Paniscollenia sp.
No picture of Paniscollenia sp. was found. Wikipedia, Wikidata and Smithsonian Open Access were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Paniscollenia sp. firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.
Time the record covers
At least 13 million years on record.
The record covers at least 538.8 Mya to 525.5 Mya. No occurrence read is dated outside 635 Mya to 521 Mya.
2 occurrences of Paniscollenia sp. 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
2 occurrences- Cambrian50%
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
- Tal Formation1
- Turkut Formation · Khorbusuonka Group1
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The named rock units Paniscollenia sp. has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Paniscollenia sp. and its relatives
CambrianWhere Paniscollenia sp. and its relatives were recorded in the Cambrian.
Found in the same rock
11 taxa- Stratifera2 sites
- Boxonia1 site
- Cambrotubulus1 site
- Chancelloridae1 site
- Colleniella singularis1 site
- Collumnaefacta vulgaris1 site
- Epiphyton1 site
- Hyolithida1 site
- Lapworthellidae1 site
- Paniscollenia emergens1 site
- Prodoconodonta indet.1 site
The Paleobiology Database records 2 sites for Paniscollenia sp., 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- Integrated approaches to terminal Proterozoic stratigraphy: an example from the Olenek Uplift, northeastern Siberia1
- Fauna and biogenic structures in Krol-Tal succession (Vendian-Early Cambrian), Lesser Himalaya: their biostratigraphic and palaeoecological significance1
Each of the 2 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 Paniscollenia sp. was found. Wikipedia, Wikidata and Smithsonian Open Access were searched and had none.
iDigBio and GBIF were not searched: the Paleobiology Database does not place Paniscollenia sp. firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itFormations of the CambrianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0.