Anomotodon sheppeyensis

Anomotodon sheppeyensis

Decker, R. · CC0 · via GBIF. 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
AnomotodonPBDB
Diet
carnivorePBDB, for Lamniformes
Life habit
nektonicPBDB, for Lamniformes
Motility
actively mobilePBDB, for Lamniformes

Time the record covers

At most 15 million years on record.

Every occurrence read is dated to somewhere between 56 Mya and 41.03 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Paleocene — about 0 of 12 occurrencesEocene — about 12 of 12 occurrencesEocene57–56 Mya — about 0.0 occurrences56–55 Mya — about 0.5 occurrences55–55 Mya — about 0.5 occurrences55–54 Mya — about 0.5 occurrences54–54 Mya — about 0.5 occurrences54–53 Mya — about 0.5 occurrences53–53 Mya — about 0.5 occurrences53–52 Mya — about 0.5 occurrences52–52 Mya — about 0.5 occurrences52–51 Mya — about 0.5 occurrences51–51 Mya — about 0.5 occurrences51–50 Mya — about 0.5 occurrences50–50 Mya — about 0.5 occurrences50–49 Mya — about 0.5 occurrences49–49 Mya — about 0.5 occurrences49–48 Mya — about 0.5 occurrences48–47 Mya — about 0.3 occurrences47–47 Mya — about 0.3 occurrences47–46 Mya — about 0.3 occurrences46–46 Mya — about 0.3 occurrences46–45 Mya — about 0.3 occurrences45–45 Mya — about 0.3 occurrences45–44 Mya — about 0.3 occurrences44–44 Mya — about 0.3 occurrences44–43 Mya — about 0.3 occurrences43–43 Mya — about 0.3 occurrences43–42 Mya — about 0.3 occurrences42–42 Mya — about 0.3 occurrences42–41 Mya — about 0.3 occurrences41–41 Mya — about 0.0 occurrences56.5 Mya40.5 Mya

12 occurrences of Anomotodon sheppeyensis 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

12 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

4 formations

London Clay — 51.40°N, 0.83°ELondon Clay — 51.51°N, 0.24°ELondon Clay — 51.83°N, 1.25°ELondon Clay — 50.78°N, 0.65°WLondon Clay — 51.64°N, 0.78°EMarnes de Donzacq — 43.75°N, 0.84°WKalinino — 52.51°N, 46.58°ELillebælt Clay — 55.60°N, 9.81°E

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

Anomotodon sheppeyensis and its relatives

Eocene

Where Anomotodon sheppeyensis and its relatives were recorded in the Eocene.

Found in the same rock

322 taxa

The Paleobiology Database records 12 sites for Anomotodon sheppeyensis, 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

Each of the 12 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 content1

Picture of Anomotodon sheppeyensis

Source
GBIF
Credit
Decker, R.
Licence
CC0
Commercial use
the licence allows it

No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.

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

Keep going

What may have been alongside itAnomotodon through timeFormations of the EoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Casier 1966)