Isotelus beta
No picture of Isotelus beta was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Isotelus beta, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- IsotelusPBDB
- Diet
- carnivorePBDB, for Trilobita
- Life habit
- low-level epifaunalPBDB, for Asaphida
- Motility
- fast-movingPBDB, for Asaphida
- Vision
- well-developedPBDB, for Asaphidae
- Environment
- marinePBDB, for Trilobita
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.
9 occurrences of Isotelus beta 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
9 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
3 formations
- Crown Point Formation · Chazy Group5
- Day Point Formation · Chazy Group2
- Valcour Formation · Chazy Group2
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The named rock units Isotelus beta has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Isotelus beta and its relatives
OrdovicianWhere Isotelus beta and its relatives were recorded in the Ordovician.
Found in the same rock
66 taxa- Leperditia canadensis9 sites
- Stenopareia globosus7 sites
- Eurychilina latimarginata6 sites
- Isotelus harrisi6 sites
- Calyptaulax annulata5 sites
- Mimella vulgaris5 sites
- Multicostella platys5 sites
- Onychoplecia longirostris5 sites
- Phylloporina incepta5 sites
- Basilicus (Basiliella) whittingtoni4 sites
- Hibbertia valcourensis4 sites
- Lonchodomas chaziensis4 sites
- Macrocoelia champlainensis4 sites
- Rafinesquina alternata4 sites
- Sphenotreta acutirostris4 sites
- Stictopora fenestrata4 sites
- Thaleops ovata4 sites
- Amphilichas minganensis3 sites
- Bolboporites americanus3 sites
- Bucania sulcatina3 sites
- Ctenodonta peracuta3 sites
- Glyptomena distans3 sites
- Kawina chazyensis3 sites
- Orthambonites exfoliata3 sites
The Paleobiology Database records 9 sites for Isotelus beta, 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
1 referenceEach of the 9 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 Isotelus beta was found. Wikidata and iDigBio were searched and had none.
Wikipedia and 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 Isotelus beta, or no answer at all. This entry cannot say which.
No 3D scan of Isotelus beta 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 itIsotelus through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Raymond 1905)