Condylarthra
Condylarthra is an informal group – previously considered an order – of extinct placental mammals, known primarily from the Paleocene and Eocene epochs. They are considered early, primitive ungulates and is now largely considered to be a wastebasket taxon, having served as a dumping ground for classifying ungulates which had not been clearly established as part of either Perissodactyla or Artiodactyla, being composed thus of several unrelated lineages.

Dmitry Bogdanov · CC BY-SA 3.0 · via Wikipedia/Commons. 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
- EpitheriaPBDB
- Diet
- insectivorePBDB, for Theria
- Life habit
- scansorialPBDB, for Eutheria
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Eutheria
Time the record covers
At least 25 million years on record.
The record covers at least 63.4 Mya to 37.71 Mya. No occurrence read is dated outside 66 Mya to 33.9 Mya.
1,295 occurrences of Condylarthra 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
1,295 occurrencesThese 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
85 formations
- Willwood Formation400
- Wind River Formation184
- Nacimiento Formation98
- Wasatch Formation92
- Bridger Formation89
- DeBeque Formation88
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The named rock units Condylarthra has been recovered from, largest first. Drawn where the rock is now, not where it formed. 61 further formations hold fewer occurrences each and are not listed. 68 occurrences have no formation on record, which is common for older literature.
Condylarthra and its relatives
EoceneWhere Condylarthra and its relatives were recorded in the Eocene.
Found in the same rock
822 taxa- Hyopsodus97 sites
- Coryphodon65 sites
- Hyracotherium56 sites
- Diacodexis55 sites
- Paramys excavatus49 sites
- Didymictis46 sites
- Esthonyx bisulcatus46 sites
- Phenacodus vortmani43 sites
- Paramys copei41 sites
- Hyopsodus lysitensis39 sites
- Hyopsodus powellianus39 sites
- Phenacodus37 sites
- Phenacolemurinae37 sites
- Sifrhippus grangeri37 sites
- Prototomus35 sites
- Haplomylus speirianus32 sites
- Microsyopidae32 sites
- Promioclaenus acolytus32 sites
- Cantius abditus31 sites
- Cantius30 sites
- Viverravus29 sites
- Prodiacodon tauricinerei27 sites
- Copecion brachypternus26 sites
- Tetraclaenodon puercensis26 sites
The Paleobiology Database records 954 sites for Condylarthra, and this reads 240 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
174 references- Revision of the Wind River faunas, early Eocene of central Wyoming. Part 13. Systematics and phylogenetic pattern of early Eocene Hyopsodus (Mammalia: Condylarthra)246
- Stratigraphy and mammalian paleontology of the McCullough Peaks, northern Bighorn Basin, Wyoming: Implications for biochronology, basin development, and community reorganization across the Paleocene-Eocene boundary233
- Synonymies and reidentifications of North American fossil mammals97
- Faunal Zonation of the Willwood Formation in the Central Bighorn Basin, Wyoming72
- Paleocene vertebrate paleontology of the San Juan Basin, New Mexico36
- Early Eocene Mammalian Fauna of the Piceance Creek Basin. Northwestern Colorado34
- Mammalian Fauna From the Lower Bridger Formation (Bridger A, Early Middle Eocene) of the Southern Green River Basin, Wyoming32
- Revision of the Wind River faunas, early Eocene of central Wyoming. Part 5. Geology and biostratigraphy of the upper part of the Wind River Formation, northeastern Wind River Basin22
- Paleontology and geology of the Bridger Formation, southern Green River Basin, southwestern Wyoming. Part 3. Notes on Hyopsodus22
- Bomburia and Ellipsodon (Mammalia: Mioclaenidae) from the Early Paleocene of New Mexico20
- The "condylarths" (archaic Ungulata, Mammalia) from the early Palaeocene of Tiupampa (Bolivia): implications on the origin of the South American ungulates17
- Stratigraphy, mammalian paleontology, paleoecology, and age correlation of the Wasatch Formation, Fossil Butte National Monument, Wyoming16
Each of the 1,295 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. 162 further references are not listed. 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 content1
Picture of Condylarthra
- Source
- Wikipedia/Commons
- Credit
- Dmitry Bogdanov
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan of Condylarthra was found in MorphoSource and Sketchfab.
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itEpitheria through timeFormations of the EoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Cope 1881)