Eridophyllum seriale
via iDigBio · CC BY · 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
- EridophyllumPBDB
- Diet
- suspension feederPBDB, for Rugosa
- Life habit
- epifaunalPBDB, for Rugosa
- Motility
- stationary, attachedPBDB, for Rugosa
- Vision
- blindPBDB, for Anthozoa
- Environment
- marinePBDB, for Rugosa
Time the record covers
At least 55 million years on record.
The record covers at least 443.1 Mya to 387.95 Mya. No occurrence read is dated outside 449.5 Mya to 385.9 Mya.
6 occurrences of Eridophyllum seriale on record, most of them in the Devonian. 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
6 occurrences- Ordovician17%
- Devonian83%
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
5 formations
- Jeffersonville Limestone Formation2
- Amherstburg Formation1
- Bou Dib Formation1
- Queenston Formation1
- Anderdon Limestone Formation1
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The named rock units Eridophyllum seriale has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Eridophyllum seriale and its relatives
DevonianWhere Eridophyllum seriale and its relatives were recorded in the Devonian.
Found in the same rock
148 taxa- Cladopora4 sites
- Siphonophrentis4 sites
- Cystiphylloides3 sites
- Favosites3 sites
- Heliophyllum3 sites
- Hexagonaria3 sites
- Hoareicardia cunea3 sites
- Acinophyllum2 sites
- Atrypa2 sites
- Aulopora2 sites
- Blothrophyllum2 sites
- Camarotoechia2 sites
- Disphyllum2 sites
- Emmonsia2 sites
- Fistulipora2 sites
- Heterophrentis2 sites
- Megastrophia2 sites
- Meristina nasuta2 sites
- Pleurodictyum2 sites
- Romingeria2 sites
- Spirifer2 sites
- Sulcoretepora2 sites
- Syringopora hisingeri2 sites
- Thamnopora2 sites
The Paleobiology Database records 5 sites for Eridophyllum seriale, 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- Colored Clays in a Groundwater Stream, Correlating Fiber-optic Reflectance with Electrical Impedance1
- The Middle Devonian "coral reef" of Ouihlane (Morocco) - New data on the geology and rugose coral fauna1
- Paleoecological Analysis of Corals and Stromatoporoids in a Devonian Biostrome, Falls of the Ohio, Kentucky-Indiana1
- Silurian and Devonian Corals of the Falls of the Ohio1
- The fauna of the Middle Devonian Formosa Reef Limestone of southwestern Ontario1
- Middle Devonian Columbus Limestone Near Ingersoll, Ontario, Canada1
Each of the 6 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 Eridophyllum seriale
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC BY
- Commercial use
- the licence allows it
No 3D scan of Eridophyllum seriale was found in MorphoSource and Sketchfab.
Smithsonian Open Access was 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 itEridophyllum through timeFormations of the DevonianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Milne-Edwards and Haime 1850