2024-03-29T10:35:57Zhttp://buleria.unileon.es/oai/requestoai:buleria.unileon.es:10612/97942020-12-10T09:10:51Zcom_10612_17col_10612_21
Paleontologia
Soto, Francisco
Fernández, Luis Pedro
Fernández Martínez, Esperanza
García Alcalde, Jenaro Luis
Méndez Bedia, Isabel
Truyols Massoni, Montse
Vera de la Puente, Carmen
2019-03-14
In the Cantabrian Zone (NW Spain), as in other North Gondwanan regions, the first Devonian stage of reef development (just a few metres above the Lochkovian-Pragian boundary) is of minor importance and it is represented by small biostromal patches composed of branching rugose corals (disphyllids), branching tabulate corals (thamnoporids) and laminar to tabular, sometimes domical, strornatoporoids (coenostromatids, labechiids, atelodictyids, actinostromatids) and tabulate corals (favositids, micheliniids). These biostromal units are located in the middle part (Mernber C) of the Lebanza formation (Palencia province: Palentine Domain, SE Cantabrian Zone) and in the upper part or the Nieva formation (Asturias province: Asturo-Leonese Domain, N Cantabrian Zone).
http://hdl.handle.net/10612/9794
spa
The first reefal episode (Earliest Plagian) in the Cantabrian Zone (NW Spain) and its relationship with the Lochkovian-Pragian Boundary Event
info:eu-repo/semantics/conferenceObject
TEXT
BULERIA. Repositorio Institucional de la Universidad de León
Hispana