Perissitys pacifica
via iDigBio · CC BY · via iDigBio. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- PerissitysPBDB
- Diet
- carnivorePBDB, for Neogastropoda
- Life habit
- epifaunalPBDB, for Neogastropoda
- Motility
- actively mobilePBDB, for Neogastropoda
- Vision
- limitedPBDB, for Gastropoda
Time the record covers
At most 12 million years on record.
Every occurrence read is dated to somewhere between 83.6 Mya and 72.2 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
10 occurrences of Perissitys pacifica 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
10 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
6 formations
- Williams Formation3
- Pigeon Point Formation2
- Debris Dam Formation1
- Chatsworth Formation1
- Tuna Canyon Formation1
- Cedar District Formation · Nanaimo Group1
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The named rock units Perissitys pacifica 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.
Perissitys pacifica and its relatives
Late CretaceousWhere Perissitys pacifica and its relatives were recorded in the Late Cretaceous.
Found in the same rock
147 taxa- Biplica obliqua7 sites
- Calva (Egelicalva) bowersiana6 sites
- Pterotrigonia evansana6 sites
- Acila (Truncacila) demessa5 sites
- Glycymerita veatchii5 sites
- Gyrodes (Sohlella) pacificus5 sites
- Metaplacenticeras pacificum5 sites
- Cymbophora popenoei4 sites
- Cymbophora stantoni4 sites
- Cymbophora triangulata4 sites
- Meekia (Mygallia) daileyi4 sites
- Paraesa lens4 sites
- Trinacria cor4 sites
- Atira ornatissima3 sites
- Euspira3 sites
- Legumen ooides3 sites
- Lispodesthes rotundatus3 sites
- Pentzia hilgardi3 sites
- Turritella chicoensis pescaderoensis3 sites
- Volutoderma averillii3 sites
- Anchura phaba2 sites
- Anomia2 sites
- Baculites inornatus2 sites
- Baculites rex2 sites
The Paleobiology Database records 10 sites for Perissitys pacifica, 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
3 references- Evolution and classification of the Late Cretaceous-Early Tertiary gastropod Perissitys7
- Checklist of Mesozoic macrofossil localities in the Santa Cruz Mountains and vicinity2
- An ornithomimosaur from the Campanian Cedar District Formation (Nanaimo Group) of Denman Island, British Columbia, Canada1
Each of the 10 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 content1
Picture of Perissitys pacifica
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC BY
- Commercial use
- the licence allows it
No 3D scan of Perissitys pacifica 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 itPerissitys through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Popenoe and Saul 1987