Anaptomorphinae

Anaptomorphinae is a pre-historic group of primates known from Eocene fossils in North America and Europe and later periods of Paleocene Asia, and are a sub-family of omomyids. The anaptomorphines is a paraphyletic group consisting of the two tribes Trogolemurini and Anaptomorphini. Anaptomorphine radiation in Wyoming, one of the most detailed records of changes within populations and between species in the fossil record, has provided remarkable evidence of transitional fossils.

Anaptomorphinae

Ambrosius Hubrecht · 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
OmomyidaePBDB
Diet
insectivorePBDB, for Omomyidae
Life habit
arborealPBDB, for Omomyidae
Motility
actively mobilePBDB, for Osteichthyes
Environment
terrestrialPBDB, for Omomyidae

Time the record covers

At least 17 million years on record.

The record covers at least 51.1 Mya to 33.9 Mya. No occurrence read is dated outside 56 Mya to 27.3 Mya.

Paleocene — about 0 of 276 occurrencesEocene — about 275 of 276 occurrencesEoceneOligocene — about 1 of 276 occurrencesOligocene57–56 Mya — about 19 occurrences56–55 Mya — about 45 occurrences55–54 Mya — about 45 occurrences54–53 Mya — about 45 occurrences53–52 Mya — about 45 occurrences52–51 Mya — about 26 occurrences51–50 Mya — about 8 occurrences50–49 Mya — about 8 occurrences49–48 Mya — about 8 occurrences48–47 Mya — about 7 occurrences47–46 Mya — about 6 occurrences46–45 Mya — about 2 occurrences45–44 Mya — about 2 occurrences44–43 Mya — about 2 occurrences43–42 Mya — about 2 occurrences42–41 Mya — about 2 occurrences41–40 Mya — about 2 occurrences40–39 Mya — about 0.4 occurrences39–38 Mya — about 0.4 occurrences38–37 Mya — about 0.3 occurrences37–36 Mya — about 0.0 occurrences36–35 Mya — about 0.0 occurrences35–34 Mya — about 0.1 occurrences34–33 Mya — about 0.2 occurrences33–32 Mya — about 0.2 occurrences32–31 Mya — about 0.2 occurrences31–30 Mya — about 0.2 occurrences30–29 Mya — about 0.2 occurrences29–28 Mya — about 0.2 occurrences28–27 Mya — about 0.1 occurrences51.1 Mya33.9 Mya56.6 Mya26.7 Mya

276 occurrences of Anaptomorphinae 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

276 occurrences

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

17 formations

Willwood — 44.00°N, 108.00°WWillwood — 44.50°N, 108.00°WWillwood — 44.59°N, 108.41°WWillwood — 44.51°N, 108.68°WWillwood — 44.30°N, 109.00°WWillwood — 44.59°N, 108.86°WWillwood — 44.44°N, 108.63°WWillwood — 44.56°N, 108.70°WWillwood — 44.59°N, 108.62°WWillwood — 44.53°N, 108.79°WWillwood — 44.53°N, 108.43°WWillwood — 44.53°N, 108.32°WWillwood — 44.65°N, 108.72°WWillwood — 44.61°N, 108.50°WWillwood — 44.52°N, 108.57°WWillwood — 44.39°N, 108.71°WWillwood — 44.41°N, 108.79°WWillwood — 44.33°N, 108.77°WWillwood — 44.58°N, 108.81°WWillwood — 44.66°N, 108.79°WWillwood — 44.66°N, 108.85°WWillwood — 44.23°N, 108.42°WWasatch — 40.60°N, 108.10°WWasatch — 41.70°N, 109.00°WWasatch — 42.70°N, 110.10°WWasatch — 41.80°N, 110.70°WWasatch — 41.75°N, 108.00°WWasatch — 42.37°N, 108.91°WWasatch — 42.53°N, 108.72°WWasatch — 41.53°N, 108.56°WBridger — 41.70°N, 109.00°WBridger — 41.20°N, 110.50°WBridger — 42.70°N, 110.10°WBridger — 41.80°N, 110.70°WBridger — 41.77°N, 110.33°WBridger — 42.37°N, 108.91°WWind River — 44.00°N, 106.60°WWind River — 43.20°N, 108.20°WWind River — 43.20°N, 107.10°WWind River — 43.20°N, 107.33°WWind River — 41.02°N, 109.68°WWagon Bed ("Tepee Trail") — 43.20°N, 107.10°WDeBeque — 39.70°N, 107.60°WSantiago — 33.19°N, 117.32°WSantiago — 32.90°N, 117.10°WSantiago — 33.11°N, 117.27°WHuerfano — 37.80°N, 105.10°WGreen River — 40.24°N, 109.13°WGreen River — 40.20°N, 109.90°W"Wasatch" — 44.00°N, 106.60°WMission Valley — 32.90°N, 117.10°WGolden Valley — 46.90°N, 102.80°WIndian Meadows — 43.20°N, 108.20°WAycross — 43.70°N, 108.70°WSespe — 34.30°N, 119.00°WJebel Qatrani — 29.45°N, 30.58°ECypress Hills — 50.20°N, 107.60°W

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The named rock units Anaptomorphinae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 6 occurrences have no formation on record, which is common for older literature.

Anaptomorphinae and its relatives

Eocene

Where Anaptomorphinae and its relatives were recorded in the Eocene.

Found in the same rock

822 taxa

The Paleobiology Database records 229 sites for Anaptomorphinae, 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

49 references

Each of the 276 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. 37 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 Anaptomorphinae

Credit
Ambrosius Hubrecht
Licence
Public Domain
Commercial use
the licence allows it

No 3D scan of Anaptomorphinae 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

Occurrence data from the Paleobiology Database, CC BY 4.0. (Cope 1883)