Condranema magna
via iDigBio · CC BY-NC-SA · 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
- CondranemaPBDB
- Diet
- suspension feederPBDB, for Condranema
- Life habit
- boringPBDB, for Condranema
- Motility
- stationaryPBDB, for Condranema
- Vision
- blindPBDB, for Gymnolaemata
- Environment
- marinePBDB, for Lophophorata
Time the record covers
At least 29 million years on record.
The record covers at least 323.4 Mya to 293.52 Mya. No occurrence read is dated outside 330.3 Mya to 290.1 Mya.
37 occurrences of Condranema magna on record, most of them in the Permian. 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
37 occurrences- Carboniferous3%
- Permian97%
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
- Wreford Formation · Council Grove Group34
- Hueco Formation2
- Redoak Hollow Formation1
Loading coastlines…
The named rock units Condranema magna has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Condranema magna and its relatives
PermianWhere Condranema magna and its relatives were recorded in the Permian.
Found in the same rock
218 taxa- Rhombopora lepidodendroides30 sites
- Septopora spinulosa28 sites
- Syringoclemis wrefordensis24 sites
- Acanthocladia guadalupensis23 sites
- Rectifenestella tenax23 sites
- Tabulipora carbonaria20 sites
- Minilya binodata17 sites
- Spinofenestella spinulosa16 sites
- Penniretepora curvula11 sites
- Fistulipora incrustans10 sites
- Polypora elliptica10 sites
- Penniretepora auernigiana7 sites
- Penniretepora flexistriata7 sites
- Polypora aestacella5 sites
- Fistulipora carbonaria4 sites
- Meekopora prosseri4 sites
- Aviculopecten3 sites
- Polypora3 sites
- Tabulipora3 sites
- Acharax radiata2 sites
- Bakevellia sulcata2 sites
- Bellerophontoidea2 sites
- Composita2 sites
- Composita bucculenta2 sites
The Paleobiology Database records 37 sites for Condranema magna, 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- Stratigraphic and Geographic Bryozoan Abundance Gradients in the Calcareous Shales of the Wreford Megacyclothem (Lower Permian, Kansas)32
- Marine fauna of the Early Permian (Wolfcampian) Robledo Mountains Member, Hueco Formation, southern Robledo Mountains, New Mexico2
- Fenestrate, pinnate, and ctenostome bryozoans and associated barnacle borings in the Wreford Megacyclothem (Lower Permian) of Kansas, Oklahoma, and Nebraska2
- Late Mississippian fauna from the Redoak Hollow Formation of southern Oklahoma, Part I1
Each of the 37 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 content1
Picture of Condranema magna
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC BY-NC-SA
- Commercial use
- the licence does not allow it
No 3D scan of Condranema magna 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 itCondranema through timeFormations of the PermianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Condra and Elias 1944)