Hindeodus
Hindeodus is an extinct genus of conodonts in the family Anchignathodontidae. The generic name Hindeodus is a tribute to George Jennings Hinde, a British geologist and paleontologist from the 1800s and early 1900s. The suffix -odus typically describes the animal's teeth, essentially making Hindeodus mean Hinde-teeth.

Muhui Zhang, Haishui Jiang, Mark A. Purnell, Xulong Lai · 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
- AnchignathodontidaePBDB
- Diet
- carnivorePBDB, for Conodonta
- Life habit
- nektonicPBDB, for Conodonta
- Motility
- actively mobilePBDB, for Conodonta
- Vision
- well-developedPBDB, for Conodonta
Time the record covers
At least 109 million years on record.
The record covers at least 346.7 Mya to 237 Mya. No occurrence read is dated outside 358.86 Mya to 201.4 Mya.
354 occurrences of Hindeodus on record, most of them in the Early Triassic. 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
354 occurrences- Carboniferous14%
- Permian29%
- Early Triassic56%
- Middle Triassicunder 1%
- Late Triassicunder 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
41 formations
- Daye Formation80
- Changxing Formation56
- Majiaoling Formation20
- Black Rock Limestone Formation18
- Khunamuh Formation16
- Werfen Formation12
Loading coastlines…
The named rock units Hindeodus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 17 further formations hold fewer occurrences each and are not listed. 62 occurrences have no formation on record, which is common for older literature.
Hindeodus and its relatives
Early TriassicWhere Hindeodus and its relatives were recorded in the Early Triassic.
Found in the same rock
612 taxa- Clarkina33 sites
- Isarcicella27 sites
- Gnathodus23 sites
- Polygnathus20 sites
- Claraia19 sites
- Idiognathodus18 sites
- Fasciculophyllum17 sites
- Ophiceras16 sites
- Spathognathodus16 sites
- Promyalina15 sites
- Caninia cornucopiae13 sites
- Pseudopolygnathus13 sites
- Eumorphotis12 sites
- Naticopsis12 sites
- Hemigordius11 sites
- Endothyra10 sites
- Gastropoda10 sites
- Isarcicella isarcica10 sites
- Neogondolella carinata10 sites
- Cavusgnathus9 sites
- Crinoidea9 sites
- Cyathoclisia9 sites
- Michelinia9 sites
- Neogondolella9 sites
The Paleobiology Database records 183 sites for Hindeodus, 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
53 references- Conodont and Ammonoid Biostratigraphies around the Permian-Triassic Boundary from the Jianzishan of South China70
- Rapid biotic rebound during the late Griesbachian indicates heterogeneous recovery patterns after the Permian-Triassic mass extinction60
- A unique Permian-Triassic boundary section from the Neotethyan Hawasina Basin, Central Oman Mountains25
- Conodonts and Carbon Isotopes during the Permian-Triassic Transition on the Napo Platform, South China20
- The distribution of platform conodonts, corals, and foraminifera from the Black Rock Limestone (late Tournaisian and early Visean) of Tears Point, Gower, south Wales18
- New data from Oman indicate benthic high biomass productivity coupled with low taxonomic diversity in the aftermath of the Permian–Triassic Boundary mass extinction13
- The Otoceras woodwardi Zone and the time-gap at the Permian-Triassic boundary in east Asia13
- A sudden end-Permian mass extinction in South China12
- Environmental and biotic turnover across the Permian-Triassic boundary on a shallow carbonate platform in western Zhejiang, South China12
- Environmental and biotic changes across the Permian-Triassic boundary in western Tethys: The Bulla parastratotype, Italy10
- Stratigraphy and regional significance of Mississippian to Jurassic rocks in Sierra Santa Teresa, Sonora, Mexico8
- The Meishan Section, Candidate of the global stratotype section and point of Permian-Triassic boundary8
Each of the 354 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. 41 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 content1
Picture of Hindeodus
- Source
- Wikipedia/Commons
- Credit
- Muhui Zhang, Haishui Jiang, Mark A. Purnell, Xulong Lai
- Licence
- CC BY 4.0
- Commercial use
- the licence allows it
No 3D scan of Hindeodus was found in MorphoSource and Sketchfab.
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Source
- Wikipedia, “Hindeodus”
- 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 itAnchignathodontidae through timeFormations of the Early TriassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Rexroad and Furnish 1964