Liuzhinia guangxiensis

No picture of Liuzhinia guangxiensis 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 Liuzhinia guangxiensis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
LiuzhiniaPBDB
Diet
detritivore, grazerPBDB, for Podocopida
Life habit
epifaunalPBDB, for Podocopida
Motility
actively mobilePBDB, for Ostracoda
Vision
limitedPBDB, for Ostracoda
Environment
marinePBDB, for Ostracoda

Time the record covers

At least 2.5 million years on record.

The record covers at least 251.1 Mya to 248.6 Mya. No occurrence read is dated outside 251.902 Mya to 247 Mya.

Permian — about 0 of 9 occurrencesEarly Triassic — about 9 of 9 occurrencesEarly TriassicMiddle Triassic — about 0 of 9 occurrences252–252 Mya — about 0.1 occurrences252–252 Mya — about 0.2 occurrences252–251 Mya — about 0.2 occurrences251–251 Mya — about 0.2 occurrences251–251 Mya — about 0.2 occurrences249–248 Mya — about 0.7 occurrences248–248 Mya — about 1.0 occurrences248–248 Mya — about 1.0 occurrences248–248 Mya — about 1.0 occurrences248–248 Mya — about 1.0 occurrences248–247 Mya — about 1.0 occurrences247–247 Mya — about 1.0 occurrences247–247 Mya — about 1.0 occurrences247–247 Mya — about 0.5 occurrences251.1 Mya248.6 Mya252.4 Mya246.5 Mya

9 occurrences of Liuzhinia guangxiensis 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

9 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

3 formations

Luolou — 24.58°N, 106.89°ETulong — 28.44°N, 86.14°EKokarkuyu — 36.69°N, 30.46°E

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The named rock units Liuzhinia guangxiensis has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Liuzhinia guangxiensis and its relatives

Early Triassic

Where Liuzhinia guangxiensis and its relatives were recorded in the Early Triassic.

Found in the same rock

29 taxa

The Paleobiology Database records 9 sites for Liuzhinia guangxiensis, 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

3 references

Each of the 9 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 Liuzhinia guangxiensis 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 Liuzhinia guangxiensis, or no answer at all. This entry cannot say which.

No 3D scan of Liuzhinia guangxiensis 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 itLiuzhinia through timeFormations of the Early TriassicThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Crasquin-Soleau 2006