Balanocrinus dumortieri
No picture of Balanocrinus dumortieri 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 Balanocrinus dumortieri, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- BalanocrinusPBDB
- Diet
- suspension feederPBDB, for Isocrinidae
- Life habit
- upper-level epifaunalPBDB, for Isocrinidae
- Motility
- stationary, attachedPBDB, for Isocrinidae
- Vision
- blindPBDB, for Crinoidea
- Environment
- marinePBDB, for Echinodermata
Time the record covers
At most 14 million years on record.
Every occurrence read is dated to somewhere between 168.6 Mya and 154.8 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
6 occurrences of Balanocrinus dumortieri 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
6 occurrencesThese 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.
Balanocrinus dumortieri and its relatives
Middle JurassicWhere Balanocrinus dumortieri and its relatives were recorded in the Middle Jurassic.
Found in the same rock
76 taxa- Cyclocrinus rugosus4 sites
- Cyrtocrinus praenutans4 sites
- Lonchocrinus dumortieri4 sites
- Balanocrinus inornatus3 sites
- Dolichocrinus aberrans3 sites
- Balanocrinus pacomei2 sites
- Eugeniacrinites2 sites
- Isocrinus dumortieri2 sites
- Isocrinus nicoleti2 sites
- Phyllocrinus colloti2 sites
- Phyllocrinus voultensis2 sites
- Acrosmilia1 site
- Acrosmilia fungina1 site
- Adelocoenia limbata1 site
- Andymetra galei1 site
- Anomiidae1 site
- Apiocrinites1 site
- Aplosmilia1 site
- Asteroidea1 site
- Balanocrinus subteres1 site
- Brachiopoda1 site
- Chariocrinus1 site
- Cryptocoenia cartieri1 site
- Cylindrophyma1 site
The Paleobiology Database records 5 sites for Balanocrinus dumortieri, 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- Crinoids from the Middle Jurassic (Bajocian–Lower Callovian) of Arde`che, France4
- The La Voulte Lagerstätte (Callovian): Evidence for a deep water setting from sponge and crinoid communities1
- Late Jurassic crinoids from Sudak environs (Crimea)1
Each of the 6 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 content0
No picture of Balanocrinus dumortieri 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 Balanocrinus dumortieri, or no answer at all. This entry cannot say which.
No 3D scan of Balanocrinus dumortieri 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 itBalanocrinus through timeFormations of the Middle JurassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. de Loriol 1887