The San Jose Formation is an
Early Eocene
In the geologic timescale the Ypresian is the oldest age (geology), age or lowest stage (stratigraphy), stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by th ...
(
Wasatchian
The Wasatchian North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 55,400,000 to 50,300,000 years BP lasting .
It is usually c ...
in the
NALMA classification)
geologic formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ...
in the
San Juan Basin
The San Juan Basin is a geologic structural basin located near the Four Corners region of the Southwestern United States. The basin covers 7,500 square miles and resides in northwestern New Mexico, southwestern Colorado, and parts of Utah ...
of
New Mexico
)
, population_demonym = New Mexican ( es, Neomexicano, Neomejicano, Nuevo Mexicano)
, seat = Santa Fe, New Mexico, Santa Fe
, LargestCity = Albuquerque, New Mexico, Albuquerque
, LargestMetro = Albuquerque metropolitan area, Tiguex
, Offi ...
and
Colorado
Colorado (, other variants) is a state in the Mountain states, Mountain West subregion of the Western United States. It encompasses most of the Southern Rocky Mountains, as well as the northeastern portion of the Colorado Plateau and the wes ...
.
[San Jose Formation]
at Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database, a large relational database assembled by hundreds of paleontologists from around the world.
History
Fossilworks was cre ...
.org
Description

The San Jose Formation is mostly
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
but with some
mudstone beds. The formation was deposited by high-energy streams on a muddy floodplain that was the last preserved sedimentation episode in the San Juan Basin. Stream direction was from the northwest, north, and east towards the south.
The basal Cuba Mesa Member is found throughout the depositional basin and is a coarse-grained sheet sandstone. The Regina Member is floodplain mudstone and disconnected sheet sandstone that intertongues with the sandstone-dominated Ditch Canyon Member in the northwestern part of the basin and the Llaves Member on the east side of the basin. The uppermost member is the
siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, ...
-dominated Tapicitos Member. The Cuba Mesa Member was deposited during subsidence in the basin center, while the later members were deposited during episodes of
monoclinal folding along the
Nacimiento Fault Nacimiento may refer to:
Settlements
* Nacimiento, Chile, a municipality in the province of Bío Bío, region of Bío Bío, Chile
*Nacimiento, Spain, a municipality in the province of Almería, Andalusia, Spain
* Nacimiento, California, United Stat ...
on the west escarpment of the
Nacimiento Mountains
The Sierra Nacimiento (official name), or Nacimiento Mountains, are a mountain range in the northwestern part of the U.S. state of New Mexico. They are just west of the more prominent Jemez Mountains near the town of Cuba, and are separated ...
.
Paleontology
The mudstone beds of the San Jose Formation are locally rich in fossils. These include the Almagre and Largo faunas of the early Eocene.
Fossil content
Among others, the following fossils have been reported from the formation:
[
]
Mammals
;Primates
* '' Copelemur tutus''
* '' Cantius angulatus''
* '' C. frugivorus''
* '' Microsyops angustidens''
* '' M. latidens''
* Omomyidae indet.
;Artiodactyls
* '' Bunophorus grangeri''
* '' Diacodexis cf. metsiacus''
* '' Simpsonodus chacensis''
;Carnivora
* '' Vulpavus australis''
;Cimolesta
* '' Esthonyx bisulcatus''
;Ferae
* '' Ambloctonus sinosus''
* '' Oxyaena lupina''
* '' O. simpsoni''
;Glires
* '' Knightomys depressus''
* '' K. reginensis''
* '' Paramys copei''
* '' P. nini''
;Hyaenodonta
* Hyaenodontidae indet.
;Insectivora
* '' Apatemys bellulus''
;Pantodonta
* '' Coryphodon armatus''
;Perissodactyla
* '' Eohippus angustidens''
* '' Systemodon tapirinus''
* '' Xenicohippus osborni''
;Placentalia
* '' Copecion brachypternus''
* '' Hyopsodus lysitensis''
* '' Hyopsodus cf. mentalis''
* '' Hyopsodus minor''
* '' Meniscotherium chamense''
* '' M. tapiacitum''
* '' Hyopsodus sp.''
;Taeniodonta
* ''Ectoganus gliriformis
''Ectoganus'' is a fossil genus of mammals belonging to the family Stylinodontidae.
The species of this genus are found in Northern America.
Species:
* ''Ectoganus bighornensis'' Schoch, 1981
* ''Ectoganus copei
''Ectoganus'' is a fossil ge ...
''
;Theriiformes
* Creodonta indet.
Reptiles
;Snakes
* '' Cheilophis huerfanoensis''
* ''Saniwa ensidens
''Saniwa'' is an extinct genus of varanid lizard that lived about 48 million years ago during the Eocene epoch. It is known from well-preserved fossils found in the Bridger and Green River Formations of Wyoming. The type species ''S. ensidens'' ...
''
* '' Sanjuanophis froehlichi''
* '' cf. Calamagras primus''
* '' cf. Saniwa sp.''
;Turtles
* ''Baena arenosa
''Baena'' is an extinct genus of baenid turtles.
Fossils of ''Baena'' have been found in locations including Kirtland Formation, Campanian New Mexico (''B.'' sp.) (Cretaceous) and Ravenscrag Formation, Maastrichtian Canada
Canada is a ...
''
* '' Baptemys garmanii''
* '' Echmatemys lativertebralis''
* '' Hadrianus majusculus''
* '' Planetochelys dithyros''
* '' Trionyx leptomitus''
* '' Baltemys sp.''
* Chelydridae indet.
* Trionychidae indet.
;Lizards
* '' Paraglyptosaurus cf. yatkolai''
* Lacertilia indet.
History of investigation
In late 1874, Edward Drinker Cope
Edward Drinker Cope (July 28, 1840 – April 12, 1897) was an American zoologist, paleontologist, comparative anatomist, herpetologist, and ichthyologist. Born to a wealthy Quaker family, Cope distinguished himself as a child prodigy intereste ...
was a member of the Wheeler Survey
The Wheeler Survey, carried out in 1872-1879, was one of the "Four Great Surveys" conducted by the US government after the Civil War primarily to document the geology and natural resources of the American West. Supervised by First Lieutenant (lat ...
but ignored orders from Wheeler to proceed north from the Chama River to Colorado
Colorado (, other variants) is a state in the Mountain states, Mountain West subregion of the Western United States. It encompasses most of the Southern Rocky Mountains, as well as the northeastern portion of the Colorado Plateau and the wes ...
. Instead, he headed south to explore the area north of the San Pedro Mountains
The Sierra Nacimiento (official name), or Nacimiento Mountains, are a mountain range in the northwestern part of the U.S. state of New Mexico. They are just west of the more prominent Jemez Mountains near the town of Cuba, and are separated from ...
, where fossils had been reported. He found early Eocene fossils in the badlands north of Regina, New Mexico
Regina is a census-designated place (CDP)) in Sandoval County, New Mexico, United States. The population was 99 at the 2000 census. It is part of the Albuquerque Metropolitan Statistical Area. It was named for Regina, Saskatchewan.
Geograph ...
and spent about seven weeks collecting fishes, reptiles, and what was then the oldest known mammal fossils in North America. He also collected the fossil of a giant flightless bird. Cope later wrote his father that this was "the most important find in geology I have ever made".
In 1948, G.G. Simpson visited the same area and assigned the fossil beds to the San Jose Formation. In 1967, the formation was divided (in ascending order) into the Cuba Mesa Member, Regina Member, Llaves Member, and Tapicitos Member.
See also
* List of fossiliferous stratigraphic units in Colorado
This article contains a list of fossil-bearing stratigraphic units in the state of Colorado, U.S.
Sites
See also
* Paleontology in Colorado
References
*
{{DEFAULTSORT:Fossiliferous stratigraphic units in Colorado
Colorado
Co ...
* List of fossiliferous stratigraphic units in New Mexico
This article contains a list of fossil-bearing stratigraphic units in the state of New Mexico, U.S.
Sites
See also
* Paleontology in New Mexico
References
*
{{DEFAULTSORT:Fossiliferous stratigraphic units in New Mexico
New Mexico
...
* Paleontology in Colorado
The location of the state of Colorado
Paleontology in Colorado refers to paleontological research occurring within or conducted by people from the U.S. state of Colorado.
The geologic column of Colorado spans about one third of Earth's history. ...
* Paleontology in New Mexico
Paleontology in New Mexico refers to paleontological research occurring within or conducted by people from the U.S. state of New Mexico. The fossil record of New Mexico is exceptionally complete and spans almost the entire stratigraphic colu ...
References
Bibliography
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{{Chronostratigraphy of Colorado, Cenozoic state=expanded
Geologic formations of Colorado
Paleogene formations of New Mexico
Eocene Series of North America
Paleogene Colorado
Ypresian Stage
Wasatchian
Sandstone formations of the United States
Fluvial deposits
Paleontology in New Mexico