Diaplococeras connectens
No picture of Diaplococeras connectens 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 Diaplococeras connectens, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- DiaplococerasPBDB
- Diet
- carnivorePBDB, for Ceratitida
- Life habit
- nektonicPBDB, for Ceratitida
- Motility
- actively mobilePBDB, for Ceratitida
- Vision
- well-developedPBDB, for Cephalopoda
- Environment
- marinePBDB, for Cephalopoda
Time the record covers
At most 3.8 million years on record.
Every occurrence read is dated to somewhere between 250.8 Mya and 247 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
7 occurrences of Diaplococeras connectens on record, most of them in the Early Triassic. 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 Triassic100%
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
1 formation
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The named rock units Diaplococeras connectens has been recovered from, largest first. Drawn where the rock is now, not where it formed. 3 occurrences have no formation on record, which is common for older literature.
Diaplococeras connectens and its relatives
Early TriassicWhere Diaplococeras connectens and its relatives were recorded in the Early Triassic.
Found in the same rock
37 taxa- Ladinaticella costata3 sites
- Dinarites dalmatinus2 sites
- Bakevellia exporrecta1 site
- Balkanites tabulatus1 site
- Bittnerites bittneri1 site
- Bittnerithyris margaritovi1 site
- Carniolites neorichianus1 site
- Carniolites planatus1 site
- Carniolites superior1 site
- Dalmatites morlaccus1 site
- Diaplococeras liccanum1 site
- Dinarites carniolicus1 site
- Eumorphotis hinnitidea1 site
- Eumorphotis inaequicostata1 site
- Eumorphotis iwanowi1 site
- Eumorphotis telleri1 site
- Eumorphotis venetiana1 site
- Gervillia1 site
- Hololobus monoptychus1 site
- Myophoria goldfussi1 site
- Naticopsis1 site
- Neomorphotis comta1 site
- Neoschizodus laevigatus1 site
- Omphaloptycha1 site
The Paleobiology Database records 4 sites for Diaplococeras connectens, 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
3 references- Die Cephalopoden der oberen Werfener Schichten von Muć in Dalmatien sowie von anderen dalmatinischen, bosnisch-herzegowinischen und alpinen Lokalitäten4
- Die Cephalopoden der Mediterranen Triasprovinz2
- Untertriassiche Ammoniten aus dem Ostbalkan (Bulgarien)1
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. Each entry links to the Paleobiology Database's own record for the work.
Media and terms
Media content0
No picture of Diaplococeras connectens 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 Diaplococeras connectens, 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 itDiaplococeras through timeFormations of the Early TriassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (von Mojsisovics 1882)