TY - JOUR
T1 - The illaenid trilobites vysocania (Vaněk & vokáč, 1997) and octillaenus (barrande, 1846) from the upper Ordovician of the Czech Republic, Portugal, Spain and Morocco
AU - Pereira, Sofia
AU - Marques da Silva, Carlos
AU - Sá, Artur Abreu
AU - Pires, Miguel
AU - Marques Guedes, Armando
AU - Budil, Petr
AU - Laibl, Lukáš
AU - Rábano, Isabel
N1 - Funding Information:
canech) for granting access to fossil collections under their care; J. Colmenar (Natural History Museum of Denmark, Copenhagen) for assisting in fieldwork in Portugal, Spain and Morocco; J. Álvaro (Instituto de Geociencias, CSIC-UCM, Madrid) and S. Lorenzo (Universidad de Castilla-La Mancha, Ciudad Real) for assisting in fieldwork in Morocco; S. Zamora (Instituto Geológico y Minero de Espańa, Madrid) for his help with Fombuena Formation material; A. Cravinho Santos (Universidade de Lisboa) for assisting with some images and formatting details; J. C. Gutiérrez-Marco (CSIC-Spanish National Research Council, Madrid) for facilitating access to MGM specimens; Martin David (Prague) for fruitful discussions on Králův Dvůr Formation specimens; and J. Adrain (University of Iowa, Iowa City) for helpful discussions on various matters. We thank David Bruton (Natural History Museum, University of Oslo) for revision and suggestions. We specially thank D. Holloway (Museums Victoria) for valuable revisions, discussion and suggestions that allowed us to significantly improve our manuscript. SP is supported by a FCT PhD grant (SFRH/BD/73722/2010) and a SYNTHESYS (Synthesis of Systematic Resources) grant (CZ-TAF-4786). AAS and IR are supported by the project CGL2012-39471 of the Spanish MINECO. PB was supported by the Czech Geological Survey internal project No. 339900. LL is supported by the Ministry of Culture of the Czech Republic (DKRVO 2016/06, National Museum, 00023272). This paper is a contribution to the International Geoscience Programme (IGCP) Project 653 – The Onset of the Great Ordovician Bio-diversification Event (IUGS-UNESCO).
Funding Information:
We thank M. Ramalho (Museu Geológico de Lisboa), J. Ignacio (Universidad de Zaragoza), J. Anger (Senckenberg Museum, Frankfurt am Main), C. Mellish (National History Museum, London) and P. Kraft (Muzeum Dr. Bohuslava Horáka v Rokycanech) for granting access to fossil collections under their care; J. Colmenar (Natural History Museum of Denmark, Copenhagen) for assisting in fieldwork in Portugal, Spain and Morocco; J. álvaro (Instituto de Geociencias, CSIC-UCM, Madrid) and S. Lorenzo (Universidad de Castilla-La Mancha, Ciudad Real) for assisting in fieldwork in Morocco; S. Zamora (Instituto Geológico y Minero de Espana, Madrid) for his help with Fombuena Formation material; A. Cravinho Santos (Universidade de Lisboa) for assisting with some images and formatting details; J. C. Gutiérrez-Marco (CSIC-Spanish National Research Council, Madrid) for facilitating access to MGM specimens; Martin David (Prague) for fruitful discussions on Králuv Dvur Formation specimens; and J. Adrain (University of Iowa, Iowa City) for helpful discussions on various matters. We thank David Bruton (Natural History Museum, University of Oslo) for revision and suggestions. We specially thank D. Holloway (Museums Victoria) for valuable revisions, discussion and suggestions that allowed us to significantly improve our manuscript. SP is supported by a FCT PhD grant (SFRH/BD/73722/2010) and a SYNTHESYS (Synthesis of Systematic Resources) grant (CZ-TAF-4786). AAS and IR are supported by the project CGL2012-39471 of the Spanish MINECO. PB was supported by the Czech Geological Survey internal project No. 339900. LL is supported by the Ministry of Culture of the Czech Republic (DKRVO 2016/06, National Museum, 00023272). This paper is a contribution to the International Geoscience Programme (IGCP) Project 653 – The Onset of the Great Ordovician Biodiversification Event (IUGS-UNESCO).
Publisher Copyright:
© 2017, Czech Geological Survey. All rights reserved.
Copyright:
Copyright 2018 Elsevier B.V., All rights reserved.
PY - 2017
Y1 - 2017
N2 - The illaenid trilobite Vysocania is widely represented in the Upper Ordovician of the Czech Republic, Portugal and Spain, and is one of the most characteristic taxa in the high-latitude peri-Gondwana palaeobiogeographical region to which it is endemic. Three species of the genus that were formerly assigned to Stenopareia and Zetillaenus, from the Czech Republic and Spain respectively, are herein revised, and a new species is described from the Czech Republic. The genus Octillaenus, of which a new species is described from the Upper Ordovician of Morocco, is considered to have arisen from Vysocania through paedomorphic (neotenic) processes. The relationships between Vysocania, Octillaenus, Stenopareia and Zetillaenus are reviewed and the criteria used in the definition of these taxa discussed. Species assigned to Vysocania are V. vaneki (type-species), V. iberica, V. moraveci sp. nov. and V. panderi; species assigned to Octillaenus are O. hisingeri (type-species) and O. marocanus sp. nov. Vysocania appears for the first time in the lower Berounian (Sandbian) and has its last undoubted record in the upper Berounian (upper Katian); Octillaenus is presently restricted to the Kralodvorian (upper Katian).
AB - The illaenid trilobite Vysocania is widely represented in the Upper Ordovician of the Czech Republic, Portugal and Spain, and is one of the most characteristic taxa in the high-latitude peri-Gondwana palaeobiogeographical region to which it is endemic. Three species of the genus that were formerly assigned to Stenopareia and Zetillaenus, from the Czech Republic and Spain respectively, are herein revised, and a new species is described from the Czech Republic. The genus Octillaenus, of which a new species is described from the Upper Ordovician of Morocco, is considered to have arisen from Vysocania through paedomorphic (neotenic) processes. The relationships between Vysocania, Octillaenus, Stenopareia and Zetillaenus are reviewed and the criteria used in the definition of these taxa discussed. Species assigned to Vysocania are V. vaneki (type-species), V. iberica, V. moraveci sp. nov. and V. panderi; species assigned to Octillaenus are O. hisingeri (type-species) and O. marocanus sp. nov. Vysocania appears for the first time in the lower Berounian (Sandbian) and has its last undoubted record in the upper Berounian (upper Katian); Octillaenus is presently restricted to the Kralodvorian (upper Katian).
KW - Dalmanitoidean Realm
KW - High-latitude peri-Gondwana
KW - Illaenidae
KW - Stenopareia
KW - Zetillaenus
UR - http://www.scopus.com/inward/record.url?scp=85040166729&partnerID=8YFLogxK
U2 - 10.3140/bull.geosci.1642
DO - 10.3140/bull.geosci.1642
M3 - Article
AN - SCOPUS:85040166729
SN - 1214-1119
VL - 92
SP - 465
EP - 490
JO - Bulletin of Geosciences
JF - Bulletin of Geosciences
IS - 4
ER -