68 D21. Laying the Foundation for the Modern Earth System at the Neoproterozoic-Paleozoic Transition
Monday, 10 October 2022
8:00 AM - 12:00 PM
Mile High Ballroom 4C
BOUGHT THE WORM FARM: VERMIFORM DIVERSITY AND TAPHONOMY IN THE CAMBRIAN SPENCE SHALE
Paper number: 68-12
Program: Technical Sessions
Time: 10:35 AM – 10:50 AM
Authors
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James SchiffbauerUniversity of Missouri - Columbia, Columbia, MO
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Rhiannon LaVineUniversity of Kansas, Lawrence, KS
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Anna WhitakerUniversity of Toronto Mississauga, Mississauga, ON
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Wade LeibachUniversity of Missouri, Columbia, MO
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Sara R. KimmigPennsylvania State University, University Park, PA
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Sven EgenhoffUniversity of North Dakota, Grand Forks, ND
Abstract
In addition, we analysed specimens from six localities using scanning electron microscopy (SEM) and integrated energy dispersive X-ray spectrometry (EDS), together with comparisons of published data. Taxa are predominantly preserved as a combination of carbonaceous compressions, iron oxide and pyrite replacement, but preservation varies between the shallower more carbonate rich locations in northern Utah and southern Idaho and the deeper water locations in the Wellsville Mountains of Utah. These variations in preservation are also linked to the quality of soft-tissue preservation in the different locations of the Spence Shale. So far, no vermiform specimens have been identified from the deepest water dark shales of the Spence Shale.
Geological Society of America Abstracts with Programs. Vol. 54, No. 6
doi: 10.1130/abs/2022AM-380803
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