Wilbernia explanata
No picture of Wilbernia explanata 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 Wilbernia explanata, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- WilberniaPBDB
- Diet
- carnivorePBDB, for Trilobita
- Life habit
- low-level epifaunalPBDB, for Trilobita
- Motility
- fast-movingPBDB, for Trilobita
- Vision
- well-developedPBDB, for Idahoiidae
- Environment
- marinePBDB, for Trilobita
Time the record covers
At most 4.6 million years on record.
Every occurrence read is dated to somewhere between 493.5 Mya and 488.9 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
4 occurrences of Wilbernia explanata on record, most of them in the Cambrian. 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
4 occurrences- Cambrian100%
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
2 formations
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The named rock units Wilbernia explanata has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Wilbernia explanata and its relatives
CambrianWhere Wilbernia explanata and its relatives were recorded in the Cambrian.
Found in the same rock
19 taxa- Pseudagnostus3 sites
- Pseudagnostus josephus3 sites
- Minkella2 sites
- Stigmacephalus oweni2 sites
- Ellipsocephaloides curtus1 site
- Idahoia serapio1 site
- Kendallina1 site
- Monocheilus micros1 site
- Neoagnostus1 site
- Orygmaspis1 site
- Orygmaspis contracta1 site
- Parabolinoides calvilimbata1 site
- Ptychaspis1 site
- Saratogia1 site
- Saratogia fria1 site
- Saratogia wisconsensis1 site
- Stigmaspis1 site
- Taenicephalina1 site
- Taenicephalus shumardi1 site
The Paleobiology Database records 4 sites for Wilbernia explanata, and this reads all of them. The number is how many of those sites it was catalogued from too.
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- Trilobites of the Upper Cambrian Sunwaptan Stage, southern Canadian Rocky Mountains, Alberta3
- Cambrian trilobites from the Nounan Dolomite and lower St. Charles Formation (upper Marjuman to lower Sunwaptan; Miaolingian to Furongian Series), Smithfield Canyon, northern Utah1
Each of the 4 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 content0
No picture of Wilbernia explanata 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 Wilbernia explanata, or no answer at all. This entry cannot say which.
No 3D scan of Wilbernia explanata 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 itWilbernia through timeFormations of the CambrianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Whitfield 1880)