Schlotheimia cuevitensis
No picture of Schlotheimia cuevitensis 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 Schlotheimia cuevitensis, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- SchlotheimiaPBDB
- Diet
- carnivorePBDB, for Ammonoidea
- Life habit
- nektonicPBDB, for Ammonoidea
- Motility
- fast-movingPBDB, for Ammonoidea
- Vision
- well-developedPBDB, for Cephalopoda
- Environment
- marinePBDB, for Cephalopoda
Time the record covers
At most 8.5 million years on record.
Every occurrence read is dated to somewhere between 201.4 Mya and 192.9 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
12 occurrences of Schlotheimia cuevitensis on record, most of them in the Early Jurassic. 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
12 occurrences- Early Jurassic100%
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 Schlotheimia cuevitensis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 10 occurrences have no formation on record, which is common for older literature.
Schlotheimia cuevitensis and its relatives
Early JurassicWhere Schlotheimia cuevitensis and its relatives were recorded in the Early Jurassic.
Found in the same rock
13 taxa- Alsatites bipartitus1 site
- Badouxia canadensis1 site
- Badouxia forticostata1 site
- Discamphiceras1 site
- Discamphiceras silberlingi1 site
- Eolytoceras guexi1 site
- Franziceras graylockense1 site
- Gyrophioceras mineralense1 site
- Paracaloceras rursicostatum1 site
- Pseudaetomoceras shoshonense1 site
- Pseudaetomoceras victoriense1 site
- Sunrisites brimblecombei1 site
- Sunrisites senililevis1 site
The Paleobiology Database records 2 sites for Schlotheimia cuevitensis, and this reads all of them. The number is how many of those sites it was catalogued from too.
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- Die Ammoniten-Fauna des südamerikanischen Hettangium (basaler Jura), Teil 110
- Late Hettangian (Early Jurassic) ammonites from Taseko Lakes, British Columbia, Canada2
Each of the 12 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 Schlotheimia cuevitensis 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 Schlotheimia cuevitensis, or no answer at all. This entry cannot say which.
No 3D scan of Schlotheimia cuevitensis 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.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itSchlotheimia through timeFormations of the Early JurassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Hillebrandt 2000