Bradyina cribrostomata
No picture of Bradyina cribrostomata was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Bradyina cribrostomata, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- BradyinaPBDB
- Diet
- omnivorePBDB, for Foraminifera
- Life habit
- semi-infaunalPBDB, for Foraminifera
- Motility
- stationaryPBDB, for Foraminifera
Time the record covers
At most 16 million years on record.
Every occurrence read is dated to somewhere between 330.3 Mya and 315.2 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
8 occurrences of Bradyina cribrostomata 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
8 occurrences- Carboniferous100%
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 Bradyina cribrostomata has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Bradyina cribrostomata and its relatives
CarboniferousWhere Bradyina cribrostomata and its relatives were recorded in the Carboniferous.
Found in the same rock
25 taxa- Biseriella parva7 sites
- Earlandia7 sites
- Endothyra7 sites
- Eostaffellidae7 sites
- Globivalvulina bulloides7 sites
- Mediocris breviscula7 sites
- Palaeonubecularia7 sites
- Asteroarchaediscus6 sites
- Pseudoglomospira6 sites
- Eostaffella5 sites
- Neoarchaediscus5 sites
- Plectostaffella jakhensis5 sites
- Climacammina3 sites
- Eostaffella postmosquensis3 sites
- Palaeotextularia3 sites
- Palaeotextulariidae3 sites
- Endotaxis brazhnikovae2 sites
- Haplophragmina2 sites
- Tetrataxis2 sites
- Turrispiroides2 sites
- Climacammina valvulinoides1 site
- Eostaffella postmosquensis acutiformis1 site
- Glomospiroides1 site
- Plectostaffella1 site
The Paleobiology Database records 7 sites for Bradyina cribrostomata, 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
2 references- Calcareous foraminifers from the Bashkirian Stratotype (Middle Carboniferous, South Urals)and their significance for intercontinental correlations and the evolution of the Fusulinidae7
- Algues et pseudo-algues des calcaires Serpoukhoviens d'Ardengost (Hautes-Pyrenees) [Algues and pseudo-algues from Serpukhovian Limestones of Ardengost (Hautes-Pyrenees)]1
Each of the 8 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 content0
No picture of Bradyina cribrostomata was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Bradyina cribrostomata, or no answer at all. This entry cannot say which.
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itBradyina through timeFormations of the CarboniferousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Rauser-Chernousova and Reitlinger 1937