Scolopodus pseudoquadratus
No picture of Scolopodus pseudoquadratus 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 Scolopodus pseudoquadratus, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- ScolopodusPBDB
- Diet
- carnivorePBDB, for Conodonta
- Life habit
- nektonicPBDB, for Conodonta
- Motility
- actively mobilePBDB, for Conodonta
- Vision
- well-developedPBDB, for Conodonta
Time the record covers
At least 10 million years on record.
The record covers at least 471.3 Mya to 461.1 Mya. No occurrence read is dated outside 475.3 Mya to 458.2 Mya.
2 occurrences of Scolopodus pseudoquadratus on record, most of them in the Ordovician. 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- Ordovician100%
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
- Fillmore Formation · Pogonip Group1
- Lower Setul Limestone Formation1
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The named rock units Scolopodus pseudoquadratus has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Scolopodus pseudoquadratus and its relatives
OrdovicianWhere Scolopodus pseudoquadratus and its relatives were recorded in the Ordovician.
Found in the same rock
36 taxa- Acidiphorus1 site
- Acodus1 site
- Acodus similaris1 site
- Amblycranium1 site
- Amblycranium linearus1 site
- Bathyurellus teretus1 site
- Benthamaspis gibberula1 site
- Carolinites killaryensis1 site
- Colaptoconus quadraplicatus1 site
- Diacanthaspis trispineus1 site
- Dimeropygiella blanda1 site
- Dimeropygiella fillmorensis1 site
- Drepanodus1 site
- Goniotelina plicolabeonus1 site
- Gothodus1 site
- Heckethornia alticapitis1 site
- Ibexaspis brevis1 site
- Kanoshia depressus1 site
- Lemureops lemurei1 site
- Oepikodus1 site
- Oistodus1 site
- Oistodus lanceolatus1 site
- Opipeuter angularis1 site
- Paltodus1 site
The Paleobiology Database records 1 site for Scolopodus pseudoquadratus, 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
2 references- An Ordovician (Arenigian) trilobite faunule of great diversity from the Ibex area, western Utah1
- Ordovician and Silurian Conodonts from the Langkawi Islands, Malaya, Part I1
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 the Paleobiology Database's own record for the work.
Media and terms
Media content0
No picture of Scolopodus pseudoquadratus 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 Scolopodus pseudoquadratus, or no answer at all. This entry cannot say which.
No 3D scan of Scolopodus pseudoquadratus 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 itScolopodus through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Branson and Mehl 1933