LSJU loc. FL 36C, Cottonwood Mountains: Arnsbergian, California
collected by J. F. McAllister 1938
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Cephalopoda
- Goniatitida
- Glaphyritidae
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Cravenoceras merriami
Youngquist 1949
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see common names |
Geography
Country: | United States | State/province: | California | County: | Inyo |
Coordinates: | 36.8° North, 117.5° West (view map) | ||||
Paleocoordinates: | 3.0° North, 46.9° West | ||||
Basis of coordinate: | estimated from map |
Time
Period: | Carboniferous | Epoch: | Mississippian |
Stage: | Serpukhovian | 10 m.y. bin: | Carboniferous 3 |
Key time interval: | Arnsbergian | ||
Age range of interval: | 327.4 - 324 m.y. ago |
Stratigraphy
Formation: | Rest Spring | ||||
Stratigraphy comments: McAllister (1952) and Gordon (1964) say this is the uppermost 10 ft and probably lower 5 ft of Rest Spring Shale
If Perdido group, this would be the Mexican Spring Formation of Stevens et al., 1996 Titus (2000) says this is lower Rest Spring Shale, but doesn't give any evidence. Says "the formational contact between the Rest Spring Shale and the underlying Mexican Spring Formation essentially coincides with the Pendleian-Arnsbergian boundary" making this Arnsbergian if Rest Spring, or Pendleian if Mexican Spring. |
Lithology and environment
Primary lithology: | fine,gray "limestone" | ||
Secondary lithology: | calcareous siltstone | ||
Includes fossils? | Y | ||
Lithology description: In the Quartz Spring area the Early Mississippian Tin Mountain Limestone is overlain by a sequence of varied beds that consists of calcareous siltstone, sand- stone, conglomerate and interbedded chert, limestone, silty limestone, and siltstone having some shale. These constitute the Perdido Formation of McAllister (1952, p. 22-25), approximately 610 feet thick in its composite type section south of Perdido Canyon and south of Rest Spring.The topmost bed of this formation, a dark-gray fine-grained limestone, 6 to 12 inches thick, is crowded with fossils, mostly Cravenoceras hesperium Miller and Furnish. Four to five feet of very soft shale, grayish red to purplish gray, separate it from the gray locally sandy limestone below that carries productids, spirifers, and other brachiopods. | |||
Environment: | marine indet. | Tectonic setting: | passive margin |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Collection methods: | survey of museum collection | ||
Reason for describing collection: | taxonomic analysis | ||
Museum repositories: | CAS | ||
Collectors: | J. F. McAllister | Collection dates: | Nov. 23,1938 |
Metadata
Database number: | 217085 | ||
Authorizer: | J. Marcot | Enterer: | J. Marcot |
Modifier: | J. Marcot | Research group: | marine invertebrate |
Created: | 2021-01-22 01:25:27 | Last modified: | 2021-01-26 19:49:10 |
Access level: | the public | Released: | 2021-01-22 01:25:27 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
70706. | M. Gordon, Jr. 1964. California Carboniferous cephalopods. United States Geological Survey Professional Paper 483-A:A1-A27 [J. Marcot/J. Marcot/J. Marcot] |