Limatula cerealis
via iDigBio · CC BY-NC-ND · 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
- LimatulaPBDB
- Diet
- suspension feederPBDB, for Limatula
- Life habit
- low-level epifaunalPBDB, for Limatula
- Motility
- facultatively mobile, attachedPBDB, for Limatula
- Vision
- blindPBDB, for Bivalvia
Time the record covers
At most 5.6 million years on record.
Every occurrence read is dated to somewhere between 170.9 Mya and 165.3 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
13 occurrences of Limatula cerealis on record, most of them in the Middle Jurassic. 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
13 occurrences- Middle Jurassic100%
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
- Calcaires marno-crayeux superieurs Formation5
- Calcaires pseudo-oolithiques superieurs Formation2
- Strungulita Formation2
- Oolithe miliaire Formation1
- Calcaires pseudo-oolithiques inferieurs Formation1
- Calcaires marneux inferieurs Formation1
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The named rock units Limatula cerealis 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.
Limatula cerealis and its relatives
Middle JurassicWhere Limatula cerealis and its relatives were recorded in the Middle Jurassic.
Found in the same rock
97 taxa- Lithophaga fabella10 sites
- Lopha costata10 sites
- Fimbria lajoyei9 sites
- Parallelodon hirsonensis9 sites
- Radulopecten vagans7 sites
- Trigonia pullus7 sites
- Cavilucina (Mesomiltha) orbignyana6 sites
- Homomya gibbosa6 sites
- Nanogyra (Nanogyra) nana6 sites
- Protocardia stricklandi6 sites
- Eonavicula gibbosa5 sites
- Eonavicula minuta5 sites
- Anisocardia beaumonti4 sites
- Camptonectes laminatus4 sites
- Cavilucina (Mesomiltha) bellona4 sites
- Ceratomya concentrica4 sites
- Lima (Plagiostoma) hellica4 sites
- Lima (Plagiostoma) subcardiiformis4 sites
- Limopsis minima4 sites
- Myophorella (Orthotrigonia) spiculifera4 sites
- Sphaeriola madridi4 sites
- Actinostreon gregarea3 sites
- Lima (Plagiostoma) bynei3 sites
- Mesolinga cardioides3 sites
The Paleobiology Database records 13 sites for Limatula cerealis, 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- Geologie, Paleontologie et Paleoecologie du Bathonien au sud-ouest du Massif Ardennais10
- The Jurassic bivalve fauna from the western side of the Bucegi Mountains, part 1 subclasses Palaeotaxodonta and Pteriomorphia (Orders Arcoida, Pterioida, Limoida)2
- Unpublished data1
Each of the 13 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 the Paleobiology Database's own record for the work.
Media and terms
Media content1
Picture of Limatula cerealis
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC BY-NC-ND
- Commercial use
- the licence does not allow it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itLimatula through timeFormations of the Middle JurassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Douglas and Arkell 1932