Bothriogenys fraasi

Bothriogenys fraasi

via iDigBio · CC BY · 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
BothriogenysPBDB
Diet
browserPBDB, for Anthracotheriidae
Life habit
ground dwellingPBDB, for Anthracotheriidae
Motility
actively mobilePBDB, for Osteichthyes
Environment
terrestrialPBDB, for Artiodactyla

Time the record covers

At most 11 million years on record.

Every occurrence read is dated to somewhere between 33.9 Mya and 23.04 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Eocene — about 0 of 5 occurrencesOligocene — about 5 of 5 occurrencesOligoceneMiocene — about 0 of 5 occurrences34–34 Mya — about 0.2 occurrences34–33 Mya — about 0.3 occurrences33–33 Mya — about 0.3 occurrences33–32 Mya — about 0.3 occurrences32–32 Mya — about 0.3 occurrences32–32 Mya — about 0.3 occurrences32–31 Mya — about 0.3 occurrences31–31 Mya — about 0.3 occurrences31–30 Mya — about 0.3 occurrences30–30 Mya — about 0.3 occurrences30–30 Mya — about 0.3 occurrences30–29 Mya — about 0.3 occurrences29–29 Mya — about 0.3 occurrences29–28 Mya — about 0.3 occurrences28–28 Mya — about 0.3 occurrences28–28 Mya — about 0.3 occurrences28–27 Mya — about 0.3 occurrences27–27 Mya — about 0.0 occurrences27–26 Mya — about 0.0 occurrences26–26 Mya — about 0.0 occurrences26–26 Mya — about 0.0 occurrences26–25 Mya — about 0.0 occurrences25–25 Mya — about 0.0 occurrences25–25 Mya — about 0.0 occurrences25–24 Mya — about 0.0 occurrences24–24 Mya — about 0.0 occurrences24–23 Mya — about 0.0 occurrences23–23 Mya — about 0.0 occurrences34.4 Mya22.5 Mya

5 occurrences of Bothriogenys fraasi 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

5 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

2 formations

Jebel Qatrani — 29.43°N, 30.58°EJebel Qatrani — 29.45°N, 30.58°EJebel Qatrani — 29.65°N, 30.58°EShumaysi — 21.68°N, 39.75°E

Loading coastlines…

The named rock units Bothriogenys fraasi has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Bothriogenys fraasi and its relatives

Oligocene

Where Bothriogenys fraasi and its relatives were recorded in the Oligocene.

Found in the same rock

51 taxa

The Paleobiology Database records 5 sites for Bothriogenys fraasi, 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

3 references

Each of the 5 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 Bothriogenys fraasi

Source
iDigBio
Credit
via iDigBio
Licence
CC BY
Commercial use
the licence allows it

CT scan

Licence
not stated by the source
Commercial use
cannot be read from the licence given — check the record
Specimen
Bothriogenys fraasi · dpc:23943

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itBothriogenys through timeFormations of the OligoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Schmidt 1913)