossil travertine deposits ha ve been recognlzed in the Aguilar Fm., which are intercalated within the typical lacustrine/palustrine limestones of this unit. Macroscopically, they are characterised by numerous plant remains and microscopically by abundant features attributable to microbial activity....
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1998 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/183352 |
| Acceso en línea: | http://hdl.handle.net/10261/183352 |
| Access Level: | acceso abierto |
| Palabra clave: | Palaeotravertine Bacteria! activity Palaeoecoiógy and palaeohidrology Aguilar Fm. Late Jurassic-earliest Cretaceous Basque-Cantabrian Basin |
| Sumario: | Fossil travertine deposits ha ve been recognlzed in the Aguilar Fm., which are intercalated within the typical lacustrine/palustrine limestones of this unit. Macroscopically, they are characterised by numerous plant remains and microscopically by abundant features attributable to microbial activity. The travertine accumulation occurred next to an important fault line that was contemporaneously active. Because of that, they are thought to record former hot-springs within a discharge-type water inflow system. |
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