Charniodiscus
Charniodiscus is an Ediacaran fossil that in life was probably a stationary filter feeder that lived anchored to a sandy sea bed. The organism had a holdfast, stalk and frond. The holdfast was bulbous shaped, and the stalk was flexible. The frond was segmented and had a pointed tip. There were two growth forms: one with a short stem and a wide frond, and another with a long stalk, elevating a smaller frond about 50 centimetres (20 in) above the holdfast. While the organism superficially resembles the sea pens (cnidaria), it is probably not a crown-group animal.

Daniel Pérez-Pinedo, Christopher McKean, Rod Taylor, Duncan McIlroy · CC BY 4.0 · via Wikipedia/Commons. 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
- ArboreomorphaPBDB
- Diet
- osmotroph, suspension feederPBDB
- Life habit
- upper-level epifaunalPBDB
- Motility
- stationary, attachedPBDB
- Environment
- marinePBDB
Time the record covers
At most 97 million years on record.
Every occurrence read is dated to somewhere between 635 Mya and 538.8 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
59 occurrences of Charniodiscus on record. 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
59 occurrencesThese 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
21 formations
- Rawnsley Quartzite Formation · Wilpena Group9
- Mistaken Point Formation · Conception Group9
- Fermeuse Formation · St John's Group7
- Bradgate Formation · Maplewell Group5
- Trepassey Formation · St John's Group5
- Siltstone Unit 1 Formation3
Loading coastlines…
The named rock units Charniodiscus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.
Found in the same rock
141 taxa- Aspidella terranovica19 sites
- Charnia masoni16 sites
- Primocandelabrum13 sites
- Bradgatia linfordensis12 sites
- Aspidella11 sites
- Hiemalora stellaris8 sites
- Pectinifrons abyssalis8 sites
- Vinlandia antecedens8 sites
- Parvancorina minchami6 sites
- Primocandelabrum hiemaloranum6 sites
- Thectardis avalonensis6 sites
- Tribrachidium heraldicum6 sites
- Arborea arborea5 sites
- Arborea spinosa5 sites
- Charnia5 sites
- Fractofusus andersoni5 sites
- Beothukis mistakensis4 sites
- Dickinsonia tenuis4 sites
- Hadryniscala avalonica4 sites
- Ivesheadia lobata4 sites
- Kimberella quadrata4 sites
- Medusinites asteroides4 sites
- Palaeopascichnus4 sites
- Planolites montanus4 sites
The Paleobiology Database records 58 sites for Charniodiscus, 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
29 references- Ediacaran biota on Bonavista Peninsula, Newfoundland, Canada12
- Ediacaran biota of the Wernecke Mountains, Yukon, Canada6
- A Chronostratigraphic Framework for the Rise of the Ediacaran Macrobiota: New Constraints from Mistaken Point Ecological Reserve, Newfoundland4
- How well do fossil assemblages of the Ediacara Biota tell time?4
- Morphometric analysis of the Ediacaran frond Charniodiscus from the Mistaken Point Formation, Newfoundland3
- Ediacaran fossils from the Sekwi Brock Area, Mackenzie Mountains, Northwestern Canada3
- Supplemental Data for Ediacaran Diversification Rates2
- How diverse were early animal communities? An example from Ediacara Conservation Park, Flinders Ranges, South Australia2
- Reconstruction of Charniodiscus yorgensis (Macrobiota from the Vendian of the White Sea)2
- A review of the frond-like fossils of the Ediacara Assemblage2
- Biotic replacement and mass extinction of the Ediacara biota1
- Ediacaran biota in the aftermath of the Kotlinian Crisis: Asha Group of the South Urals1
Each of the 59 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. 17 further references are not listed. 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 content2
Picture of Charniodiscus
- Source
- Wikipedia/Commons
- Credit
- Daniel Pérez-Pinedo, Christopher McKean, Rod Taylor, Duncan McIlroy
- Licence
- CC BY 4.0
- Commercial use
- the licence allows it
3D model
- Source
- Sketchfab
- Licence
- CC Attribution-NonCommercial
- Commercial use
- the licence does not allow it
Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itArboreomorpha through time
Occurrence data from the Paleobiology Database, CC BY 4.0. Ford 1958