Palaeopinnixa rathbunae
No picture of Palaeopinnixa rathbunae 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 Palaeopinnixa rathbunae, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- PalaeopinnixaPBDB
- Diet
- carnivorePBDB, for Decapoda
- Life habit
- epifaunalPBDB, for Decapoda
- Motility
- actively mobilePBDB, for Malacostraca
- Vision
- well-developedPBDB, for Malacostraca
Time the record covers
At most 19 million years on record.
Every occurrence read is dated to somewhere between 56 Mya and 37.71 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
6 occurrences of Palaeopinnixa rathbunae on record, most of them in the Eocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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
6 occurrences- Eocene100%
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
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The named rock units Palaeopinnixa rathbunae has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Palaeopinnixa rathbunae and its relatives
EoceneWhere Palaeopinnixa rathbunae and its relatives were recorded in the Eocene.
Found in the same rock
17 taxa- Eriosachila orri5 sites
- Orbitoplax weaveri4 sites
- Raninoides vaderensis4 sites
- Rogueus orri4 sites
- Panopeus baldwini3 sites
- Ctenocheles hokoensis2 sites
- Archaeozius occidentalis1 site
- Branchioplax washingtoniana1 site
- Carpilius occidentalis1 site
- Glyphea micheleae1 site
- Laeviranina goedertorum1 site
- Macroacaena alseanus1 site
- Marycarcinus hannae1 site
- Portunites macrospinus1 site
- Pulalius dunhamorum1 site
- Pulalius vulgaris1 site
- Raninoides fulgidus1 site
The Paleobiology Database records 6 sites for Palaeopinnixa rathbunae, 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
2 references- The Early Eocene decapod crustacean fauna of the Lookingglass Formation, Oregon5
- Eocene decapod crustaceans from Pulali Point, Washington1
Each of the 6 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 content0
No picture of Palaeopinnixa rathbunae 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 Palaeopinnixa rathbunae, or no answer at all. This entry cannot say which.
No 3D scan of Palaeopinnixa rathbunae 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 itPalaeopinnixa through timeFormations of the EoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Schweitzer et al. 2000