Leptictida
Leptictida is a possibly paraphyletic extinct order of eutherian mammals. Their classification is contentious: according to cladistic studies, they may be (distantly) related to Euarchontoglires, although they are more recently regarded as the first branch to split from basal eutherians. One recent large-scale cladistic analysis of eutherian mammals favored lepictidans as close to the placental crown-clade; and several other recent analyses that included data from Cretaceous non-eutherian mammals found Leptictis to belong to the superorder Afrotheria.
LadyofHats · Public Domain · 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
- EutheriaPBDB
- Diet
- insectivorePBDB, for Theria
- Life habit
- scansorialPBDB, for Eutheria
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Eutheria
Time the record covers
At least 40 million years on record.
The record covers at least 72.2 Mya to 31.8 Mya. No occurrence read is dated outside 83.6 Mya to 29.5 Mya.
458 occurrences of Leptictida on record, most of them in the Eocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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
458 occurrences- Late Cretaceous21%
- Paleocene20%
- Eocene52%
- Oligocene6%
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
65 formations
- Willwood Formation88
- Fort Union Formation46
- Hell Creek Formation · Montana Group35
- Wasatch Formation29
- Lance Formation22
- Wind River Formation20
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The named rock units Leptictida has been recovered from, largest first. Drawn where the rock is now, not where it formed. 41 further formations hold fewer occurrences each and are not listed. 50 occurrences have no formation on record, which is common for older literature.
Leptictida and its relatives
EoceneWhere Leptictida and its relatives were recorded in the Eocene.
Found in the same rock
1,732 taxa- Coryphodon54 sites
- Hyopsodus53 sites
- Phenacolemurinae46 sites
- Meniscoessus robustus42 sites
- Prodiacodon tauricinerei41 sites
- Paramys excavatus39 sites
- Cimolodon nitidus38 sites
- Diacodexis36 sites
- Phenacodus vortmani36 sites
- Didelphodon vorax34 sites
- Paramys copei34 sites
- Haplomylus speirianus32 sites
- Didelphodus absarokae31 sites
- Phenacodus31 sites
- Didymictis30 sites
- Mesodma thompsoni30 sites
- Sifrhippus grangeri30 sites
- Gypsonictops hypoconus29 sites
- Prototomus29 sites
- Pediomys elegans28 sites
- Gypsonictops illuminatus27 sites
- Lepisosteus occidentalis27 sites
- Scapherpeton tectum27 sites
- Thryptacodon antiquus27 sites
The Paleobiology Database records 364 sites for Leptictida, 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
150 references- Synonymies and reidentifications of North American fossil mammals43
- Faunal Zonation of the Willwood Formation in the Central Bighorn Basin, Wyoming32
- Stratigraphy and mammalian paleontology of the McCullough Peaks, northern Bighorn Basin, Wyoming: Implications for biochronology, basin development, and community reorganization across the Paleocene-Eocene boundary28
- Origin and evolution of the Pseudorhyncocyonidae, a European Paleogene family of insectivorous placental mammals20
- Fossil mammals of the type Lance Formation, Wyoming. Part III. Eutheria and summary18
- The Clarkforkian Land-Mammal Age and Mammalian Faunal Composition Across the Paleocene-Eocene Boundary16
- Paleontology and biostratigraphy of lower part of Polecat Bench Formation, southern Bighorn Basin, Wyoming14
- The Bug Creek problem and the Cretaceous-Tertiary transition at McGuire Creek, Montana12
- Distribution and stratigraphic correlation of upper Paleocene and lower Eocene fossil mammal and plant localities of the Fort Union, Willwood, and Tatman formations, southern Bighorn Basin, Wyoming12
- Early Eocene Mammalian Fauna of the Piceance Creek Basin. Northwestern Colorado12
- The Tiffanian Land-Mammal Age (middle and late Paleocene) in the northern Bighorn Basin, Wyoming9
- 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 Basin8
Each of the 458 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. 138 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 Leptictida
- Source
- Wikipedia/Commons
- Credit
- LadyofHats
- Licence
- Public Domain
- Commercial use
- the licence allows it
No 3D scan of Leptictida 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.
The description on this site
- Source
- Wikipedia, “Leptictida”
- 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 itEutheria through timeFormations of the EoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (McKenna 1975)