Lucinoma columbiana

via iDigBio · 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
- LucinomaPBDB
- Diet
- chemosymbioticPBDB, for Lucinoma
- Life habit
- infaunalPBDB, for Lucinoma
- Motility
- facultatively mobilePBDB, for Lucinoma
- Vision
- blindPBDB, for Bivalvia
Time the record covers
At most 11 million years on record.
Every occurrence read is dated to somewhere between 33.9 Mya and 23.04 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
7 occurrences of Lucinoma columbiana on record, most of them in the Oligocene. 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- Oligocene100%
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
5 formations
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The named rock units Lucinoma columbiana has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Lucinoma columbiana and its relatives
OligoceneWhere Lucinoma columbiana and its relatives were recorded in the Oligocene.
Found in the same rock
90 taxa- Bruclarkia columbiana3 sites
- Dentalium (Fissidentalium) laneensis3 sites
- Glossaulax reclusiana3 sites
- Macrocallista pittsburgensis3 sites
- Mactromeris pittsburgensis3 sites
- Molopophorus gabbi3 sites
- Perse pittsburgensis3 sites
- Scaphander stewarti3 sites
- Solena (Eosolen) eugenensis3 sites
- Tellina (Eurytellina)3 sites
- Acila (Truncacila) shumardi2 sites
- Acteon2 sites
- Acteon chehalisensis2 sites
- Architectonica blanda2 sites
- Cardium (Laevicardium) alaskensis2 sites
- Eosiphonalia oregonensis2 sites
- Felaniella (Felaniella) snavelyi2 sites
- Neverita (Neverita) washingtonensis2 sites
- Nucula (Leionucula) vokesi2 sites
- Nuculana (Saccella) washingtonensis2 sites
- Panomya norvegica2 sites
- Polinices (Euspira) galianoi2 sites
- Polinices washingtonensis2 sites
- Priscofusus stewarti2 sites
The Paleobiology Database records 6 sites for Lucinoma columbiana, 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
4 references- Oligocene marine mollusks from the Pittsburg Bluff Formation in Oregon3
- Fauna of the Poul and Yakataga Formations (Upper Oligocene) of Southern Alaska2
- Makah Formation - A deep-marginal-basin sequence of Late Eocene and Oligocene age in the Northwestern Olympic Peninsula, Washington1
- Fauna of the Sooke Formation Vancouver Island1
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 Lucinoma columbiana
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
No 3D scan of Lucinoma columbiana 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 itLucinoma through timeFormations of the OligoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Clark and Arnold 1923)