CSUN Loc. 1559 - Grays Harbor [Crescent Fm]: Ypresian, Washington
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Rhynchonellata
- Terebratulida
- Cancellothyrididae
|
||||||||||
Terebratulina weaveri
|
||||||||||
Terebratulina unguicula weaveri | ||||||||||
Scaphopoda
- Dentaliida
- Dentaliidae
|
||||||||||
Dentalium sp.
Linnaeus 1758
|
||||||||||
see common names |
Geography
Country: | United States | State/province: | Washington | County: | Grays Harbor |
Coordinates: | 47.3° North, 123.5° West (view map) | ||||
Paleocoordinates: | 51.3° North, 103.9° West | ||||
Basis of coordinate: | based on political unit | ||||
Geographic resolution: | outcrop |
Time
Period: | Paleogene | Epoch: | Eocene |
Stage: | Ypresian | 10 m.y. bin: | Cenozoic 2 |
*Period: | Tertiary | *Epoch: | Early/Lower Eocene - Middle Eocene |
*International age/stage: | Lutetian | *Local age/stage: | Capay |
Key time interval: | Ypresian | ||
Age range of interval: | 56 - 47.8 m.y. ago | ||
* legacy (obsolete) database fields |
Stratigraphy
Formation: | Crescent |
Stratigraphic resolution: | group of beds |
Lithology and environment
Primary lithology: | pebbly,green poorly lithified argillaceous,conglomeratic sandstone |
Includes fossils? | Y |
Lithology description: the main macrofossiliferous sedimentary unit is approximately 100 m thick and consists mostly of dark green, very fine to medium basaltic sandstone with rounded to subrounded grains. near the base of the unit, pebble conglomerates grade rapidly upward into coarse sandstone. intermixed with fossils are subrounded basaltic clasts that range in size from granule to medium. there are also some large pebble-sized lumpy calcareous nodules. the matrix of the pebble conglomerate is mudstone and the amount is variable. | |
Environment: | marine indet. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Collection methods: | bulk,field collection |
Reason for describing collection: | taxonomic analysis |
Museum repositories: | LACM |
Metadata
Database number: | 5551 | ||
Authorizer: | A. Miller | Enterer: | K. Layou |
Modifier: | M. Uhen | Research group: | marine invertebrate |
Created: | 1999-10-13 08:04:59 | Last modified: | 2019-04-23 16:18:08 |
Access level: | the public | Released: | 1999-10-13 08:04:59 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
332. | R. L. Squires and J. L. Goedert. 1994. Macropaleontology of the Eocene Crescent Formation in the Little River Area, Southern Olympic Peninsula, Washington. Contributions in Science (Natural History Museum of Los Angeles County) 444:1-32 [A. Miller/K. Layou/A. Hendy] |
Secondary references:
18061 | E. A. Nesbitt. 2018. Cenozoic Marine Formations of Washington and Oregon: an annotated catalogue. PaleoBios 35:1-20 [M. Uhen/M. Uhen/M. Uhen] |