Walliserodus curvatus
No picture of Walliserodus curvatus was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Walliserodus curvatus, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- WalliserodusPBDB
- 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 40 million years on record.
The record covers at least 471.3 Mya to 430.6 Mya. No occurrence read is dated outside 486.85 Mya to 413.02 Mya.
244 occurrences of Walliserodus curvatus on record, most of them in the Silurian. 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
244 occurrences- Ordovician13%
- Silurian86%
- Devonianunder 1%
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
44 formations
- Gun River Formation35
- Becscie Formation30
- Brassfield Formation18
- Salamonie Formation12
- Birstonas Formation10
- Maut Formation9
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The named rock units Walliserodus curvatus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 20 further formations hold fewer occurrences each and are not listed. 21 occurrences have no formation on record, which is common for older literature.
Walliserodus curvatus and its relatives
SilurianWhere Walliserodus curvatus and its relatives were recorded in the Silurian.
Found in the same rock
302 taxa- Panderodus unicostatus59 sites
- Panderodus32 sites
- Pseudooneotodus beckmanni32 sites
- Panderodus panderi27 sites
- Distomodus kentuckyensis22 sites
- Oulodus22 sites
- Ozarkodina20 sites
- Drepanoistodus suberectus18 sites
- Decoriconus fragilis15 sites
- Panderodus gracilis15 sites
- Icriodella13 sites
- Ozarkodina oldhamensis13 sites
- Pseudolonchodina expansa13 sites
- Rexroadus kentuckyensis13 sites
- Ozarkodina hassi12 sites
- Dapsilodus obliquicostatus10 sites
- Wurmiella excavata excavata10 sites
- Amorphognathus ordovicicus9 sites
- Panderodus serratus9 sites
- Pseudooneotodus bicornis9 sites
- Aphelognathus8 sites
- Belodina7 sites
- Decoriconus7 sites
- Distomodus7 sites
The Paleobiology Database records 92 sites for Walliserodus curvatus, 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
27 references- A New Llandovery (Early Silurian) Conodont Biozonation and Conodonts from the Becscie,Merrimack, and Gun River Formations, Anticosti Island, Québec65
- Stratigraphy and conodont paleontology of the Salamonie Dolomite and Lee Creek Member of the Brassfield Limestone (Silurian) in southeastern Indiana and adjacent Kentucky33
- Hirnantian (Ordovician) through Wenlock (Silurian) conodont biostratigraphy, bioevents, and integration with graptolite biozones, Cape Phillips Formation slope facies, Cornwallis Island, Canadian Arctic Islands22
- Conodonts from the Upper Ordovician–lower Silurian carbonate platform of North Greenland17
- Upper Ordovician – Upper Silurian conodont biostratigraphy, Devon Island and southern Ellesmere Island, Canadian Arctic Islands, with implications for regional stratigraphy, eustasy, and thermal maturation11
- Late Ordovician- Early Silurian conodont biostratigraphy and thermal maturity, Hudson Bay Basin11
- Upper Wenlock d13C chemostratigraphy, conodont biostratigraphy and palaeoecological dynamics in the Ledai-179 drill core (Eastern Lithuania)10
- Late Ordovician to Early Silurian Conodont faunas from the Kolyma Terrane, Omulev Mountains, Northeast Russia, and their paleobiogeographic affinity10
- Late Ordovician-Early Silurian Strata in the Central United States and the Hirnantian Age8
- Local variations in the distribution of Silurian conodonts of the Distomodus kentuckyensis Zone of the Oslo Region, Norway8
- Restudy of conodonts (Late Ordovician – Early Silurian) from the Edgewood Group, Clarksville, Missouri7
- Conodont biostratigraphy across the Ordovician-Silurian boundary, Ellis Bay Formation, Anticosti Island, Québec6
Each of the 244 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. 15 further references are not listed. 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 Walliserodus curvatus was found. Wikidata and iDigBio were searched and had none.
Wikipedia and 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 Walliserodus curvatus, or no answer at all. This entry cannot say which.
No 3D scan of Walliserodus curvatus 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 itWalliserodus through timeFormations of the SilurianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Branson and Branson 1947)