Rhynchocamara

Rhynchocamara

Eksp. 1956 · CC BY-NC 4.0 · via GBIF. 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
CamerellinaePBDB
Diet
suspension feederPBDB, for Pentamerida
Life habit
epifaunalPBDB, for Pentamerida
Motility
stationaryPBDB, for Pentamerida
Vision
blindPBDB, for Rhynchonellata
Environment
marinePBDB, for Lophophorata

Time the record covers

At least 6.2 million years on record.

The record covers at least 475.3 Mya to 469.1 Mya. No occurrence read is dated outside 481.7 Mya to 464.3 Mya.

Ordovician — about 5 of 5 occurrencesOrdovician482–482 Mya — about 0.0 occurrences482–481 Mya — about 0.2 occurrences481–480 Mya — about 0.2 occurrences480–480 Mya — about 0.2 occurrences480–479 Mya — about 0.2 occurrences479–479 Mya — about 0.2 occurrences479–478 Mya — about 0.2 occurrences478–477 Mya — about 0.2 occurrences477–477 Mya — about 0.2 occurrences477–476 Mya — about 0.2 occurrences476–475 Mya — about 0.2 occurrences475–475 Mya — about 0.1 occurrences475–474 Mya — about 0.1 occurrences474–474 Mya — about 0.1 occurrences474–473 Mya — about 0.1 occurrences473–472 Mya — about 0.1 occurrences472–472 Mya — about 0.2 occurrences472–471 Mya — about 0.2 occurrences471–471 Mya — about 0.1 occurrences471–470 Mya — about 0.1 occurrences470–469 Mya — about 0.1 occurrences469–469 Mya — about 0.2 occurrences469–468 Mya — about 0.2 occurrences468–467 Mya — about 0.2 occurrences467–467 Mya — about 0.2 occurrences467–466 Mya — about 0.2 occurrences466–466 Mya — about 0.2 occurrences466–465 Mya — about 0.1 occurrences465–464 Mya — about 0.1 occurrences464–464 Mya — about 0.0 occurrences475.3 Mya469.1 Mya482.2 Mya463.8 Mya

5 occurrences of Rhynchocamara 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

4 formations

Ninemile — 39.00°N, 116.00°WObukhovo — 60.00°N, 32.57°ELynna — 59.97°N, 32.57°EGarden City — 39.08°N, 116.25°W

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

Rhynchocamara and its relatives

Ordovician

Where Rhynchocamara and its relatives were recorded in the Ordovician.

Found in the same rock

28 taxa

The Paleobiology Database records 4 sites for Rhynchocamara, 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

4 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 Rhynchocamara

Source
GBIF
Credit
Eksp. 1956
Licence
CC BY-NC 4.0
Commercial use
the licence does not allow it

No 3D scan of Rhynchocamara 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 itCamerellinae through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Schuchert and Cooper 1931