Conularida indet.
No picture of Conularida indet. was found. Wikidata was searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Conularida indet. 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. Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.
Time the record covers
At least 25 million years on record.
The record covers at least 458.2 Mya to 432.9 Mya. No occurrence read is dated outside 461.1 Mya to 422.7 Mya.
14 occurrences of Conularida indet. 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
14 occurrences- Ordovician64%
- Silurian36%
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
4 formations
- Ffairfach Flags and Grits Formation · Ffairfach Group9
- Lipeon Formation3
- Wilhelmi Formation1
- Mosalem Formation1
Loading coastlines…
The named rock units Conularida indet. has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Conularida indet. and its relatives
OrdovicianWhere Conularida indet. and its relatives were recorded in the Ordovician.
Found in the same rock
102 taxa- Crinoidea13 sites
- Trepostomata10 sites
- Basilicus tyrannus9 sites
- Bryozoa9 sites
- Dalmanella parva9 sites
- Hyalostelia9 sites
- Macrocoelia llandeiloensis9 sites
- Tallinnella9 sites
- Trilobita9 sites
- Cryptostomata8 sites
- Brachiopoda7 sites
- Flexicalymene cambrensis7 sites
- Marrolithus7 sites
- Triplesia edgelliana7 sites
- Gelidorthis6 sites
- Glyptorthis viriosa6 sites
- Tissintia immatura6 sites
- Gastropoda5 sites
- Kullervo5 sites
- Anabaia3 sites
- Anacaenaspis3 sites
- Ancillotoechia3 sites
- Atractopyge3 sites
- Australonucula3 sites
The Paleobiology Database records 14 sites for Conularida indet., 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
4 references- Benthic palaeocommunities represented in the Ffairfach Group and coeval Ordovician successions of Wales9
- Lithofacies, taphonomy, and brachiopod assemblages in the Silurian of western Argentina: A review of Malvinokaffric Realm communities3
- Habitat of Llandoverian-Lochkovian eurypterids1
- Silurian brachiopod and related benthic communities from carbonate platform and mound environments of Iowa and surrounding areas1
Each of the 14 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 Conularida indet. was found. Wikidata was searched and had none.
iDigBio and GBIF were not searched: the Paleobiology Database does not place Conularida indet. 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.
Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.
No 3D scan of Conularida indet. 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 itFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0.