Permian crinoids from the type-section of the Callytharra Formation, Callytharra Springs, Western Australia
Gary D. Webster
Abstract
Gary D. Webster
Abstract
An extremely diverse Permian crinoid fauna, one of the largest known from the Australian Palaeozoic, is described from the type section of the Callytharra Formation, west of Callytharra Springs, Western Australia. Forty species are recognized including 14 camerates, 25 inadunates, and 1 flexible. One new genus, Tapinocrinus, and three new species, T. macurdai, T. ingrami and Notiocatillocrinus callytharraensis are recorded. Recognition of Notiocatillocrinus and a dichocrinid in Western Australia establishes additional links with the eastern Australia Early Permian marine faunas. Eleven of the species are known to occur in the Permian of Timor. Recognition of these species suggests that the accepted age of the Callytharra Formation or, more likely, the Timor crinoid-bearing beds should be reconsidered.
OpenAlex reports 31 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
An extremely diverse Permian crinoid fauna, one of the largest known from the Australian Palaeozoic, is described from the type section of the Callytharra Formation, west of Callytharra Springs, Western Australia. Forty species are recognized including 14 camerates, 25 inadunates, and 1 flexible. One new genus, Tapinocrinus, and three new species, T. macurdai, T. ingrami and Notiocatillocrinus callytharraensis are recorded. Recognition of Notiocatillocrinus and a dichocrinid in Western Australia establishes additional links with the eastern Australia Early Permian marine faunas. Eleven of the species are known to occur in the Permian of Timor. Recognition of these species suggests that the accepted age of the Callytharra Formation or, more likely, the Timor crinoid-bearing beds should be reconsidered.
Key concepts: Crinoid, Permian, Fauna, Paleozoic, Paleontology, Geology, Genus, Section (typography)