Inaperturopollenites
No picture of Inaperturopollenites was found. Wikipedia, Wikidata and iDigBio were searched and had none. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Inaperturopollenites, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- CupressalesPBDB
- Diet
- "photoautotroph"PBDB, for Streptophyta
Time the record covers
At least 262 million years on record.
The record covers at least 274.4 Mya to 11.63 Mya. No occurrence read is dated outside 298.9 Mya to 3.6 Mya.
250 occurrences of Inaperturopollenites on record, most of them in the Late Cretaceous. 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
250 occurrences- Permian4%
- Early Triassic6%
- Early Jurassicunder 1%
- Middle Jurassic1%
- Late Jurassicunder 1%
- Early Cretaceous32%
- Late Cretaceous32%
- Paleocene4%
- Eocene15%
- Oligocene1%
- Miocene3%
- Plioceneunder 1%
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
47 formations
- Bima Formation · Bornu Basin Group18
- Bathurst Island Formation14
- Fort Union Formation13
- Hell Creek Formation12
- Burg El-Arab Formation11
- Bahariya Formation10
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The named rock units Inaperturopollenites has been recovered from, largest first. Drawn where the rock is now, not where it formed. 23 further formations hold fewer occurrences each and are not listed. 82 occurrences have no formation on record, which is common for older literature.
Inaperturopollenites and its relatives
Late CretaceousWhere Inaperturopollenites and its relatives were recorded in the Late Cretaceous.
Found in the same rock
1,167 taxa- Tricolpites77 sites
- Laevigatosporites74 sites
- Classopollis65 sites
- Tricolporopollenites61 sites
- Cycadopites58 sites
- Deltoidospora57 sites
- Ephedripites57 sites
- Botryococcus52 sites
- Triporopollenites52 sites
- Cicatricosisporites50 sites
- Afropollis jardinus46 sites
- Araucariacites australis46 sites
- Gleicheniidites46 sites
- Pityosporites39 sites
- Retimonocolpites39 sites
- Ephedripites multicostatus38 sites
- Concavisporites37 sites
- Liliacidites34 sites
- Monocolpopollenites32 sites
- Osmundacidites32 sites
- Monosulcites30 sites
- Taxodiaceaepollenites29 sites
- Momipites28 sites
- Triatriopollenites28 sites
The Paleobiology Database records 196 sites for Inaperturopollenites, 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
51 references- Vegetation dynamics in a disturbed lacustrine record: The Eocene maar lake of Groß-Zimmern (Hesse, Germany)26
- Biostratigraphy of selected K/T boundary sections in southwestern North Dakota, USA: toward a refinement of palynological identification criteria25
- Palynological Investigation of the Albian to Lower Cenomanian Bima Formation, Bornu Basin, Nigeria21
- Jurassic-Cretaceous (Bathonian to Cenomanian) palynology and stratigraphy of the West Tiba-1 borehole, northern Western Desert, Egypt18
- Aptian-Turonian palynology of the Ghazalat-1 well (GTX-1), Qattara Depression, Egypt18
- Palynostratigraphy of the Permian and lowermost Triassic succession, Finnmark Platform, Barents Sea.16
- Palynology of the Cenomanian of Bathurst Island, Northern Territory, Australia14
- Palynological study of the Early Cretaceous Kurnub Sandstone Formation, Mahis area, Central Jordan10
- Palynozonation of the Cretaceous to Lower Paleogene Strata of the Muglad Basin, Sudan10
- Late Cretaceous spore-pollen zonation of the Central African Rift System (CARS), Kaikang Trough, Muglad Basin, South Sudan: angiosperm spread and links to the Elaterates Province9
- Palynologuie et stratigraphie du Crétacé des Bassin du Sénégal et Cote d'Ivoire7
- Distribution of pollen and spores in a subsurface marine Wilcox (Paleocene-Eocene) section in southwest Louisiana6
Each of the 250 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. 39 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 content0
No picture of Inaperturopollenites was found. Wikipedia, Wikidata and iDigBio were searched and had none.
Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Inaperturopollenites, or no answer at all. This entry cannot say which.
No 3D scan of Inaperturopollenites 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 itCupressales through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Potonié 1966