Poleta Formation

Geological unit located in eastern California and Nevada From Wikipedia, the free encyclopedia

The Poleta Formation is a geological unit known for the exceptional fossil preservation in the Indian Springs Lagerstätte, located in eastern California and Nevada.[3]

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Poleta Formation
Stratigraphic range: Cambrian Series 2
~519–518 Ma
UnderliesHarkless Formation[1]
OverliesCampito Formation[2]
Lithology
PrimaryFine siliciclastics
Location
LocationWestern Nevada and Eastern California, USA
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Occurrence

The formation dates to the Stage 3 of the yet-to-be-ratified Cambrian Series 2; the lower portion base of the formation and the youngest Lagerstätte beds date to the Nevadella trilobite zone (= Laurentian Montezuman stage), with higher beds dating to the Olenellus trilobite zone (= Laurentian Dyeran stage), making the formation the same age as the Sirius Passet and just younger than the Chengjiang.[3] It outcrops in Esmeralda County in western Nevada.[3]

Depositional setting

The formation was deposited on an offshore shelf, and experienced storm-related pulses of siliciclastic sediment input.[3] Like many other Burgess Shale-type Lagerstätten, this unit was deposited on the Cordilleran margin of the Laurentian continent; it is among the oldest of the Lagerstätten from this region.[3]

Taphonomy

The fossil preservation is markedly similar to that in Utah Lagerstätten, particularly the Spence Shale.[3] The quality of preservation was obtained by the rapid burial of organisms in obrution events, which buried them out of reach of would-be scavengers.[3]

Fauna

Thumb
Archeocyathids from the Death Valley area

Most of the fauna is biomineralized, including brachiopods, hyolithids, trilobites, archeocyathids,[4] and helicoplacoids, which are often articulated.[3] Non-mineralized components of these fossils are also preserved, as are sponges, anomalocaridid parts, and a range of algae and cyanobacteria.[3]

Trace fossils, mainly Planolites, are also common; ichnofossils generally lie on the bedding plane and very few penetrate more than 1 millimetre (0.039 in) into the sediment.[3]

See also

References

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