Homotrypa alta

No picture of Homotrypa alta 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 Homotrypa alta, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
HomotrypaPBDB
Diet
suspension feederPBDB, for Stenolaemata
Life habit
epifaunalPBDB, for Bryozoa
Motility
stationary, attachedPBDB, for Stenolaemata
Vision
blindPBDB, for Stenolaemata
Environment
marinePBDB, for Lophophorata

Time the record covers

At least 800 thousand years on record.

The record covers at least 449.6 Mya to 448.8 Mya. No occurrence read is dated outside 450.2 Mya to 445.2 Mya.

Ordovician — about 2 of 2 occurrencesOrdovician450–450 Mya — about 0.2 occurrences450–450 Mya — about 0.3 occurrences450–450 Mya — about 0.3 occurrences450–450 Mya — about 0.2 occurrences449–449 Mya — about 0.0 occurrences449–449 Mya — about 0.1 occurrences449–448 Mya — about 0.1 occurrences448–448 Mya — about 0.1 occurrences448–448 Mya — about 0.1 occurrences448–448 Mya — about 0.1 occurrences448–448 Mya — about 0.1 occurrences448–447 Mya — about 0.1 occurrences447–447 Mya — about 0.1 occurrences447–447 Mya — about 0.1 occurrences447–447 Mya — about 0.1 occurrences447–447 Mya — about 0.1 occurrences447–446 Mya — about 0.1 occurrences446–446 Mya — about 0.1 occurrences446–446 Mya — about 0.1 occurrences446–446 Mya — about 0.1 occurrences446–446 Mya — about 0.1 occurrences446–445 Mya — about 0.1 occurrences445–445 Mya — about 0.0 occurrences449.6 Mya448.8 Mya450.7 Mya444.7 Mya

2 occurrences of Homotrypa alta on record, most of them in the Ordovician. 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

2 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

Fairview — 39.17°N, 84.91°WKhabt-el-Hajar — 31.41°N, 4.11°W

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

Homotrypa alta and its relatives

Ordovician

Where Homotrypa alta and its relatives were recorded in the Ordovician.

Found in the same rock

7 taxa

The Paleobiology Database records 2 sites for Homotrypa alta, 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

1 reference

Each of the 2 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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Homotrypa alta 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 Homotrypa alta, or no answer at all. This entry cannot say which.

No 3D scan of Homotrypa alta was found in Sketchfab.

Smithsonian Open Access and MorphoSource were 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 itHomotrypa through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Cumings and Galloway 1913