Isisaurus colberti

Isisaurus is a genus of titanosaurian dinosaur from the Late Cretaceous Lameta Formation of India and Pab Formation of Pakistan. The genus contains a single species, Isisaurus colberti.

Isisaurus colberti

Ansh Saxena · CC BY-SA 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
IsisaurusPBDB
Diet
herbivorePBDB, for Sauropoda
Life habit
ground dwelling, gregariousPBDB, for Sauropoda
Motility
actively mobilePBDB, for Sauropoda
Environment
terrestrialPBDB, for Sauropoda

Time the record covers

At most 6.2 million years on record.

Every occurrence read is dated to somewhere between 72.2 Mya and 66 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Late Cretaceous — about 4 of 4 occurrencesLate CretaceousPaleocene — about 0 of 4 occurrences72–72 Mya — about 0.1 occurrences72–72 Mya — about 0.2 occurrences72–72 Mya — about 0.2 occurrences72–71 Mya — about 0.2 occurrences71–71 Mya — about 0.2 occurrences71–71 Mya — about 0.2 occurrences71–71 Mya — about 0.2 occurrences71–70 Mya — about 0.2 occurrences70–70 Mya — about 0.2 occurrences70–70 Mya — about 0.2 occurrences70–70 Mya — about 0.2 occurrences70–69 Mya — about 0.2 occurrences69–69 Mya — about 0.2 occurrences69–69 Mya — about 0.2 occurrences69–69 Mya — about 0.2 occurrences69–68 Mya — about 0.2 occurrences68–68 Mya — about 0.2 occurrences68–68 Mya — about 0.2 occurrences68–68 Mya — about 0.2 occurrences68–67 Mya — about 0.2 occurrences67–67 Mya — about 0.2 occurrences67–67 Mya — about 0.2 occurrences67–67 Mya — about 0.2 occurrences67–66 Mya — about 0.2 occurrences66–66 Mya — about 0.2 occurrences66–66 Mya — about 0.1 occurrences72.7 Mya65.5 Mya

4 occurrences of Isisaurus colberti on record, most of them in the Late Cretaceous. 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

4 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

Lameta — 21.18°N, 80.37°ELameta — 21.42°N, 78.00°EVitakri — 29.71°N, 69.49°EVitakri — 29.70°N, 69.40°E

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

Isisaurus colberti and its relatives

Late Cretaceous

Where Isisaurus colberti and its relatives were recorded in the Late Cretaceous.

Found in the same rock

20 taxa

The Paleobiology Database records 4 sites for Isisaurus colberti, 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 4 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 Isisaurus colberti

Credit
Ansh Saxena
Licence
CC BY-SA 4.0
Commercial use
the licence allows it

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

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 itIsisaurus through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Jain and Bandyopadhyay 1997)