@article{10272/8969,
year = {2003},
url = {http://hdl.handle.net/10272/8969},
abstract = {The taphonomic analysis of the Osteichthyes and Condrichthyes of the Arenas de Huelva Formation permits to delimitate three parts into this Neogene unit: a) basal, glauconitic layer, with numerous teeths and caudal stings well preserved of the carchariniforms, lamniforms and skates that lived in a open marine environment; b) intermediate layer with several rich-shell horizons due to storms, with scarce eroded otholithes and teeths; and c) upper layer, without any remain of these groups because of the high dissolution level},
publisher = {Sociedad Geológica de España},
keywords = {Taphonomy},
keywords = {Osteichthyes},
keywords = {Condrichthyes},
keywords = {Neogene},
keywords = {SW Spain},
title = {Análisis tafonómico preliminar de la ictiofauna pliocènica del S.O. de España},
title = {Taphonomic analysis of the Pliocene Icthyofaune of southwestern Spain},
author = {Ruiz Muñoz, Francisco and Abad de los Santos, Manuel and García García, Edith Xiomara},
}