Euspira compressa
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
- EuspiraPBDB
- Diet
- carnivorePBDB, for Euspira
- Life habit
- semi-infaunalPBDB, for Euspira
- Motility
- actively mobilePBDB, for Euspira
- Vision
- limitedPBDB, for Gastropoda
Time the record covers
At most 35 million years on record.
Every occurrence read is dated to somewhere between 100.5 Mya and 66 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
7 occurrences of Euspira compressa 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
7 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
- Tuna Canyon Formation2
- Moreno Formation · Great Valley Group1
- Pigeon Point Formation1
- Chatsworth Formation1
- Ladd Formation1
- Deer Valley Formation1
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The named rock units Euspira compressa has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Euspira compressa and its relatives
Late CretaceousWhere Euspira compressa and its relatives were recorded in the Late Cretaceous.
Found in the same rock
24 taxa- Biplica obliqua3 sites
- Calva (Calva) peninsularis2 sites
- Calva (Egelicalva) nitida2 sites
- Dentalium (Entalis) whiteavesi2 sites
- Glycymerita veatchii2 sites
- Gyrodes (Sohlella) expansus2 sites
- Meekia (Meekia) sella2 sites
- Metaplacenticeras sanctaemonicae2 sites
- Mytilus quadratus2 sites
- Pterotrigonia evansana2 sites
- Ampullina pseudoalveata1 site
- Anchura1 site
- Baculites chicoensis1 site
- Calva (Calva) varians1 site
- Calva (Egelicalva) bowersiana1 site
- Cymbophora gabbiana1 site
- Gyrodes (Sohlella) pacificus1 site
- Lysis suciensis1 site
- Nuculana1 site
- Ostrea taxidonta1 site
- Perissitys brevirostris1 site
- Protocardia1 site
- Turritella chicoensis1 site
- Volutoderma blakei1 site
The Paleobiology Database records 7 sites for Euspira compressa, 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
4 references- Upper Cretaceous of the Pacific Coast3
- Geology of the eastern part of the Santa Monica Mountains, Los Angeles County, California2
- Paleogeographic implications of molluscan assemblages in the Upper Cretaceous (Campanian) Pigeon Point Formation, California1
- Stratigraphic and faunal relations of the Martinez to the Chico and Tejon of Southern California1
Each of the 7 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 content1
Picture of Euspira compressa
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC BY
- Commercial use
- the licence allows it
No 3D scan of Euspira compressa 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 itEuspira through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Waring 1917)