Hyperamminoides
via GBIF · CC0 · 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
- AstrorhizidaePBDB
- Diet
- detritivorePBDB, for Textulariina
- Life habit
- infaunalPBDB, for Textulariina
- Motility
- stationaryPBDB, for Foraminifera
Time the record covers
At least 146 million years on record.
The record covers at least 315.2 Mya to 168.6 Mya. No occurrence read is dated outside 323.4 Mya to 168.2 Mya.
23 occurrences of Hyperamminoides on record, most of them in the Carboniferous. 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
23 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
5 formations
- Johns Valley Formation10
- Djangura Formation4
- Graham Formation · Cisco Group4
- Callytharra Formation2
- ? Thrifty Formation · Cisco Group1
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The named rock units Hyperamminoides has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.
Hyperamminoides and its relatives
CarboniferousWhere Hyperamminoides and its relatives were recorded in the Carboniferous.
Found in the same rock
86 taxa- Nodosinella glennensis7 sites
- Ammodiscus6 sites
- Cornuspira semiconstrictus6 sites
- Hippocrepina bendensis5 sites
- Hyperammina elongata clavatula5 sites
- Polygnathidae5 sites
- Trochammina5 sites
- Amphissites marginiferus4 sites
- Healdia caneyensis4 sites
- Monoceratina ventralis4 sites
- Nodosinella4 sites
- Reophax4 sites
- Ammobaculites3 sites
- Amphissites rugosus3 sites
- Bythocypris tomlinsoni3 sites
- Hyperammina3 sites
- Orobias ciscoensis3 sites
- Paraparchites wapanuckensis3 sites
- Spiroplectammina3 sites
- Ammovertella2 sites
- Calcivertella2 sites
- Cavellina lata2 sites
- Cavellina subovata2 sites
- Climacammina2 sites
The Paleobiology Database records 18 sites for Hyperamminoides, 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- Micropaleontology of the Pennsylvanian Johns Valley shale of the Ouachita Mountains, Oklahoma, and its relationship to the Mississippian Caney shale10
- Foraminifera of the Cisco Group of Texas7
- Ammonites, Microfauna, and Palynomorphs from the Lower Part of the Upper Bajocian Parkinsoni Zone of the Basin of the Bolshoi Zelenchuk River, Northern Caucasus4
- Foraminifera and their habitats within a cool-water carbonate succession following glaciation, Early Permian (Sakmarian), Western Australia2
Each of the 23 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 Hyperamminoides
- Source
- GBIF
- Credit
- via GBIF
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Hyperamminoides 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 itAstrorhizidae through timeFormations of the CarboniferousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0.