Eocatenipora parallela

via GBIF · CC BY-NC 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
- EocateniporaPBDB
- Diet
- suspension feeder, photosymbioticPBDB, for Tabulata
- Life habit
- epifaunalPBDB, for Tabulata
- Motility
- stationary, attachedPBDB, for Tabulata
- Vision
- blindPBDB, for Anthozoa
Time the record covers
At most 9.7 million years on record.
Every occurrence read is dated to somewhere between 452.8 Mya and 443.1 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
10 occurrences of Eocatenipora parallela 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
10 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 Eocatenipora parallela has been recovered from, largest first. Drawn where the rock is now, not where it formed. 7 occurrences have no formation on record, which is common for older literature.
Eocatenipora parallela and its relatives
OrdovicianWhere Eocatenipora parallela and its relatives were recorded in the Ordovician.
Found in the same rock
58 taxa- Ecclimadictyon porkuni2 sites
- Palaeofavosites porkuniensis2 sites
- Plumatalinia ferax2 sites
- Rhabdotetradium frutex2 sites
- Stenocamara biohermica2 sites
- Strombodes middendorfi2 sites
- Amplocularia sp.1 site
- Apendispinograptus supernus1 site
- Aphyllum1 site
- Barbarorthis porkuniensis1 site
- Boreadorthis sadewitzensis1 site
- Brachielasma sp.1 site
- Brachyelasma duncani1 site
- Catenipora rubraeformis1 site
- Chasmatoporella1 site
- Clathrodictyon gregale1 site
- Clathrodictyon zonatum1 site
- Clathropora1 site
- Climacograptus1 site
- Coccoseris tumulosus1 site
- Codonophyllum bekkeri1 site
- Codonophyllum rhizobolon1 site
- Dicellograptus1 site
- Dicellograptus anceps1 site
The Paleobiology Database records 9 sites for Eocatenipora parallela, 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- The Incommunicate Tabulata of Estonia7
- Ordovician Sedimentary Basin and Paleobiotas of the Gorny Altai1
- Stratotype of the Porkuni Stage with comments on the Röa Member (uppermost Ordovician, Estonia)1
- Stratigrafiya i fauna ordovika i silura Chukotskogo poluostrova [Stratigraphy and fauna of the Ordovician and the Silurian of the Chukotsk Peninsula]1
Each of the 10 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 Eocatenipora parallela
- Source
- GBIF
- Credit
- via GBIF
- Licence
- CC BY-NC 4.0
- Commercial use
- the licence does not allow it
No 3D scan of Eocatenipora parallela 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 itEocatenipora through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Schmidt 1858)