Aegiromena descendens
No picture of Aegiromena descendens 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 Aegiromena descendens, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- AegiromenaPBDB
- Diet
- suspension feederPBDB, for Strophomenida
- Life habit
- epifaunalPBDB, for Strophomenida
- Motility
- stationaryPBDB, for Strophomenida
- Vision
- blindPBDB, for Strophomenata
- Environment
- marinePBDB, for Lophophorata
Time the record covers
At most 15 million years on record.
Every occurrence read is dated to somewhere between 459.3 Mya and 445.2 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
12 occurrences of Aegiromena descendens 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
12 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
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The named rock units Aegiromena descendens has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Aegiromena descendens and its relatives
OrdovicianWhere Aegiromena descendens and its relatives were recorded in the Ordovician.
Found in the same rock
197 taxa- Iberomena sardoa5 sites
- Dalmanella4 sites
- Eudolatites angelini4 sites
- Hedstroemina4 sites
- Protomendacella4 sites
- Flexicalymene incerta3 sites
- Jezercia3 sites
- Kloucekia phillipsi3 sites
- Onnia3 sites
- Paterula bohemica3 sites
- Sinuitopsis neglecta3 sites
- Barrandicella tarda2 sites
- Chonetoidea homolensis2 sites
- Ctenodonta2 sites
- Dceruska primula2 sites
- Dicranograptus clingani2 sites
- Diplograptus2 sites
- Grandostoma bohemica2 sites
- Haplospira vermiculosa2 sites
- Hyolithes2 sites
- Lophospira viator2 sites
- Nobiliasaphus2 sites
- Onniella2 sites
- Onnizetina2 sites
The Paleobiology Database records 12 sites for Aegiromena descendens, 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- Late Ordovician and early Silurian brachiopods from the Zagros Ranges, Iran7
- The biostratigraphy of the Ordovician of Bohemia3
- Sinuites community in the Upper Ordovician Bohdalec Formation at Praha-Radotín (Barrandian Area, Czech Republic)1
- Caradoc through early Ashgill brachiopods from the Central-Iberian Zone (central Spain)1
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 Aegiromena descendens 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 Aegiromena descendens, 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 itAegiromena through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Havlicek 1952)