T9 The Early Paleozoic I: Radiations, Extinctions, and Environment
Sunday, 15 October 2023
8:00 AM - 12:00 PM
304 / 305
WAS EARTH’S OLDEST MINERAL COLLECTOR A CNIDARIAN? MORPHOLOGICAL, MINERALOGICAL, AND MICROSTRUCTURAL ANALYSIS OF SALTERELLA
Paper number: T9-5
Program: Technical Sessions
Time: 8:50 AM – 9:05 AM
Authors
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Shuhai XiaoVirginia Tech, Blacksburg, VA
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Noah KellerVirginia Tech, Blacksburg, VA
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Justin StraussDartmouth College, Hanover, NH
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Mary C. LonsdaleJohns Hopkins University, Baltimore, MD
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Amy HagenVirginia Tech, Blacksburg, VA
Abstract
Here, we present new morphological, mineralogical and microstructural evidence that supports Salterella as a stem cnidarian. Specimens have been collected from multiple localities across the Laurentian paleocontinent representing a range of depositional environments and taphonomic modes. The funnel-shaped body plan of Salterella is shared with other Cambrian organisms of cnidarian affinity including Cambrorhytium, Glossolites, and Sphenothallus. Salterella was selective in the grains it incorporated into its shell and must have had a morphology conducive to interacting with sediments in its environment. The tentacle structure of cnidarians would allow Salterella to pick grains and move them into its shell. The shell microstructures of Salterella consist of small lath-shaped prisms arranged in inclined lamellae, similar to the microstructures observed in Conularia and Sphenothallus. There are modern cnidarians known to create biomineralized shells and others that agglutinate grains. This study indicates that the capacity to use both mechanisms of skeleton construction is deeply rooted in Cnidarian biology.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-389588
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