Virgiana decussata
No picture of Virgiana decussata was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Virgiana decussata, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- VirgianaPBDB
- Diet
- suspension feederPBDB, for Pentamerida
- Life habit
- epifaunalPBDB, for Pentamerida
- Motility
- stationaryPBDB, for Pentamerida
- Vision
- blindPBDB, for Rhynchonellata
- Environment
- marinePBDB, for Lophophorata
Time the record covers
At most 24 million years on record.
Every occurrence read is dated to somewhere between 443.1 Mya and 419.62 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
22 occurrences of Virgiana decussata on record, most of them in the Silurian. 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
22 occurrences- Silurian100%
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
- Fisher Branch Dolomite Formation · Interlake Group8
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The named rock units Virgiana decussata has been recovered from, largest first. Drawn where the rock is now, not where it formed. 14 occurrences have no formation on record, which is common for older literature.
Virgiana decussata and its relatives
SilurianWhere Virgiana decussata and its relatives were recorded in the Silurian.
Found in the same rock
24 taxa- Neozaphrentis6 sites
- Pentameridae5 sites
- Lyellia affinis4 sites
- Multisolenia4 sites
- Paleofavosites4 sites
- Clathrodictyon3 sites
- Favosites gothlandicus3 sites
- Megastrophia (Eomegastrophia) paskoiacensis3 sites
- Paleofavosites poulseni3 sites
- Camarotoechia2 sites
- Dalmanella2 sites
- Fardenia transversalis2 sites
- Monomerella2 sites
- Tryplasma2 sites
- Asthenophyllum1 site
- Conchidium1 site
- Eomegastrophia philomena1 site
- Favosites1 site
- Halysites compactus1 site
- Leperditia1 site
- Liospira affinis1 site
- Modiolopsis1 site
- Nuculoidea1 site
- Paleofavosites transiens1 site
The Paleobiology Database records 22 sites for Virgiana decussata, 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- Kaskattama no. 1 well, central Hudson Bay lowland, Manitoba, Canada14
- Stratigraphy and palaeontology of the Interlake Group and Stonewall Formation of Southern Manitoba8
Each of the 22 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 Virgiana decussata was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Virgiana decussata, or no answer at all. This entry cannot say which.
No 3D scan of Virgiana decussata was found in Smithsonian Open Access and Sketchfab.
MorphoSource 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 itVirgiana through timeFormations of the SilurianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Whiteaves 1891)