Crenatosiren olseni

Crenatosiren olseni

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

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 11 occurrencesOligocene — about 11 of 11 occurrencesOligoceneMiocene — about 0 of 11 occurrences34–34 Mya — about 0.2 occurrences34–33 Mya — about 0.2 occurrences33–33 Mya — about 0.2 occurrences33–32 Mya — about 0.2 occurrences32–32 Mya — about 0.2 occurrences32–32 Mya — about 0.2 occurrences32–31 Mya — about 0.2 occurrences31–31 Mya — about 0.2 occurrences31–30 Mya — about 0.2 occurrences30–30 Mya — about 0.2 occurrences30–30 Mya — about 0.2 occurrences30–29 Mya — about 0.2 occurrences29–29 Mya — about 0.2 occurrences29–28 Mya — about 0.2 occurrences28–28 Mya — about 0.2 occurrences28–28 Mya — about 0.2 occurrences28–27 Mya — about 0.3 occurrences27–27 Mya — about 0.7 occurrences27–26 Mya — about 0.7 occurrences26–26 Mya — about 0.7 occurrences26–26 Mya — about 0.7 occurrences26–25 Mya — about 0.7 occurrences25–25 Mya — about 0.7 occurrences25–25 Mya — about 0.7 occurrences25–24 Mya — about 0.7 occurrences24–24 Mya — about 0.7 occurrences24–23 Mya — about 0.7 occurrences23–23 Mya — about 0.5 occurrences34.4 Mya22.5 Mya

11 occurrences of Crenatosiren olseni 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

11 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

Chandler Bridge — 32.97°N, 80.15°WChandler Bridge — 32.85°N, 80.40°WChandler Bridge — 32.85°N, 80.08°WChandler Bridge — 33.01°N, 80.06°WAshley — 32.97°N, 80.20°WAshley — 32.84°N, 80.39°WAshley — 32.83°N, 79.99°WParachucla — 30.34°N, 82.78°WBelgrade — 34.57°N, 77.27°W

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

Crenatosiren olseni and its relatives

Oligocene

Where Crenatosiren olseni and its relatives were recorded in the Oligocene.

Found in the same rock

55 taxa

The Paleobiology Database records 11 sites for Crenatosiren olseni, 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

2 references

Each of the 11 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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content2

Picture of Crenatosiren olseni

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

3D model

Source
Sketchfab
Licence
CC Attribution-NonCommercial-NoDerivs
Commercial use
the licence does not allow it

Smithsonian Open Access and MorphoSource were 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

Occurrence data from the Paleobiology Database, CC BY 4.0. (Reinhart 1976)