The Poleta Formation is a geological unit known for the exceptional fossil preservation in the Indian Springs Lagerstätte, located in eastern California and Nevada.
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 Stage 3 Nevadella trilobite zone (= Laurentian Montezuman stage), with higher beds dating to the Stage 4 Olenellus trilobite zone (= Laurentian Dyeran stage), making the formation the same age as the Sirius Passet and just younger than the Chengjiang. It outcrops in Esmeralda County in western Nevada.
The Poleta Formation is mainly composed of limestone rocks within its lower and upper sections, with its middle section containing siltstone, quartzite, and some limestone.
The formation contains three members, which are as follows, in ascending age:
The formation was deposited on an offshore shelf between the wave base and storm base, and experienced storm-related pulses of siliciclastic sediment input. 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.
The modes of preservation of the non-biomineralised material found within the Indian Springs Lagerstätte has been noted to be either clay-mineral replacement, and pyrite or iron oxide staining. This is similar to the modes of preservation seen in the Chengjiang Lagerstätte. The Lagerstätte is also an example of a obrution-type deposition, which is a rapid burial of organisms, with some helicoplacoids being buried alive, still in their upright position. This form of deposition will have also obscured the buried specimens from scavengers.
Most of the fauna is biomineralized, including brachiopods, hyolithids, trilobites, archeocyathids from the Gold Point Reef locality, and helicoplacoids, which are often articulated. Non-mineralized components of these fossils are also preserved, as are sponges, anomalocaridid parts, and a range of algae and cyanobacteria.
Trace fossils, mainly Planolites, are also common; ichnofossils generally lie on the bedding plane and very few penetrate more than into the sediment. The biota of this formation has been noted to be similar to the Utah Lagerstätten, more so to the Spence Shale.