Cretacocarcinus smithi

No picture of Cretacocarcinus smithi was found. Wikidata and iDigBio were searched and had none. Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cretacocarcinus smithi, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
CretacocarcinusPBDB
Diet
carnivorePBDB, for Decapoda
Life habit
semi-infaunalPBDB, for Raninoidia
Motility
actively mobilePBDB, for Malacostraca
Vision
well-developedPBDB, for Malacostraca

Time the record covers

At most 12 million years on record.

The one occurrence read is dated to somewhere between 83.6 Mya and 72.2 Mya, which is a dating window rather than a span.

Late Cretaceous — about 1 of 1 occurrenceLate Cretaceous84–83 Mya — about 0.0 occurrences83–83 Mya — about 0.0 occurrences83–82 Mya — about 0.0 occurrences82–82 Mya — about 0.0 occurrences82–82 Mya — about 0.0 occurrences82–81 Mya — about 0.0 occurrences81–81 Mya — about 0.0 occurrences81–80 Mya — about 0.0 occurrences80–80 Mya — about 0.0 occurrences80–80 Mya — about 0.0 occurrences80–79 Mya — about 0.0 occurrences79–79 Mya — about 0.0 occurrences79–78 Mya — about 0.0 occurrences78–78 Mya — about 0.0 occurrences78–77 Mya — about 0.0 occurrences77–77 Mya — about 0.0 occurrences77–77 Mya — about 0.0 occurrences77–76 Mya — about 0.0 occurrences76–76 Mya — about 0.0 occurrences76–75 Mya — about 0.0 occurrences75–75 Mya — about 0.0 occurrences75–75 Mya — about 0.0 occurrences75–74 Mya — about 0.0 occurrences74–74 Mya — about 0.0 occurrences74–73 Mya — about 0.0 occurrences73–73 Mya — about 0.0 occurrences73–73 Mya — about 0.0 occurrences73–72 Mya — about 0.0 occurrences84.1 Mya71.7 Mya

1 occurrence of Cretacocarcinus smithi 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

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

Pierre Shale — 50.74°N, 101.43°W

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

Cretacocarcinus smithi and its relatives

Late Cretaceous

Where Cretacocarcinus smithi and its relatives were recorded in the Late Cretaceous.

Found in the same rock

No other named taxon is catalogued from that site.

The Paleobiology Database records 1 site for Cretacocarcinus smithi, 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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Cretacocarcinus smithi was found. Wikidata and iDigBio were searched and had none.

Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cretacocarcinus smithi, or no answer at all. This entry cannot say which.

No 3D scan of Cretacocarcinus smithi 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 itCretacocarcinus through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Feldmann et al. 2007