RT info:eu-repo/semantics/conferenceObject T1 The first reefal episode (Earliest Plagian) in the Cantabrian Zone (NW Spain) and its relationship with the Lochkovian-Pragian Boundary Event A1 Soto, Francisco A1 Fernández, Luis Pedro A1 Fernández Martínez, Esperanza A1 García Alcalde, Jenaro Luis A1 Méndez Bedia, Isabel A1 Truyols Massoni, Montse A1 Vera de la Puente, Carmen A2 Paleontologia K1 Paleontología K1 Corales K1 Corals K1 Cordillera Cantábrica (España) K1 Devónico K1 Devonian K1 Arrecifes K1 Sedimentos (Geología) K1 Estratigrafía K1 Thamnoporids K1 Disphyllids K1 Coenostromatids K1 Labechiids K1 Atelodictyids K1 Actinostromatids K1 Favositids K1 Micheliniids K1 Asturias (Comunidad Autónoma) K1 Palencia AB 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). YR 2019 FD 2019-03-14 LK http://hdl.handle.net/10612/9794 UL http://hdl.handle.net/10612/9794 NO X Internacional Congress on Fossil Cnidaria and Porifera, 12-16 de agosto, 2007, San Petersburgo (Rusia) DS BULERIA. Repositorio Institucional de la Universidad de León RD 29-mar-2024