Parabolablastus elongatus
No picture of Parabolablastus elongatus 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 Parabolablastus elongatus, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- ParabolablastusPBDB
- Diet
- suspension feederPBDB, for Parablastoidea
- Life habit
- epifaunalPBDB, for Parablastoidea
- Motility
- stationaryPBDB, for Parablastoidea
- Environment
- marinePBDB, for Echinodermata
Time the record covers
At most 14 million years on record.
Every occurrence read is dated to somewhere between 471.3 Mya and 457.3 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
3 occurrences of Parabolablastus elongatus on record, most of them in the Ordovician. 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
3 occurrences- Ordovician100%
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
1 formation
- Antelope Valley Formation · Pogonip Group3
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The named rock units Parabolablastus elongatus has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Parabolablastus elongatus and its relatives
OrdovicianWhere Parabolablastus elongatus and its relatives were recorded in the Ordovician.
Found in the same rock
41 taxa- Blastoidocrinus nevadensis3 sites
- Anomalorthis fascicostellatus1 site
- Anthaspidella clintoni1 site
- Anthaspidella traini1 site
- Archaeoscyphia pulchra1 site
- Bryozoa1 site
- Calycocoelia typicalis1 site
- Conodonta1 site
- Cuparius1 site
- Deltacystis symmetricus1 site
- Ectenonotus whittingtoni1 site
- Eoleperditia1 site
- Eurychilina1 site
- Hadrocystis1 site
- Hesperocoelia typicalis1 site
- Hesperocoelia undulata1 site
- Illaenus auriculatus1 site
- Kawina1 site
- Leperditella1 site
- Leptellina1 site
- Lissocoelia ramosa1 site
- Nevadocoelia grandis1 site
- Nevadocoelia traini1 site
- Nevadocoelia wistae1 site
The Paleobiology Database records 3 sites for Parabolablastus elongatus, 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
2 references- New parablastoids from the western United States2
- Fossils from the Ordovician bioherm at Meiklejohn Peak, Nevada1
Each of the 3 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 content0
No picture of Parabolablastus elongatus 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 Parabolablastus elongatus, or no answer at all. This entry cannot say which.
No 3D scan of Parabolablastus elongatus 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 itParabolablastus through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Sprinkle 1973)