Diacalymene consimilis

via iDigBio · CC0 · via iDigBio. 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
- DiacalymenePBDB
- Diet
- carnivorePBDB, for Calymenidae
- Life habit
- nektobenthicPBDB, for Calymenidae
- Motility
- actively mobilePBDB, for Calymenidae
- Vision
- well-developedPBDB, for Calymenidae
- Environment
- marinePBDB, for Trilobita
Time the record covers
At most 19 million years on record.
Every occurrence read is dated to somewhere between 451 Mya and 432.9 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
11 occurrences of Diacalymene consimilis 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
11 occurrences- Ordovician91%
- Silurian9%
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
- White Head Formation · Matapédia Group7
- Grande Coupe Formation3
- Grande Coupe Beds Formation · Matapedia Group1
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The named rock units Diacalymene consimilis has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Diacalymene consimilis and its relatives
OrdovicianWhere Diacalymene consimilis and its relatives were recorded in the Ordovician.
Found in the same rock
106 taxa- Lonchodomas7 sites
- Calyptaulax glabella6 sites
- Tretaspis6 sites
- Cyclospira5 sites
- Leangella (Leangella) septata5 sites
- Microparia (Heterocyclopyge) insolens5 sites
- Microparia (Heterocyclopyge) kindlei5 sites
- Stenopareia perceensis5 sites
- Calyptaulax4 sites
- Cliftonia4 sites
- Spirigerina (Eospirigerina) gaspeensis4 sites
- Stenopareia4 sites
- Cyclopyge vigilans3 sites
- Encrinurus3 sites
- Otarion3 sites
- Symphysops3 sites
- Symphysops spinifera3 sites
- Ceraurinus icarus2 sites
- Ceraurus2 sites
- Cheirurus percensis2 sites
- Christiania2 sites
- Cyclopyge2 sites
- Cyphoproetus bellus2 sites
- Eophacops2 sites
The Paleobiology Database records 11 sites for Diacalymene consimilis, 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
5 references- New brachiopods and trilobites from the Ordovician of Perce, Quebec6
- Ordovician and Silurian trilobite faunas of the White Head Formation, Percé Region, Québec2
- Gaspé Peninsula, Percé area1
- The occurrence of the Ordovician brachiopod Foliomena at Percé, Quebec1
- Lower Llandovery of the Northern Appalachians and Adjacent Regions1
Each of the 11 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 Diacalymene consimilis
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Diacalymene consimilis 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 itDiacalymene through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Schuchert and Cooper 1930)