Pseudoperna
Pseudoperna is a genus of extinct very small oysters. Pseudoperna lived in tight groups. This small oyster is commonly found attached in groups to the shell of large species such as Inoceramus. Pycnodonte and Pseudoperna are preserved mostly as calcitic valves and are also found attached to Mytiloides.
No picture of Pseudoperna 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 Pseudoperna, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- LophinaePBDB
- Diet
- suspension feederPBDB, for Ostreidae
- Life habit
- epifaunalPBDB, for Ostreidae
- Motility
- stationary, attachedPBDB, for Ostreidae
- Vision
- blindPBDB, for Bivalvia
- Environment
- hypersaline,marine,brackishPBDB, for Ostreidae
Time the record covers
At least 21 million years on record.
The record covers at least 93.9 Mya to 72.2 Mya. No occurrence read is dated outside 100.5 Mya to 66 Mya.
76 occurrences of Pseudoperna 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
76 occurrences- Late Cretaceous100%
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
12 formations
- Mancos Shale Formation37
- Niobrara Formation · Colorado Group16
- Corsicana Marl Formation7
- Coleraine Formation3
- Greenhorn Limestone Formation2
- Aguja Formation2
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The named rock units Pseudoperna has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.
Pseudoperna and its relatives
Late CretaceousWhere Pseudoperna and its relatives were recorded in the Late Cretaceous.
Found in the same rock
315 taxa- Ostrea congesta40 sites
- Inoceramus37 sites
- Baculites20 sites
- Ostrea16 sites
- Mytiloides stantoni13 sites
- Platyceramus platinus11 sites
- Corbula10 sites
- Cymbophora10 sites
- Nuculana10 sites
- Baculites codyensis9 sites
- Inoceramidae9 sites
- Mytiloides9 sites
- Anomia8 sites
- Baculites asper8 sites
- Lucina8 sites
- Tellina8 sites
- Anisomyon6 sites
- Mytiloides opalensis6 sites
- Phelopteria6 sites
- Placenticeras6 sites
- Pycnodonte6 sites
- Dentalium leve5 sites
- Exogyra5 sites
- Lopha mesenterica5 sites
The Paleobiology Database records 76 sites for Pseudoperna, 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
21 references- Revised interpretation of the Cretaceous section on Vermilion Creek, Moffat County, Colorado25
- Stratigraphy of the Upper Cretaceous Niobrara Formation in the Raton basin, New Mexico10
- The paleoecology of the Cenomanian-Turonian (Cretaceous) stage boundary extinctions at Black Mesa, Arizona9
- Patterns of molluscan extinction and recovery across the Cretaceous-Tertiary boundary in east Texas; report on new outcrops7
- Paleontology of the Greenhorn cylcothem (Cretaceous: late Cenomanian to middle Turonian) at Black Mesa, northeastern Arizona5
- Cretaceous of the Mesabi Iron Range, Minnesota3
- Paleoecology of the Aguja formation, Brewster County, Texas2
- American Journal of Science2
- A ‘woollgari-zone mosasaur’ (Squamata; Mosasauridae) from the Carlile Shale (Lower Middle Turonian) of central Kansas and the stratigraphic overlap of early mosasaurs and pliosaurid plesiosaurs1
- A survey of fossils and geology of Red Rock Canyon Open Space, Colorado Springs, Colorado1
- Paleoecology of giant Inoceramidae (Platyceramus) on a Santonian (Cretaceous) seafloor in Colorado1
- The molluscan and brachiopod fauna of the Late Cretaceous Pierre Shale (Baculites compressus/Baculites cuneatus biozones) near Kremmling, Colorado1
Each of the 76 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. 9 further references are not listed. 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 Pseudoperna 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 Pseudoperna, or no answer at all. This entry cannot say which.
No 3D scan of Pseudoperna 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.
The description on this site
- Source
- Wikipedia, “Pseudoperna”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itLophinae through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Logan 1899