Wheeler Shale

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Template:Short description Script error: No such module "Infobox".Template:Template otherScript error: No such module "check for unknown parameters". Template:CEXNAV The Wheeler Shale (named by Charles Walcott) is a Cambrian (c.Script error: No such module "Check for unknown parameters". 507 Ma) fossil locality world-famous[1] for prolific agnostid and Elrathia kingii trilobite remains (even though many areas are barren of fossils)[2] and represents a Konzentrat-Lagerstätte. Varied soft bodied organisms are locally preserved, a fauna (including Naraoia, Wiwaxia and Hallucigenia) and preservation style (carbonaceous film) normally associated with the more famous Burgess Shale.[3] As such, the Wheeler Shale also represents a Konservat-Lagerstätten.[4]

Together with the Marjum Formation and lower Weeks Formation, the Wheeler Shale forms Script error: No such module "convert". of limestone and shale exposed in one of the thickest, most fossiliferous and best exposed sequences of Middle Cambrian rocks in North America.[5]

At the type locality of Wheeler Amphitheater, House Range, Millard County, western Utah, the Wheeler Shale consists of a heterogeneous succession of highly calcareous shale, shaley limestone, mudstone and thin, flaggy limestone.[6] The Wheeler Formation (although the Marjum & Weeks Formations are missing) extends into the Drum Mountains, northwest of the House Range where similar fossils and preservation are found.[6]

Taphonomy and sedimentology

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File:Asaphiscuswheelerii.jpg
Asaphiscus wheeleri, Cambrian, Wheeler shale, Utah
File:Emeraldella brocki.jpg
Emeraldella brocki an arthropod From the Burgess Shale

Detailed work recognises a number of ~10 m thick lagerstätten sequences in the formation, each of which formed at a sea-level high stand[7] in deep water.[8] The lagerstätte were deposited by turbidities and mudslides onto an oxygenated sea floor.[7] The productive layers comprise mud and clay particles, with a tiny fraction of wind-blown quartz.[9]

Stratigraphy

The Wheeler Shale spans the Ptychagnostus atavus[10] and uppermost-Middle Cambrian Bolaspidella trilobite zones (See House Range for full stratigraphy).

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File:Stanleycaris sp. KUMIP 153923.png
Stanleycaris sp. from Wheeler shale, originally described as Aysheaia prolata

Script error: No such module "Labelled list hatnote". Incomplete list of the fauna of the Wheeler Shale:[6][11][12][13][14][15][16] (Note: the preservation of hard bodied trilobite remains and soft bodied animals seems to be mutually exclusive within particular horizons.)[4][17]


Protista

Arthropoda

Dinocaridida

Trilobita

Brachiopoda

Chordata

Cnidaria

Mollusca

Echinodermata

Porifera

Priapulida

Unclassified

References

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  12. Photos of Wheeler Shale fossils from UC Berkeley
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  14. Utah's Cambrian Life from University of Kansas Natural History Museum
  15. Cambrian fossils from Utah by the University of Utah
  16. Comprehensive treatment from The Virtual Fossil Museum
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