Rhodesognathus elegans
No picture of Rhodesognathus elegans was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Rhodesognathus elegans, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- RhodesognathusPBDB
- 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 1.8 million years on record.
The record covers at least 451 Mya to 449.2 Mya. No occurrence read is dated outside 453.8 Mya to 445.2 Mya.
6 occurrences of Rhodesognathus elegans 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
6 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
3 formations
- Welling Formation3
- Sugar River Limestone Formation · Lower Trenton Group2
- Portrane Limestone Formation · Duncannon Group1
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The named rock units Rhodesognathus elegans has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Rhodesognathus elegans and its relatives
OrdovicianWhere Rhodesognathus elegans and its relatives were recorded in the Ordovician.
Found in the same rock
121 taxa- Drepanoistodus suberectus6 sites
- Amorphognathus5 sites
- Phragmodus undatus5 sites
- Dapsilodus mutatus3 sites
- Panderodus3 sites
- Petrocrania3 sites
- Amplexopora2 sites
- Belodina confluens2 sites
- Ceraurus pleurexanthemus2 sites
- Cincinnaticrinus varibrachialus2 sites
- Conularia2 sites
- Crinoidea2 sites
- Cryptolithus tessellatus2 sites
- Ctenodonta peracuta2 sites
- Cymatonota2 sites
- Dekayia2 sites
- Drepanoistodus2 sites
- Endoceras proteiforme2 sites
- Eridotrypa mutabilis2 sites
- Flexicalymene (Flexicalymene) senaria2 sites
- Glossina riciniformis2 sites
- Graptodictya2 sites
- Hallopora2 sites
- Iocrinus subcrassus2 sites
The Paleobiology Database records 6 sites for Rhodesognathus elegans, 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- Fossil communities of the lower Trenton Group (Middle Ordovician) of central and northwestern New York State2
- Articulate brachiopods of the Viola Formation (Ordovician) in the Arbuckle Mountains, Oklahoma2
- Katian conodonts from the Portrane Limestone: the first Ordovician conodont fauna described from Ireland1
- Late Ordovician-Early Silurian Strata in the Central United States and the Hirnantian Age1
Each of the 6 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 Rhodesognathus elegans was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Rhodesognathus elegans, or no answer at all. This entry cannot say which.
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itRhodesognathus through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Rhodes 1953)