Antodicranomyia rubra

No picture of Antodicranomyia rubra 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 Antodicranomyia rubra, or no answer at all. This entry cannot say which.

On record

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

Time the record covers

At most 13 million years on record.

The one occurrence read is dated to somewhere between 106.3 Mya and 93.9 Mya, which is a dating window rather than a span.

Early Cretaceous — about 0 of 1 occurrenceEarly CretaceousLate Cretaceous — about 1 of 1 occurrenceLate Cretaceous106–106 Mya — about 0.0 occurrences106–105 Mya — about 0.0 occurrences105–105 Mya — about 0.0 occurrences105–105 Mya — about 0.0 occurrences105–104 Mya — about 0.0 occurrences104–104 Mya — about 0.0 occurrences104–103 Mya — about 0.0 occurrences103–103 Mya — about 0.0 occurrences103–102 Mya — about 0.0 occurrences102–102 Mya — about 0.0 occurrences102–101 Mya — about 0.0 occurrences101–101 Mya — about 0.0 occurrences101–101 Mya — about 0.0 occurrences101–100 Mya — about 0.0 occurrences100–100 Mya — about 0.0 occurrences100–99 Mya — about 0.0 occurrences99–99 Mya — about 0.0 occurrences99–98 Mya — about 0.0 occurrences98–98 Mya — about 0.0 occurrences98–97 Mya — about 0.0 occurrences97–97 Mya — about 0.0 occurrences97–97 Mya — about 0.0 occurrences97–96 Mya — about 0.0 occurrences96–96 Mya — about 0.0 occurrences96–95 Mya — about 0.0 occurrences95–95 Mya — about 0.0 occurrences95–94 Mya — about 0.0 occurrences94–94 Mya — about 0.0 occurrences106.8 Mya93.4 Mya

1 occurrence of Antodicranomyia rubra 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.

Antodicranomyia rubra and its relatives

Late Cretaceous

Where Antodicranomyia rubra and its relatives were recorded in the Late Cretaceous.

Found in the same rock

26 taxa

The Paleobiology Database records 1 site for Antodicranomyia rubra, 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

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 Antodicranomyia rubra 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 Antodicranomyia rubra, or no answer at all. This entry cannot say which.

No 3D scan of Antodicranomyia rubra 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.

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itAntodicranomyia through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Kania‑Kłosok et al. 2022