Cathayamodus fournieri

No picture of Cathayamodus fournieri was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cathayamodus fournieri, or no answer at all. This entry cannot say which.

On record

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

Time the record covers

At most 4.4 million years on record.

Every occurrence read is dated to somewhere between 125.77 Mya and 121.4 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Early Cretaceous — about 2 of 2 occurrencesEarly Cretaceous126–126 Mya — about 0.0 occurrences126–126 Mya — about 0.1 occurrences126–125 Mya — about 0.1 occurrences125–125 Mya — about 0.1 occurrences125–125 Mya — about 0.1 occurrences125–125 Mya — about 0.1 occurrences125–125 Mya — about 0.1 occurrences125–124 Mya — about 0.1 occurrences124–124 Mya — about 0.1 occurrences124–124 Mya — about 0.1 occurrences124–124 Mya — about 0.1 occurrences124–124 Mya — about 0.1 occurrences124–124 Mya — about 0.1 occurrences124–123 Mya — about 0.1 occurrences123–123 Mya — about 0.1 occurrences123–123 Mya — about 0.1 occurrences123–123 Mya — about 0.1 occurrences123–123 Mya — about 0.1 occurrences123–123 Mya — about 0.1 occurrences123–122 Mya — about 0.1 occurrences122–122 Mya — about 0.1 occurrences122–122 Mya — about 0.1 occurrences122–122 Mya — about 0.1 occurrences122–122 Mya — about 0.1 occurrences122–121 Mya — about 0.1 occurrences121–121 Mya — about 0.0 occurrences126.3 Mya120.9 Mya

2 occurrences of Cathayamodus fournieri 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

2 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 Cathayamodus fournieri has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Cathayamodus fournieri and its relatives

Early Cretaceous

Where Cathayamodus fournieri and its relatives were recorded in the Early Cretaceous.

Found in the same rock

37 taxa

The Paleobiology Database records 2 sites for Cathayamodus fournieri, 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 2 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. 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 Cathayamodus fournieri was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

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

No 3D scan of Cathayamodus fournieri was found in Smithsonian Open Access and Sketchfab.

MorphoSource 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 itCathayamodus through timeFormations of the Early CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Gao et al. 2016