Holopea obliqua

Holopea obliqua

via iDigBio · CC0 · via iDigBio. 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
HolopeaPBDB
Diet
suspension feederPBDB, for Euomphaloidea
Life habit
epifaunalPBDB, for Euomphaloidea
Motility
stationaryPBDB, for Euomphaloidea
Vision
limitedPBDB, for Gastropoda

Time the record covers

At most 7.7 million years on record.

Every occurrence read is dated to somewhere between 457.3 Mya and 449.6 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Ordovician — about 5 of 5 occurrencesOrdovician458–457 Mya — about 0.1 occurrences457–457 Mya — about 0.2 occurrences457–457 Mya — about 0.2 occurrences457–456 Mya — about 0.2 occurrences456–456 Mya — about 0.2 occurrences456–456 Mya — about 0.2 occurrences456–455 Mya — about 0.2 occurrences455–455 Mya — about 0.2 occurrences455–455 Mya — about 0.2 occurrences455–455 Mya — about 0.2 occurrences455–454 Mya — about 0.2 occurrences454–454 Mya — about 0.2 occurrences454–454 Mya — about 0.2 occurrences454–453 Mya — about 0.2 occurrences453–453 Mya — about 0.2 occurrences453–453 Mya — about 0.2 occurrences453–453 Mya — about 0.2 occurrences453–452 Mya — about 0.2 occurrences452–452 Mya — about 0.2 occurrences452–452 Mya — about 0.2 occurrences452–451 Mya — about 0.2 occurrences451–451 Mya — about 0.2 occurrences451–451 Mya — about 0.2 occurrences451–451 Mya — about 0.2 occurrences451–450 Mya — about 0.2 occurrences450–450 Mya — about 0.2 occurrences450–450 Mya — about 0.2 occurrences450–449 Mya — about 0.1 occurrences457.8 Mya449.1 Mya

5 occurrences of Holopea obliqua 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

5 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

St. Peter Sandstone — 44.90°N, 93.03°WSt. Peter Sandstone — 43.73°N, 92.13°WSt. Peter Sandstone — 46.00°N, 94.00°WSt. Peter Sandstone — 42.00°N, 90.50°WChaumont — 45.88°N, 76.93°W

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

Holopea obliqua and its relatives

Ordovician

Where Holopea obliqua and its relatives were recorded in the Ordovician.

Found in the same rock

91 taxa

The Paleobiology Database records 5 sites for Holopea obliqua, 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 5 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 content1

Picture of Holopea obliqua

Source
iDigBio
Credit
via iDigBio
Licence
CC0
Commercial use
the licence allows it

No 3D scan of Holopea obliqua was found in Smithsonian Open Access and Sketchfab.

MorphoSource 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 itHolopea through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Hall 1847