The Sundance Formation is a western
North American sequence of
Middle Jurassic to
Upper Jurassic age
Dating from the
Bathonian
In the geologic timescale the Bathonian is an age and stage of the Middle Jurassic. It lasted from approximately 168.3 Ma to around 166.1 Ma (million years ago). The Bathonian Age succeeds the Bajocian Age and precedes the Callovian Age.
Str ...
to the
Oxfordian, around 168-157 Ma, It is up to 100 metres thick and consists of
marine shale, sandy shale,
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
, and
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...
deposited in the
Sundance Sea
The Sundance Sea was an epeiric sea that existed in North America during the mid-to-late Jurassic Period of the Mesozoic Era. It was an arm of what is now the Arctic Ocean, and extended through what is now western Canada into the central west ...
, an
inland sea that covered large parts of western North America during the Middle and early Late Jurassic.
Geology
The Sundance Formation underlies the western North American
Morrison Formation, the most fertile source of
dinosaur
Dinosaurs are a diverse group of reptiles of the clade Dinosauria. They first appeared during the Triassic period, between 243 and 233.23 million years ago (mya), although the exact origin and timing of the evolution of dinosaurs is t ...
fossils in the Americas, and is separated by a
disconformity
An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval ...
from the underlying
Middle Jurassic Gypsum Springs Formation
The Gypsum Springs Formation is a stratigraphical unit of Middle Jurassic age in the Williston Basin.
It takes the name from Gypsum Springs in Wyoming, and was first described in outcrop in Freemont County by J.D. Love in 1939.Love, J.D., 1939. ...
.
Fossils
The Sundance Formation is known for fossils of an extinct species of marine
cephalopod, the
belemnite
Belemnitida (or the belemnite) is an extinct order of squid-like cephalopods that existed from the Late Triassic to Late Cretaceous. Unlike squid, belemnites had an internal skeleton that made up the cone. The parts are, from the arms-most ...
''
Pachyteuthis densus'', as well as several extinct species of
oyster
Oyster is the common name for a number of different families of salt-water bivalve molluscs that live in marine or brackish habitats. In some species, the valves are highly calcified, and many are somewhat irregular in shape. Many, but not ...
, including ''Deltoideum'', ''Liostrea'', and ''Gryphaea nebrascensis''.
Fossil dinosaur 'footprints' on an ancient ocean shoreline are preserved in the formation and protected at the
Red Gulch Dinosaur Tracksite, located in the
Bureau of Land Management Red Gulch/Alkali National Back Country Byway, near Shell in
Big Horn County, Wyoming
Big Horn County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 11,521. The county seat is Basin. Its north boundary abuts the south boundary of Montana.
History
Big Horn County was created by ...
.
BLM−Bureau of Land Management, Wyoming Office: "Red Gulch Dinosaur Tracksite" website
info, maps, photo gallery, accessed 8.21.2015
Paleobiota
Vertebrates
Invertebrates
Fish
References
Jurassic geology of South Dakota
Jurassic geology of Wyoming
Jurassic System of North America
Upper Jurassic Series
Geology of the Rocky Mountains
Geologic formations of Montana
Geologic formations of Wyoming
Paleontology in Wyoming
{{Wyoming-geologic-formation-stub
Middle Jurassic Series
Bathonian Stage
Callovian Stage
Oxfordian Stage