Glabrocingulum (Stenozone) lyndonensis

No picture of Glabrocingulum (Stenozone) lyndonensis was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Glabrocingulum (Stenozone) lyndonensis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
StenozonePBDB
Diet
detritivorePBDB, for Gosseletinidae
Life habit
epifaunalPBDB, for Gosseletinidae
Motility
slow-movingPBDB, for Gosseletinidae
Vision
limitedPBDB, for Gosseletinidae
Environment
coastal,marinePBDB, for Murchisoniina

Time the record covers

At least 15 million years on record.

The record covers at least 290.1 Mya to 274.4 Mya. No occurrence read is dated outside 293.52 Mya to 259.857 Mya.

Permian — about 3 of 3 occurrencesPermian294–293 Mya — about 0.3 occurrences293–292 Mya — about 0.7 occurrences292–291 Mya — about 0.7 occurrences291–290 Mya — about 0.3 occurrences276–274 Mya — about 0.0 occurrences274–273 Mya — about 0.1 occurrences273–272 Mya — about 0.1 occurrences272–271 Mya — about 0.1 occurrences271–270 Mya — about 0.1 occurrences270–269 Mya — about 0.1 occurrences269–267 Mya — about 0.1 occurrences267–266 Mya — about 0.1 occurrences266–265 Mya — about 0.1 occurrences265–264 Mya — about 0.1 occurrences264–263 Mya — about 0.1 occurrences263–262 Mya — about 0.1 occurrences262–260 Mya — about 0.1 occurrences260–259 Mya — about 0.0 occurrences290.1 Mya274.4 Mya294.2 Mya259.2 Mya

3 occurrences of Glabrocingulum (Stenozone) lyndonensis on record, most of them in the Permian. 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

3 occurrences

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

2 formations

Carrandibby — 25.85°S, 115.29°EZhesi — 43.98°N, 114.95°E

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The named rock units Glabrocingulum (Stenozone) lyndonensis 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.

Glabrocingulum (Stenozone) lyndonensis and its relatives

Permian

Where Glabrocingulum (Stenozone) lyndonensis and its relatives were recorded in the Permian.

Found in the same rock

13 taxa

The Paleobiology Database records 3 sites for Glabrocingulum (Stenozone) lyndonensis, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

3 references

Each of the 3 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 Glabrocingulum (Stenozone) lyndonensis was found. Wikidata and iDigBio were searched and had none.

Wikipedia and 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 Glabrocingulum (Stenozone) lyndonensis, or no answer at all. This entry cannot say which.

No 3D scan of Glabrocingulum (Stenozone) lyndonensis 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.

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itStenozone through timeFormations of the PermianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Dickins 1957)