Also known as USGS 21651
Where: Ventura County, California (33.2° N, 119.6° W: paleocoordinates 33.0° N, 107.2° W)
• coordinate stated in text
• outcrop-level geographic resolution
When: Unnamed Formation, Middle Eocene to Middle Eocene (47.8 - 33.9 Ma)
• 3,500 feet of alternating marine sandstone and siltstone beds that contain minor amounts of interbedded conglomerate and pebbly mudstone. Is divided into 35 mapping units in Vedder and Norris (1963) but thestratigraphic location of the fossil collections are not indicated. Small andesite dikes of Miocene age intrude the Eocene strata. Dune sand and fossiliferous marine terrace deposits of Quaternary age overlie most of the Eocene strata. Bulk of the specific identifications suggest a middle to late Eocene age based on forms conspecific with those found in the Domengine Formation, the upper part of the Llajas Formation, the Rose Canyon shale member of the La Jolla Formation, and the Tejon Formation, all of whihc are considered to be in the upper half of the Eocene in Calfornia
• bed-level stratigraphic resolution
Environment/lithology: coastal; sandstone and siltstone
Size class: macrofossils
Reposited in the USGS
Collection methods: quarrying,
• Collected by Norris, Vedder et al. (1955, 1956). Earlier collections by Bowers (1890), Harbor and Reed (1933).
Primary reference: J. G. Vedder and R. M. Norris. 1963. Geology of San Nicolas Island, California. United States Geological Survey Professional Paper 369:1-65 [A. Miller/A. Hendy/P. Wagner]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 37932: authorized by Austin Hendy, entered by Austin Hendy on 27.03.2004
Creative Commons license: CC BY (attribution)
Taxonomic list
Bivalvia | |
"Ostrea aff. stewarti" = Phygraea stewarti
"Ostrea aff. stewarti" = Phygraea stewarti Hanna 1927 oyster |