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A 3594 - San Lorenzo Island, Mulegé Municipality, Baja California Sur, Mexico

Lat/Long (Decimal)27.1,-113.75
Co-ordinates Derivationbased on nearby landmark
Given LocationBaja California Sur, Mexico
Mindat.org Region (for given coordinates)Mulegé Municipality, Baja California Sur, Mexico

Collections

CollectionReferenceStratigraphic NameCommentsLithologyAge
A 3594 - San Lorenzo IslandDurham J. W. (1950)San MarcosFrom well-bedded coarse sandstone dipping northwest, overlain by conglomerates and volcanics. About 200 ft of conglomerate and sandstone dip northwest and are capped with lava. A few fossils are found in thick-bedded sandstone interbedded between conglomerates indicating that at least part of the section is marine.sandstone5.333 - 3.6 Ma
Neogene

Recorded Fossils

Accepted NameHierarchyAge
Encope sp.
genus
Animalia : Echinodermata : Echinoidea : Clypeasteroida : Mellitidae : Encope5.333 - 3.6 Ma
Neogene
Dendostrea vespertina
species
Animalia : Mollusca : Bivalvia : Ostreida : Ostreidae : Dendostrea : Dendostrea vespertina5.333 - 3.6 Ma
Neogene
Argopecten deserti
species
Animalia : Mollusca : Bivalvia : Pectinida : Pectinidae : Argopecten : Argopecten deserti5.333 - 3.6 Ma
Neogene
Argopecten sverdrupi
species
Animalia : Mollusca : Bivalvia : Pectinida : Pectinidae : Argopecten : Argopecten sverdrupi5.333 - 3.6 Ma
Neogene
Argopecten ventricosus
species
Animalia : Mollusca : Bivalvia : Pectinida : Pectinidae : Argopecten : Argopecten ventricosus5.333 - 3.6 Ma
Neogene
Euvola keepi
species
Animalia : Mollusca : Bivalvia : Pectinida : Pectinidae : Euvola : Euvola keepi5.333 - 3.6 Ma
Neogene

References

Durham J. W. (1950) 1940 E.W. Scripps cruise to the Gulf of California. Part II - Megascopic paleontology and marine stratigraphy, Geological Society of America Memoir 43 2
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!
 
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