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Multiple trilobite fragments fossilized in the same rock

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Summary

USNM_35225 and USNM_35227: Pictured are multiple trilobite fragments fossilized in the same rock. These are commonly known as hash beds. "Hash" is an indicator of a near-shore environment, where waves could have broken apart trilobite exoskeletons and molts then re-deposited them. These particular “hash” beds are composed of trilobites Idahoia wyomingensis (USNM 35225) and Wilbernia walcotti (USNM 35227). Both samples were collected during the early 1900’s in the northern region of Yellowstone National Park, from an exposed section of the Upper Cambrian (~500 million years ago) Snowy Range Formation.;

Megan Norr;

March 2016;

Catalog #20792d;

Original #USNM_35225

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Tags

yellowstone national park fossils trilobites paleontology 20792 d usnm 35225 geology multiple trilobite fragments hash trilobites idahoia wyomingensis hash beds usnm trilobite fragments trilobite exoskeletons beds near shore environment wilbernia walcotti upper cambrian million years snowy range megan norr national parks gallery wyoming natural history 3d object
date_range

Date

1900
place

Location

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Source

National Parks Gallery
link

Link

https://npgallery.nps.gov/
copyright

Copyright info

Public Domain Dedication

label_outline Explore Trilobites, Megan Norr, Hash

Topics

yellowstone national park fossils trilobites paleontology 20792 d usnm 35225 geology multiple trilobite fragments hash trilobites idahoia wyomingensis hash beds usnm trilobite fragments trilobite exoskeletons beds near shore environment wilbernia walcotti upper cambrian million years snowy range megan norr national parks gallery wyoming natural history 3d object