Campanorco inauguralis

Campanorco is an extinct genus of notoungulate mammal from the Middle Eocene Lumbrera Formation, Argentina, South America and the only member of the family Campanorcidae. It contains only a single species, Campanorco inauguralis.

Campanorco inauguralis

Rodrigues, H. G.; Cornette, R. ; Clavel, J.; Cassini, G.; Bhart-Anjan, S. B.; Fernández-Monescillo, M., Moreno, K.; H… · CC BY 4.0 · 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
CampanorcoPBDB
Diet
herbivorePBDB, for Notoungulata
Life habit
scansorialPBDB, for Eutheria
Motility
actively mobilePBDB, for Osteichthyes
Environment
terrestrialPBDB, for Eutheria

Time the record covers

At most 8 million years on record.

The one occurrence read is dated to somewhere between 56 Mya and 48.07 Mya, which is a dating window rather than a span.

Paleocene — about 0 of 1 occurrenceEocene — about 1 of 1 occurrenceEocene56–56 Mya — about 0.0 occurrences56–56 Mya — about 0.0 occurrences56–55 Mya — about 0.0 occurrences55–55 Mya — about 0.0 occurrences55–55 Mya — about 0.0 occurrences55–54 Mya — about 0.0 occurrences54–54 Mya — about 0.0 occurrences54–54 Mya — about 0.0 occurrences54–54 Mya — about 0.0 occurrences54–53 Mya — about 0.0 occurrences53–53 Mya — about 0.0 occurrences53–53 Mya — about 0.0 occurrences53–52 Mya — about 0.0 occurrences52–52 Mya — about 0.0 occurrences52–52 Mya — about 0.0 occurrences52–51 Mya — about 0.0 occurrences51–51 Mya — about 0.0 occurrences51–51 Mya — about 0.0 occurrences51–51 Mya — about 0.0 occurrences51–50 Mya — about 0.0 occurrences50–50 Mya — about 0.0 occurrences50–50 Mya — about 0.0 occurrences50–49 Mya — about 0.0 occurrences49–49 Mya — about 0.0 occurrences49–49 Mya — about 0.0 occurrences49–48 Mya — about 0.0 occurrences48–48 Mya — about 0.0 occurrences48–48 Mya — about 0.0 occurrences56.5 Mya47.6 Mya

1 occurrence of Campanorco inauguralis 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

1 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

1 formation

Lumbrera — 25.95°S, 65.60°W

Loading coastlines…

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

Campanorco inauguralis and its relatives

Eocene

Where Campanorco inauguralis and its relatives were recorded in the Eocene.

Found in the same rock

No other named taxon is catalogued from that site.

The Paleobiology Database records 1 site for Campanorco inauguralis, and this reads all of them.

Entered from

1 reference

Each of the 1 occurrence 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 the Paleobiology Database's own record for the work.

Media and terms

Media content1

Picture of Campanorco inauguralis

Credit
Rodrigues, H. G.; Cornette, R. ; Clavel, J.; Cassini, G.; Bhart-Anjan, S. B.; Fernández-Monescillo, M., Moreno, K.; H…
Licence
CC BY 4.0
Commercial use
the licence allows it

No 3D scan of Campanorco inauguralis was found in Sketchfab.

Smithsonian Open Access and MorphoSource were 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

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

Occurrence data from the Paleobiology Database, CC BY 4.0. Bond et al. 1984