Leptictis dakotensis
via iDigBio · CC0 · 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
- LeptictisPBDB
- Diet
- insectivore, carnivorePBDB, for Leptictidae
- Life habit
- ground dwellingPBDB, for Leptictidae
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Eutheria
Time the record covers
At least 2.1 million years on record.
The record covers at least 33.9 Mya to 31.8 Mya. No occurrence read is dated outside 37 Mya to 29.5 Mya.
11 occurrences of Leptictis dakotensis on record, most of them in the Oligocene. 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
11 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
2 formations
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The named rock units Leptictis dakotensis has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Leptictis dakotensis and its relatives
OligoceneWhere Leptictis dakotensis and its relatives were recorded in the Oligocene.
Found in the same rock
177 taxa- Palaeolagus haydeni9 sites
- Megalagus turgidus8 sites
- Hyaenodon horridus7 sites
- Merycoidodon culbertsonii7 sites
- Hesperocyon gregarius6 sites
- Hyaenodon crucians6 sites
- Leptomeryx evansi5 sites
- Eumys elegans4 sites
- Hypertragulus calcaratus4 sites
- Ischyromys4 sites
- Miniochoerus chadronensis4 sites
- Poebrotherium eximium4 sites
- Poebrotherium wilsoni4 sites
- Willeumys viduus4 sites
- Brontotheriidae3 sites
- Daphoenus3 sites
- Ischyromys typus3 sites
- Leptomeryx speciosus3 sites
- Palaeolagus intermedius3 sites
- Poebrotherium3 sites
- Centetodon magnus2 sites
- Dinictis2 sites
- Dinictis felina2 sites
- Domnina gradata2 sites
The Paleobiology Database records 11 sites for Leptictis dakotensis, 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
7 references- Elocene-Oligocene climatic change in North America: The White River Formation near Douglass, East-Central Wyoming5
- Fossil mammals from ant mounds situated on exposures of the Big Cottonwood Creek Member of the Chadron Formation (latest Eocene - Early Oligocene), Sioux County, Nebraska1
- Synonymies and reidentifications of North American fossil mammals1
- Vertebrate fossil record, age, and paleoenvironmental setting of the Brule Formation (Oligocene) in North Dakota1
- Geology and paleontology of the Oligocene Harris Ranch Badlands, southwestern South Dakota1
- Geology, paleoecology, and paleoclimatology of the Chadron Formation1
- The Faunas of the Concretionary Zones of the Oreodon Beds, White River Oligocene1
Each of the 11 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. Each entry links to the Paleobiology Database's own record for the work.
Media and terms
Media content1
Picture of Leptictis dakotensis
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Leptictis dakotensis was found in Sketchfab.
Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itLeptictis through timeFormations of the OligoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Leidy 1868)