Trilobites ordovícicos del macizo de Aragoncillo (Geoparque Mundial de la UNESCO Molina-Alto Tajo, Guadalajara, España)

  1. Sara Romero 1
  2. Juan Carlos Gutiérrez-Marco 2
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  2. 2 Instituto de Geociencias
    info

    Instituto de Geociencias

    Madrid, España

    ROR https://ror.org/04qan0m84

Aldizkaria:
Revista de la Sociedad Geológica de España

ISSN: 0214-2708

Argitalpen urtea: 2021

Alea: 34

Zenbakia: 2

Orrialdeak: 71-89

Mota: Artikulua

Beste argitalpen batzuk: Revista de la Sociedad Geológica de España

Laburpena

The Aragoncillo Paleozoic inlier, located to the east of the Guadalajara province near Molina de Aragón, was the place of discovery, more than 250 years ago, of the first trilobites found in the Iberian Peninsula. But beyond some later cites of Ordovician species in the 19th and 20th centuries, the group has never been the subject of local paleontological studies or descriptions. In this work, all the preceding data are reviewed and eleven Ordovician trilobite localities were studied in the upper part of the Villar del Saz Formation of the Aragoncillo inlier, being placed approximately at the same stratigraphic horizon of fossiliferous nodules included in dark shales. The trilobite assemblage comprises 14 species belonging to 13 different genera of 9 families and 4 orders. Among the taxonomic results, the first Iberian representatives of the phacopid Zeliszkella lapeyrei (Bureau) are described and illustrated for the first time outside the French Armorican Massif. The calymenacean Colpocoryphe grandis (Šnajdr) is also detected for the first time in Spanish Dobrotivian strata. The excellent preservation of some specimens of the phacopids Eodalmanitina destombesi (Henry) and Phacopidina micheli (Tromelin), allows to complete the knowledge of the delicate ornamentation of the cephalon of both species. From a biostratigraphic perspective, the entire trilobite assemblage is assigned to the upper part of the Placoparia borni trilobite Biozone of the upper Dobrotivian, which is correlated with the lower Sandbian due to the concurrence with graptolites of the Nemagraptus gracilis Biozone. The late record of Neseuretus tristani (Brongniart) on the same Upper Ordovician strata constitutes one of the very few evidences of the last occurrence of the important Gondwanan genus Neseuretus prior to its extinction. The study of the trilobites and their localities in the Aragoncillo inlier constitutes a contribution to knowledge of the geological heritage in an area that belongs to the Molina-Alto Tajo UNESCO Global Geopark.