Crypholestes vaughni

via iDigBio · via iDigBio. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- CrypholestesPBDB
- Diet
- insectivorePBDB, for Theria
- Life habit
- scansorialPBDB, for Eutheria
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Eutheria
Time the record covers
At most 8.9 million years on record.
Every occurrence read is dated to somewhere between 45.9 Mya and 37 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
31 occurrences of Crypholestes vaughni on record, most of them in the Eocene. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
31 occurrences- Eocene100%
These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
3 formations
- Friars Formation · La Jolla Group29
- Santiago Formation1
- Stadium Formation1
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The named rock units Crypholestes vaughni has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Crypholestes vaughni and its relatives
EoceneWhere Crypholestes vaughni and its relatives were recorded in the Eocene.
Found in the same rock
85 taxa- Sciuravus powayensis28 sites
- Microparamys minutus24 sites
- Uintasorex montezumicus23 sites
- Herpetotherium knighti22 sites
- Patriolestes novaceki21 sites
- Metanoiamys agorus19 sites
- Batodonoides powayensis16 sites
- Peradectes16 sites
- Aethomylos simplicidens14 sites
- Pareumys grangeri14 sites
- Washakius woodringi14 sites
- Centetodon aztecus13 sites
- Omomys carteri10 sites
- Glyptosaurinae9 sites
- Omomyidae9 sites
- Peradectes californicus7 sites
- Chiroptera6 sites
- Metanoiamys6 sites
- Nyctitherium6 sites
- Parasauromalus olseni6 sites
- Tinosaurus stenodon6 sites
- Apatemys bellus5 sites
- Iguanidae5 sites
- Leptoreodon major5 sites
The Paleobiology Database records 31 sites for Crypholestes vaughni, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
4 references- Eocene mammal faunas of San Diego County17
- Summary of known occurrences of terrestrial vertebrates from Eocene strata of southern California12
- New specimens of Metanoiamys, Pauromys, and Simimys (Rodentia: Myomorpha) from the Uintan (middle Eocene) of San Diego County, California, and comments on the relationships of selected Paleogene Myomorpha1
- Middle Eocene mammal faunas of San Diego County, California1
Each of the 31 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content2

Picture of Crypholestes vaughni
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
CT scan
- Source
- MorphoSource
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Crypholestes vaughni · sdsnh:43516
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itCrypholestes through timeFormations of the EoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Novacek 1976)