Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography
BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems

Collection: CSUN 1580 Kern County, California, USA

Age37.2 - 33.9 Ma (Paleogene)
IntervalLate Eocene
Lat/Long35.7036,-119.992
LocationCSUN 1580
Mindat.org Region (for given coordinates)Kern County, California, USA
FormationWagonwheel
Membermiddle siltstone
ZoneRefugian Stage
Lithology Description"The calcareous sandstone bodies are each about 20 m in lateral extent and consist of closely spaced, triple-stacked discontinuous massive units separated by thin intervals of silty mudstone.... At a few places in the lower part of the calcareous sandstone body ... there are wavy-banded layers of cement and rip-up clasts (9 cm in length) of cross-bedded sandy limestone...."
Lithologysandstone
Minor Lithologycalcareous
Second Lithologysiltstone
Second Minor Lithologymuddy
Environmentsubmarine fan
Geology Comments"The taxonomic composition and low diversity (almost mono- specific) of the megafauna, as well as the dense concentration of articulated lucinid, thyasirid, and vesicomyid bivalves in isolated and anomalous carbonate-bearing deposits that have a petroliferous odor, are very similar to modern-day and Cenozoic examples of chemosynthetic communities associated with cool- fluid seepage"

Recorded Fossils

Accepted NameHierarchyPreservationAge
Epilucina washingtoniana
species
Animalia : Mollusca : Bivalvia : Lucinida : Lucinidae : Epilucina : Epilucina washingtonianaaragonite
body,trace
37.2 - 33.9 Ma
Paleogene
Conchocele conradii
species
Animalia : Mollusca : Bivalvia : Lucinida : Thyasiridae : Conchocele : Conchocele conradiiaragonite
body,trace
37.2 - 33.9 Ma
Paleogene
Archivesica tschudi
species
Animalia : Mollusca : Bivalvia : Veneroidei : Vesicomyidae : Archivesica : Archivesica tschudiaragonite
body,trace
37.2 - 33.9 Ma
Paleogene
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
and/or  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: May 10, 2024 12:27:43
Go to top of page