Phasianella variegata
Phasianella solida, common name the solid pheasant, is a species of sea snail, a marine gastropod mollusk in the family Phasianellidae.
H. Zell · CC BY-SA 3.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- PhasianellaPBDB
- Diet
- grazerPBDB, for Trochoidea
- Life habit
- epifaunalPBDB, for Trochoidea
- Motility
- actively mobilePBDB, for Trochoidea
- Vision
- limitedPBDB, for Gastropoda
Time the record covers
At least 15 million years on record.
The record covers at least 15.98 Mya to 129 ka. No occurrence read is dated outside 23.04 Mya to 11.7 ka.
3 occurrences of Phasianella variegata on record, most of them in the Miocene. 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
3 occurrences- Miocene67%
- Pleistocene33%
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 Phasianella variegata has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.
Phasianella variegata and its relatives
MioceneWhere Phasianella variegata and its relatives were recorded in the Miocene.
Found in the same rock
29 taxa- Agaronia pupa1 site
- Athleta (Volutospina) dentata1 site
- Cerithium (Ptychocerithium) pseudocorrugatum1 site
- Cerithium (Ptychocerithium) rude1 site
- Cernina carlei1 site
- Clypeaster1 site
- Distorsio decipiens1 site
- Gemmula gajensis1 site
- Gyrineum bituberculare1 site
- Haustator tauroperturritus1 site
- Hemipolygona1 site
- Kuphus1 site
- Lyria (Harpeola) jugosa1 site
- Natica obscura1 site
- Pachycrommium harrisi1 site
- Pectinidae1 site
- Periglypta1 site
- Persististrombus depertitus1 site
- Placuna1 site
- Pugilina eulactea1 site
- Scleractinia1 site
- Solen1 site
- Tectus cognatus1 site
- Thalassinoides1 site
The Paleobiology Database records 1 site for Phasianella variegata, 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
3 references- Late Pleistocene gastropods from the raised reefal limestone of Jeddah, Saudi Arabia: taxonomic and palaeoenvironmental implications1
- Oligocene and Early Miocene gastropods from Kutch (NW India) document an early biogeographic switch from Western Tethys to Indo-Pacific1
- The Miocene Mollusca from Quilon, Kerala (India)1
Each of the 3 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 content1
Picture of Phasianella variegata
- Source
- Wikipedia/Commons
- Credit
- H. Zell
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan of Phasianella variegata 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.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itPhasianella through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Lamarck 1822