@article{10272/10329,
year = {1997},
url = {http://hdl.handle.net/10272/10329},
abstract = {Fossil travertine deposits have been recognized in the Aguilar Fm., which are intercalated vyithin the typical lacüstrine/palustrine limestones of this unit. Microscopically, they are characterised by numerous plant, remains and microscopically by abundant features atributáble 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},
publisher = {Sociedad Geológica de España},
keywords = {Palaeotravertine},
keywords = {Bacterial activity},
keywords = {Palaeoecoldgy and palaeohidrology},
keywords = {Aguilar Fm.},
keywords = {Late jurassic-earliest Cretaceous},
keywords = {Basquecahtabrian basin},
title = {Reconocimiento de acumulaciones travertínicas fósiles en la Fm. Aguilar (Kimmeridgiense-Berriasiense de Palencia y Burgos): implicaciones paleoecológicas y paleohidrológicas},
title = {Recognition of fossil travertine accumulations in the Aguilar Fm. (Kimmeridgian-Berriasian of Palencia and Burgos): palaeoecological and palaeohidrological implications},
author = {Hernández, José María and Diéguez, C. and Pujalte, Victoriano and Robles, Sergio and Wright, V. P.},
}