Uhligella walleranti
Waterlot, Georges · CC BY 4.0 · via GBIF. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- UhligellaPBDB
- 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 least 3.8 million years on record.
The record covers at least 110.1 Mya to 106.3 Mya. No occurrence read is dated outside 113.2 Mya to 100.5 Mya.
7 occurrences of Uhligella walleranti on record, most of them in the Early Cretaceous. 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
7 occurrences- Early Cretaceous100%
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
Loading coastlines…
The named rock units Uhligella walleranti has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.
Uhligella walleranti and its relatives
Early CretaceousWhere Uhligella walleranti and its relatives were recorded in the Early Cretaceous.
Found in the same rock
51 taxa- Desmoceras (Desmoceras) latidorsatum3 sites
- Douvilleiceras mammillatum3 sites
- Beudanticeras (Beudanticeras)2 sites
- Beudanticeras beudanti2 sites
- Desmoceras (Desmoceras) latidorsatum complanatum2 sites
- Douvilleiceras2 sites
- Phylloceras (Hypophylloceras) velledae2 sites
- Roberticeras newtoni2 sites
- Tegoceras camatteanum2 sites
- Uhligella rebouli2 sites
- Acanthoceras1 site
- Anagaudryceras1 site
- Belemnites1 site
- Beudanticeras1 site
- Conulus1 site
- Cymatoceras1 site
- Desmoceras (Desmoceras)1 site
- Desmoceras (Desmoceras) latidorsatum inflatum1 site
- Discoides1 site
- Douvilleiceras inaequinodum1 site
- Engonoceras1 site
- Epiaster1 site
- Hamites1 site
- Hamites intermedius1 site
The Paleobiology Database records 7 sites for Uhligella walleranti, 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
6 references- Beschreibung neugefundener Ammonoidea aus der Vorarlberger Garschella-Formation (Aptian-Albian)2
- Renz, 19821
- Geologie de Madagascar I. Les Terrains Sedimentaires1
- Nouvelles données sur l'Albien de la Chartreuse et du Vercors1
- The Cretaceous and Tertiary of southern Texas and northern Mexico1
- Monograph of the Ammonoidea of the Gault. Part I1
Each of the 7 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 content1
Picture of Uhligella walleranti
- Source
- GBIF
- Credit
- Waterlot, Georges
- Licence
- CC BY 4.0
- Commercial use
- the licence allows it
No 3D scan of Uhligella walleranti 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 itUhligella through timeFormations of the Early CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Jacob 1908)