Section 1/Locality 11222: Norian, Nevada

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Anthozoa
Anthozoa indet. Ehrenberg 1834
1 specimen
originally entered as "Anthozoa (colonial) sp."; changed by JA 30.6.04
Rhynchonellata - Terebratulida - Zeilleriidae
Zeilleria cf. elliptica (Zugmayer 1882)
1 specimen
Rhynchonellata - Terebratulida - Plectoconchidae
Plectoconcha aequiplicata (Gabb 1864)
105 specimens
Bivalvia
Bivalvia indet. Linnaeus 1758
11 specimens
Bivalvia - Ostreida - Pteriidae
Arcavicula sp. Cox 1964
1 specimen
Gastropoda
Gastropoda informal a
4 specimens
"Snail a"
Gastropoda informal t
6 specimens
"Snail t"
see common names

Geography
Country:United States State/province:Nevada County:Nye
Coordinates: 38.9° North, 117.6° West (view map)
Paleocoordinates:15.7° North, 53.8° West
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period:Triassic Epoch:Late/Upper Triassic
Stage:Norian 10 m.y. bin:Triassic 4
*Period:Late/Upper Triassic
*International age/stage:Late/Upper Carnian - Early/Lower Norian
Key time interval:Norian
Age range of interval:227.00000 - 208.50000 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Formation:Luning
Local section:Section 1 Local bed:11222
Local order:bottom to top
Stratigraphic resolution:group of beds
Stratigraphy comments: The Luning Formation is a remnant of a tectonically dismembered Lower Mesozoic carbonate platform complex exposed in scattered ranges throughout west-central Nevada. It rests unconformably upon different, often unamed, Late Paleozoic and Triassic units in each outcrop, but is regoinally overlain by the Upper Triassic through Lower Jurassic Gabbs and Sunrise Formations.
Lithology and environment
Primary lithology: lithified silty lime mudstone
Secondary lithology: lithified silty wackestone
Includes fossils?Y
Includes fossils?Y
Lithology description: The lowest, clastic member consists of 250m of chert pebble conglomerates, silty sandstones, and argillites. Except for rare fragments of petrified wood, these sediments are without fossils. The shaly limestone and calcareous shale members, each 200m thick, overlie the clastic unit. These are formed of interbedded silty and shaly limestones, limey shales, mudstones, and claystones, and contain a rich fossil component. The upper most carbonate member is a 400m thick sequence of comparatively silt- and clay-free limestones and secondary dolomites. This unit is also characterized by an abundance of fossils. The upper, fossi-bearing members of the Luning Formation are the focus of this report.
Environment:basinal (carbonate)
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Collection methods:bulk,field collection
Collection size:129 specimens
Reason for describing collection:paleoecologic analysis
Museum repositories:UCMP
Metadata
Database number:32597
Authorizer:D. Bottjer Enterer:N. Bonuso
Modifier:N. Bonuso Research group:marine invertebrate
Created:2003-07-09 14:23:33 Last modified:2004-08-19 12:32:37
Access level:the public Released:2003-07-09 14:23:33
Creative Commons license:CC BY
Reference information

Primary reference:

8769. J. A. Hogler. 1992. Community structure, paleoecology, and depositional environments within the Upper Triassic Luning Formation of Nevada. [D. Bottjer/N. Bonuso/N. Bonuso]