Abrocar concavus

No picture of Abrocar concavus was found. Wikipedia, Wikidata and iDigBio were searched and had none. 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 Abrocar concavus, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
AbrocarPBDB
Motility
actively mobilePBDB, for Arthropoda
Environment
terrestrialPBDB, for Insecta

Time the record covers

At most 4.4 million years on record.

The one occurrence read is dated to somewhere between 125.77 Mya and 121.4 Mya, which is a dating window rather than a span.

Early Cretaceous — about 1 of 1 occurrenceEarly Cretaceous126–126 Mya — about 0.0 occurrences126–126 Mya — about 0.0 occurrences126–125 Mya — about 0.0 occurrences125–125 Mya — about 0.0 occurrences125–125 Mya — about 0.0 occurrences125–125 Mya — about 0.0 occurrences125–125 Mya — about 0.0 occurrences125–124 Mya — about 0.0 occurrences124–124 Mya — about 0.0 occurrences124–124 Mya — about 0.0 occurrences124–124 Mya — about 0.0 occurrences124–124 Mya — about 0.0 occurrences124–124 Mya — about 0.0 occurrences124–123 Mya — about 0.0 occurrences123–123 Mya — about 0.0 occurrences123–123 Mya — about 0.0 occurrences123–123 Mya — about 0.0 occurrences123–123 Mya — about 0.0 occurrences123–123 Mya — about 0.0 occurrences123–122 Mya — about 0.0 occurrences122–122 Mya — about 0.0 occurrences122–122 Mya — about 0.0 occurrences122–122 Mya — about 0.0 occurrences122–122 Mya — about 0.0 occurrences122–121 Mya — about 0.0 occurrences121–121 Mya — about 0.0 occurrences126.3 Mya120.9 Mya

1 occurrence of Abrocar concavus on record, most of them in the Early 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

Yixian — 41.62°N, 120.83°E

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

Abrocar concavus and its relatives

Early Cretaceous

Where Abrocar concavus and its relatives were recorded in the Early Cretaceous.

Found in the same rock

13 taxa

The Paleobiology Database records 1 site for Abrocar concavus, 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

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 Abrocar concavus was found. Wikipedia, Wikidata and iDigBio were searched and had none.

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 Abrocar concavus, or no answer at all. This entry cannot say which.

No 3D scan of Abrocar concavus 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 itAbrocar through timeFormations of the Early CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Davis et al. 2013