New species of the Early Permian cerioid coral Kleopatrina from northwest Chihuahua, Mexico

Early Permian massive corals define a narrow zone (the Thysanophyllum coral belt of Stevens, 1982) that surrounded the northern and western margins of Pangaea from the southern Ural Mountains through western North America to Bolivia (Stevens, 1982; Wilson, 1990). This belt appears to have been essen...

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Bibliographic Details
Published in:Journal of Paleontology
Main Author: Stevens, Calvin H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1995
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022336000038154
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000038154
Description
Summary:Early Permian massive corals define a narrow zone (the Thysanophyllum coral belt of Stevens, 1982) that surrounded the northern and western margins of Pangaea from the southern Ural Mountains through western North America to Bolivia (Stevens, 1982; Wilson, 1990). This belt appears to have been essentially continuous in the Wolfcampian, and although massive corals persisted along this belt into the Leonardian, they were restricted to many fewer localities.