Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-25T05:59:25.123Z Has data issue: false hasContentIssue false

Late Ordovician trilobites from the Karagach Formation of the western Tarbagatai Range, Kazakhstan

Published online by Cambridge University Press:  11 February 2011

Mansoureh Ghobadi Pour
Affiliation:
Department of Geology, Faculty of Sciences, Golestan University, Gorgan, Iran Email: [email protected]; [email protected]
Lucy M. E. McCobb
Affiliation:
Department of Geology, National Museum of Wales, Cathays Park, Cardiff, CF10 3NP Wales, UK Email: [email protected]; [email protected]; [email protected]
Robert M. Owens
Affiliation:
Department of Geology, National Museum of Wales, Cathays Park, Cardiff, CF10 3NP Wales, UK Email: [email protected]; [email protected]; [email protected]
Leonid E. Popov
Affiliation:
Department of Geology, National Museum of Wales, Cathays Park, Cardiff, CF10 3NP Wales, UK Email: [email protected]; [email protected]; [email protected]

Abstract

Two trilobite faunas of late Ordovician (Sandbian and Katian) age are described from the siliciclastic Karagach Formation, western Tarbagatai Range, eastern Kazakhstan. They comprise 15 families and 24 genera and include the new taxa Agerina acutilimbata sp. nov., Birmanites akchiensis sp. nov., Dulanaspis karagachensis sp. nov. and Kimakaspis kovalevskyi gen. et sp. nov. Most of the Karagach Formation yields graptolites characteristic of the Diplograptus foliaceus [multidens] Biozone, which are associated with the older trilobite fauna; the uppermost part, which is the source of the younger trilobite fauna, contains Orthograptus quadrimucronatus and Dicranograptus hians which suggest a younger age, equating with the lowermost Ensigraptus caudatus Biozone, and the base of the Katian Stage. Most of the trilobite genera in both faunas have a wide geographical distribution in the late Ordovician, although Dulanaspis and Sinocybele are characteristic of low latitude eastern peri-Gondwanan faunas.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 2011

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)