The Spence Shale Lagerstatte; an important window into Cambrian biodiversity

The Spence Shale Member of the Langston Formation is a Cambrian (Miaolingian: Wuliuan) Lagerstatte in northeastern Utah and southeastern Idaho. It is older than the more well-known Wheeler and Marjum Lagerstatten from western Utah, and the Burgess Shale from Canada. The Spence Shale shares several s...

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Bibliographic Details
Published in:Journal of the Geological Society Vol. 176; no. 4; pp. 609 - 619
Main Authors: Kimmig, Julien, Strotz, Luke C, Kimmig, Sara R, Egenhoff, Sven O, Lieberman, Bruce S
Format: Journal Article
Language:English
Published: Oxford Geological Society of London 01-07-2019
The Geological Society of London
Geological Society Publishing House
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Summary:The Spence Shale Member of the Langston Formation is a Cambrian (Miaolingian: Wuliuan) Lagerstatte in northeastern Utah and southeastern Idaho. It is older than the more well-known Wheeler and Marjum Lagerstatten from western Utah, and the Burgess Shale from Canada. The Spence Shale shares several species in common with these younger deposits, yet it also contains a remarkable number of unique species. Because of its relatively broad geographic distribution, and the variety of different palaeoenvironments and taphonomy, the fossil composition and likelihood of recovering weakly skeletonized (or soft-bodied) taxa varies across localities. The Spence Shale is not only widely acknowledged for its collection of soft-bodied taxa, but also for its abundant trilobites and hyoliths. Recent discoveries from the Spence include problematic taxa and insights about the nature of palaeoenvironmental and taphonomic variation between different localities. Supplementary material: https://doi.org/10.6084/m9.figshare.c.4423145
Bibliography:USDOE
AC05-76RL01830
PNNL-SA-139163
ISSN:0016-7649
2041-479X
DOI:10.1144/jgs2018-195