USGS D2119: Late Maastrichtian, Wyoming

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Cephalopoda - Ammonitida - Baculitidae
Baculites grandis Hall and Meek 1855
Cephalopoda - Ammonitida - Scaphitidae
Hoploscaphites sp. Nowak 1911
    = Hoploscaphites sargklofak Landman et al. 2015
Landman et al. 2015
Bivalvia - Nuculanida - Nuculanidae
Nuculana bisulcata
unclassified
Bryozoa indet. Ehrenberg 1831
membraniporoid bryozoan
see common names

Geography
Country:United States State/province:Wyoming County:Niobrara
Coordinates: 43.3° North, 104.3° West (view map)
Paleocoordinates:49.7° North, 79.1° West
Basis of coordinate:estimated from map
Geographic resolution:small collection
Time
Period: Cretaceous Epoch: Late Cretaceous
Stage: Maastrichtian 10 m.y. bin: Cretaceous 8
*Epoch:Senonian
Key time interval: Late Maastrichtian Ammonoid zone:  Baculites grandis
Age range of interval: 72.1 - 66 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Formation:Pierre Shale Member:upper unnamed shale
Regional section:Formation Regional bed:363 - 418 ft
Regional order:top to bottom
Stratigraphic resolution:bed
Stratigraphy comments: Pierre shale, from limestone concretions 363 - 418' below top. Was bed 98
Lithology and environment
Primary lithology:gray lithified silty "shale"
Secondary lithology: "carbonate"
Environment:offshore Tectonic setting:cratonic basin
Geology comments: "Shale. dark gray where fresh, weathers gray; contains laminae of lighter gray soft siltstone and fine-gr. ss. a few small brown-weathering concretions, commonly very fossiliferous, are scattered throughout the unit."
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Collection methods:mechanical,field collection
Reason for describing collection:biostratigraphic analysis
Museum repositories:USGS
Collection method comments: "[collected] from concretions throughout unit"
Taxonomic list comments:"The fossils are ordinarily well-preserved. Most of the cephalopod shells and the inner nacreous layer of Inoceramus are aragonitic, especially specimens from above the Red Bird Silty Member. Shell material and specimens from the Red Bird member and the upper 50' of the underlying Mitten Member is partially transformed to calcite...Ammonites...of the [mid-upper third] of the Mitten Member are...entirely aragonite whereas shell material [of underlying material] is completely transformed to calcite."
Metadata
Also known as:Pierre Shale (USGS D2119)
Database number:1581
Authorizer:J. Alroy, P. Wagner Enterer:M. Sommers, P. Wagner
Modifier:P. Wagner Research group:marine invertebrate
Created:1999-05-17 16:22:55 Last modified:2024-03-17 14:34:18
Access level:the public Released:1999-05-17 16:22:55
Creative Commons license:CC BY
Reference information

Primary reference:

45. J. R. Gill, W. A. Cobban, and P. M. Kier. 1966. The Red Bird Section of the Upper Cretaceous Pierre Shale in Wyoming. United States Geological Survey Professional Paper 393-A:1-73 [J. Alroy/M. Sommers/A. Clement]

Secondary references:

87912 N. H. Landman, W. J. Kennedy, and N. L. Larson. 2015. A new species of scaphitid ammonite from the Lower Maastrichtian of the Western Interior of North America, with Close Affinities to Hoploscaphites constrictus Sowerby, 1817. American Museum Novitates 3833:1-40 [P. Wagner/P. Wagner]