Zamora, Samuel, Sumrall, Colin D., Sprinkle, James (2015) New long-stemmed eocrinoid from the Furongian Point Peak Shale Member of the Wilberns Formation, central Texas. Journal of Paleontology, 89 (1) 189-193 doi:10.1017/jpa.2014.16
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | New long-stemmed eocrinoid from the Furongian Point Peak Shale Member of the Wilberns Formation, central Texas | ||
| Journal | Journal of Paleontology | ||
| Authors | Zamora, Samuel | Author | |
| Sumrall, Colin D. | Author | ||
| Sprinkle, James | Author | ||
| Year | 2015 (January) | Volume | 89 |
| Issue | 1 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/jpa.2014.16Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 422266 | Long-form Identifier | mindat:1:5:422266:2 |
| GUID | 0 | ||
| Full Reference | Zamora, Samuel, Sumrall, Colin D., Sprinkle, James (2015) New long-stemmed eocrinoid from the Furongian Point Peak Shale Member of the Wilberns Formation, central Texas. Journal of Paleontology, 89 (1) 189-193 doi:10.1017/jpa.2014.16 | ||
| Plain Text | Zamora, Samuel, Sumrall, Colin D., Sprinkle, James (2015) New long-stemmed eocrinoid from the Furongian Point Peak Shale Member of the Wilberns Formation, central Texas. Journal of Paleontology, 89 (1) 189-193 doi:10.1017/jpa.2014.16 | ||
| In | (2015, January) Journal of Paleontology Vol. 89 (1) Cambridge University Press (CUP) | ||
| Abstract/Notes | AbstractLlanocystis wilbernsensisn. gen. n. sp. (Eocrinoidea, Echinodermata) is described based on three specimens from the Furongian Point Peak Shale Member of the Wilberns Formation in central Texas. It displays a unique morphology including a very long stem constructed with holomeric columnals, few feeding appendages, and a polyplated theca. The specimens occur in an intraformational conglomerate deposited in a proximal carbonate platform environment and represent an example of the poorly documented “pelmatozoan” radiation that occurred in proximal facies by the end of the Cambrian. | ||
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