Kallokibotion
Kallokibotion is an extinct genus of stem-turtle from the Upper Cretaceous, known from fossils found in Romania. One species is known, Kallokibotion bajazidi, which was named by Franz Nopcsa after his lover Bajazid Doda. It literally means 'beautiful box of Bajazid'; Nopcsa chose the name because, in the words of British palaeontologist Gareth Dyke, "the shape of the shell reminded him of Bajazid's arse". A second undescribed species is known from the Santonian of Hungary. Turtles similar to Kallokibotion were reported from the Paleocene of France and the Lower Maastrichtian of Volgograd Oblast, Russia, but these similarities were dismissed later.

Gyik Toma (Tommy the paleobear) from Romania · CC BY 2.0 · 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
- TestudinataPBDB
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Diapsida
Time the record covers
At least 11 million years on record.
The record covers at least 83.6 Mya to 72.2 Mya. No occurrence read is dated outside 85.7 Mya to 66 Mya.
28 occurrences of Kallokibotion 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
28 occurrences- Late Cretaceous100%
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
8 formations
- Densuș-Ciula Formation9
- Sebeş Formation6
- Sînpetru Formation4
- Şard Formation3
- Râul Mare Formation2
- Grünbach Formation · Gosau Group1
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The named rock units Kallokibotion 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.
Kallokibotion and its relatives
Late CretaceousWhere Kallokibotion and its relatives were recorded in the Late Cretaceous.
Found in the same rock
218 taxa- Zalmoxes17 sites
- Dortokidae11 sites
- Dinosauria10 sites
- Doratodon10 sites
- Telmatosaurus10 sites
- Theropoda9 sites
- Titanosauria9 sites
- Allodaposuchus8 sites
- Albanerpeton7 sites
- Anura7 sites
- Gastropoda7 sites
- Paronychodon7 sites
- Allodaposuchus precedens6 sites
- Struthiosaurus6 sites
- Velociraptorinae6 sites
- Acynodon5 sites
- Albanerpetontidae5 sites
- Crocodyliformes5 sites
- Ferenceratops shqiperorum5 sites
- Multituberculata5 sites
- Paralatonia transylvanica5 sites
- Richardoestesia5 sites
- Testudines5 sites
- Kogaionidae4 sites
The Paleobiology Database records 28 sites for Kallokibotion, 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
13 references- ‘X’ marks the spot! Sedimentological, geochemical and palaeontological investigations of upper Cretaceous (Maastrichtian) vertebrate fossil localities from the Vălioara valley (Densuş-Ciula Formation, Hațeg basin, Romania)4
- An infant ornithopod dinosaur tibia from the Late Cretaceous of Sebes, Romania4
- Taphonomic modes in the Maastrichtian continental deposits of the Haţeg Basin, Romania—palaeoecological and palaeobiological inferences3
- New latest Cretaceous microvertebrate fossil assemblages from the Haţeg Basin (Romania)3
- A Review of the Fossil Record of Basal Mesozoic Turtles2
- New insights on the anatomy and systematics of Kallokibotion Nopcsa, 1923, the enigmatic uppermost Cretaceous basal turtle (stem Testudines) from Transylvania2
- The East Side Story – The Transylvanian latest Cretaceous continental vertebrate record and its implications for understanding Cretaceous–Paleogene boundary events2
- More than just Nopcsa's Transylvanian dinosaurs: A look outside the Hateg Basin2
- New faunal elements from the Late Cretaceous (Maastrichtian) continental deposits of Sebeş area (Transylvania)2
- Paleontological and paleoecological significance of the oldest highly productive Upper Cretaceous (lowermost Maastrichtian) bonebed of Haţeg Basin (western Romania; Densuş-Ciula Formation)1
- Upper Cretaceous (Maastrichtian) landvertebrate diversity in Alba District (Romania)1
- The Budurone microvertebrate site from the Maastrichtian of the Hateg Basin – flora, fauna, taphonomy and paleoenvironment1
Each of the 28 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. 1 further reference is 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 Kallokibotion
- Source
- Wikipedia/Commons
- Credit
- Gyik Toma (Tommy the paleobear) from Romania
- Licence
- CC BY 2.0
- Commercial use
- the licence allows it
CT scan
- Source
- MorphoSource
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Kallokibotion bajazidi · NHMUK:PAL:PV R 4925
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 itTestudinata through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0.