Pseudohuangia chitralicum
No picture of Pseudohuangia chitralicum 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 Pseudohuangia chitralicum, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- PseudohuangiaPBDB
- Diet
- suspension feederPBDB, for Rugosa
- Life habit
- epifaunalPBDB, for Rugosa
- Motility
- stationary, attachedPBDB, for Rugosa
- Vision
- blindPBDB, for Anthozoa
- Environment
- marinePBDB, for Rugosa
Time the record covers
At most 24 million years on record.
Every occurrence read is dated to somewhere between 283.3 Mya and 259.857 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
4 occurrences of Pseudohuangia chitralicum on record, most of them in the Permian. 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- Permian100%
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
- Lashkargaz Formation · Chapursan Group2
Loading coastlines…
The named rock units Pseudohuangia chitralicum has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.
Pseudohuangia chitralicum and its relatives
PermianWhere Pseudohuangia chitralicum and its relatives were recorded in the Permian.
Found in the same rock
14 taxa- Acosarina juresanensis2 sites
- Dasysaria inca2 sites
- Protomichelinia siyangensis2 sites
- Spiriferina octoplicata2 sites
- Buxtonia juresanensis1 site
- Cancrinella cancriniformis1 site
- Chonetes dereimsii1 site
- Derbyia buchi1 site
- Eolyttonia tenuis1 site
- Hoskingia hochstetteri1 site
- Linoproductus lineatus1 site
- Marginifera (Arenaria) ovalis1 site
- Spinomarginifera spinosocostata1 site
- Wentzelophyllum douglasi1 site
The Paleobiology Database records 4 sites for Pseudohuangia chitralicum, 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
3 references- A Permo-Carboniferous fauna from south-west Persia (Iran)2
- New findings of Permian fusulinids and corals from western Karakorum and E Hindu Kush (Pakistan)1
- Two Anthracolithic corals from British Columbia, and related species from the Tethys1
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. Each entry links to the Paleobiology Database's own record for the work.
Media and terms
Media content0
No picture of Pseudohuangia chitralicum 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 Pseudohuangia chitralicum, or no answer at all. This entry cannot say which.
No 3D scan of Pseudohuangia chitralicum 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 itPseudohuangia through timeFormations of the PermianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Smith 1935)