Conodonts from Late Devonian island arc settings (Baruunhuurai Terrane, western Mongolia)

0524534 - GLÚ 2021 RIV NL eng J - Článek v odborném periodiku
Suttner, T. J. - Kido, E. - Ariunchimeg, Y. - Sersmaa, G. - Waters, J. A. - Carmichael, S. K. - Batchelor, C. J. - Ariuntogos, M. - Hušková, Aneta - Slavík, Ladislav - Valenzuela-Ríos, J. I. - Liao, J-C. - Gatovsky, Y. A.
Conodonts from Late Devonian island arc settings (Baruunhuurai Terrane, western Mongolia).
Palaeogeography, Palaeoclimatology, Palaeoecology. Roč. 549, July (2020), č. článku 109099. ISSN 0031-0182. E-ISSN 1872-616X.
[International Conodont Symposium (ICOS) on Progress on Conodont Investigation /4./. Valencia, 25.06.2017-30.06.2017]
Institucionální podpora: RVO:67985831
Klíčová slova: Famennian * Samnuuruul Formation * Conodont biodiversity analysis * Remote palaeoenvironments
Obor OECD: Paleontology
Impakt faktor: 3.318, rok: 2020
Způsob publikování: Omezený přístup
https://www.sciencedirect.com/science/article/pii/S0031018218302268

Upper Devonian marine deposits of the Baruunhuurai Terrane in western Mongolia represent island arc settings, which yielded a diverse conodont assemblage of 30 taxa, including species of Ancyrognathus (as well as one new species), Icriodus, Mehlina, Polygnathus and Palmatolepis. Biodiversity analysis of Ancyrognathus, Pelekysgnathus, Mehlina and Icriodus shows that the Mongolian conodont assemblage consists of two endemic and few cosmopolitan taxa. Representatives of the otherwise globally distributed genus Pelekysgnathus are absent. An important factor influencing the regional distribution of conodont taxa seems to be the siliciclastic-dominated sedimentation of the Baruunhuurai Terrane during the early Famennian.
Trvalý link: http://hdl.handle.net/11104/0309173