Dioplotherium manigaulti

Dioplotherium manigaulti

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
DioplotheriumPBDB
Diet
herbivorePBDB, for Dugongidae
Life habit
aquaticPBDB, for Sirenia
Motility
actively mobilePBDB, for Osteichthyes
Environment
marinePBDB, for Sirenia

Time the record covers

At least 7 million years on record.

The record covers at least 23.04 Mya to 15.98 Mya. No occurrence read is dated outside 27.3 Mya to 13.82 Mya.

Oligocene — about 2 of 6 occurrencesOligoceneMiocene — about 4 of 6 occurrencesMiocene27–27 Mya — about 0.2 occurrences27–26 Mya — about 0.2 occurrences26–26 Mya — about 0.2 occurrences26–25 Mya — about 0.2 occurrences25–25 Mya — about 0.2 occurrences25–24 Mya — about 0.2 occurrences24–24 Mya — about 0.2 occurrences24–23 Mya — about 0.2 occurrences23–23 Mya — about 0.2 occurrences23–22 Mya — about 0.1 occurrences22–22 Mya — about 0.1 occurrences22–22 Mya — about 0.1 occurrences22–21 Mya — about 0.1 occurrences21–21 Mya — about 0.1 occurrences21–20 Mya — about 0.1 occurrences20–20 Mya — about 0.1 occurrences20–19 Mya — about 0.1 occurrences19–19 Mya — about 0.1 occurrences19–18 Mya — about 0.1 occurrences18–18 Mya — about 0.1 occurrences18–17 Mya — about 0.1 occurrences17–17 Mya — about 0.1 occurrences17–16 Mya — about 0.1 occurrences16–16 Mya — about 0.3 occurrences16–15 Mya — about 0.4 occurrences15–15 Mya — about 0.4 occurrences15–14 Mya — about 0.4 occurrences14–14 Mya — about 0.4 occurrences23.04 Mya15.98 Mya27.8 Mya13.3 Mya

6 occurrences of Dioplotherium manigaulti on record, most of them in the Miocene. 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

6 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

3 formations

Statenville — 30.68°N, 82.71°WStatenville — 30.40°N, 83.00°WParachucla — 30.33°N, 82.73°WChandler Bridge — 32.93°N, 79.83°W

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The named rock units Dioplotherium manigaulti has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.

Dioplotherium manigaulti and its relatives

Miocene

Where Dioplotherium manigaulti and its relatives were recorded in the Miocene.

Found in the same rock

22 taxa

The Paleobiology Database records 6 sites for Dioplotherium manigaulti, and this reads all of them. The number is how many of those sites it was catalogued from too.

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 6 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 Dioplotherium manigaulti

Source
iDigBio
Credit
via iDigBio
Licence
CC0
Commercial use
the licence allows it

No 3D scan of Dioplotherium manigaulti 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.

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

Keep going

What may have been alongside itDioplotherium through timeFormations of the MioceneThe world it lived on

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