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Gilmour, Ernest H., McColloch, Miriam E., Wardlaw, Bruce R. (1997) Bryozoa of the Murdock Mountain Formation (Wordian, Permian), Leach Mountains, northeastern Nevada. Journal of Paleontology, 71 (2) 214-236 doi:10.1017/s0022336000039159

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Reference TypeJournal (article/letter/editorial)
TitleBryozoa of the Murdock Mountain Formation (Wordian, Permian), Leach Mountains, northeastern Nevada
JournalJournal of Paleontology
AuthorsGilmour, Ernest H.Author
McColloch, Miriam E.Author
Wardlaw, Bruce R.Author
Year1997 (March)Volume71
Issue2
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000039159Search in ResearchGate
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Mindat Ref. ID417258Long-form Identifiermindat:1:5:417258:5
GUID0
Full ReferenceGilmour, Ernest H., McColloch, Miriam E., Wardlaw, Bruce R. (1997) Bryozoa of the Murdock Mountain Formation (Wordian, Permian), Leach Mountains, northeastern Nevada. Journal of Paleontology, 71 (2) 214-236 doi:10.1017/s0022336000039159
Plain TextGilmour, Ernest H., McColloch, Miriam E., Wardlaw, Bruce R. (1997) Bryozoa of the Murdock Mountain Formation (Wordian, Permian), Leach Mountains, northeastern Nevada. Journal of Paleontology, 71 (2) 214-236 doi:10.1017/s0022336000039159
In(1997, March) Journal of Paleontology Vol. 71 (2) Cambridge University Press (CUP)
Abstract/NotesA thin limestone tongue in the upper part of the Murdock Mountain Formation of northeastern Nevada contains abundant bryozoans of earliest Wordian age. This bryozoan fauna is close to the Kungurian-Kazanian boundary in Russia. These bryozoans are younger than those found in the Kaibab Formation of southern Nevada and slightly older than those in the Gerster Limestone of northern Nevada. This limestone tongue, herein referred to as the Stenodiscus beds, lies below the Thamnosia beds described by Wardlaw in the Murdock Mountain section of the Leach Mountains. This bryozoan-rich limestone tongue serves as a marker unit for mapping the Murdock Formation in the Leach Mountains.Nine new species of bryozoans occur in the Stenodiscus beds of the Murdock Mountain Formation: Hinganella felderi, Neoeridotrypella schilti, Stenopora parvaexozona, Stenodiscus murdockensis, Dyscritella acanthostylia, Pseudobatostomella irregularis, Streblotrypa (Streblotrypa) elongata, Morozoviella praecurriensis, and Thamniscus erraticus, Hinganella felderi, Neoeridotrypella schilti, Dyscritella acanthostylia, and Streblotrypa (Streblotrypa) elongata are very similar to species described from Russia.


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To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
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