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Marcos Vaqueiro Rodríguez
Instituto Universitario de Xeoloxía. Universidade da Coruña. Campus de Elviña, Edificio ESCI. 15071 A Coruña, Galicia, EspañaClube de Espeleoloxía A Trapa (CETRA), Vigo, España
Spain
https://orcid.org/0000-0001-9086-2891
Reimundo Costas Vázquez
Clube de Espeleoloxía A Trapa (CETRA), Vigo
David Costas-Suarez
Clube de Espeleoloxía A Trapa (CETRA), Vigo
Juan Ramón Vidal-Romaní
Instituto Universitario de Xeoloxía. Universidade da Coruña. Campus de Elviña, Edificio ESCI. 15071 A Coruña, Galicia, España
Spain
https://orcid.org/0000-0001-7158-4945
Vol. 39 (2017), Articles, pages 23-34
DOI: https://doi.org/10.17979/cadlaxe.2017.39.0.3550
Submitted: Jul 4, 2018 Published: Mar 1, 2017
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Abstract

Sima del Uro (NW, Spain) is a cave that although it has been developed in limestone, it has morphological characteristics defined by the recent tectonic activity in the area. Inside this cave it has been discovered a quality important paleontological fini-Holocene deposit that does not correspond, as is usual in the area, with a cave of hibernation or room but it was developed by the fauna fallen from the outside in the trap defined by a doline of collapse. This work presents the morphological cartography of the cavity that indicates the situation of the paleontological remains found.

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