Teichichnus rectus

No picture of Teichichnus rectus was found. Wikipedia and Wikidata were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Teichichnus rectus firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

On record

Recorded, not inferred
Sits inside
TeichichnusPBDB

Time the record covers

At least 506 million years on record.

The record covers at least 512.1 Mya to 5.333 Mya. No occurrence read is dated outside 516 Mya to 3.6 Mya.

Cambrian — about 2 of 4 occurrencesOrdovician — about 1 of 4 occurrencesOrdovicianSilurian — about 0 of 4 occurrencesDevonian — about 0 of 4 occurrencesCarboniferous — about 0 of 4 occurrencesPermian — about 0 of 4 occurrencesEarly Triassic — about 0 of 4 occurrencesMiddle Triassic — about 0 of 4 occurrencesLate Triassic — about 0 of 4 occurrencesEarly Jurassic — about 0 of 4 occurrencesMiddle Jurassic — about 0 of 4 occurrencesLate Jurassic — about 0 of 4 occurrencesEarly Cretaceous — about 0 of 4 occurrencesLate Cretaceous — about 0 of 4 occurrencesPaleocene — about 0 of 4 occurrencesEocene — about 0 of 4 occurrencesOligocene — about 0 of 4 occurrencesMiocene — about 0 of 4 occurrencesPliocene — about 1 of 4 occurrencesPleistocene — about 0 of 4 occurrences526–509 Mya — about 2 occurrences491–474 Mya — about 1 occurrence18–0 Mya — about 1 occurrence512.1 Mya5.333 Mya526 Mya0 Mya

4 occurrences of Teichichnus rectus on record, most of them in the Cambrian. 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

4 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

Ocieseki Sandstone — 50.90°N, 20.90°EBeach — 47.62°N, 52.94°W

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The named rock units Teichichnus rectus 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.

Teichichnus rectus and its relatives

Cambrian

Where Teichichnus rectus and its relatives were recorded in the Cambrian.

Found in the same rock

15 taxa

The Paleobiology Database records 1 site for Teichichnus rectus, 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 4 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 Teichichnus rectus was found. Wikipedia and Wikidata were searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Teichichnus rectus firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.

Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

No 3D scan of Teichichnus rectus 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. Seilacher 1955