Gryphaeostrea callophyla

Gryphaeostrea callophyla

Maricelsevi96 · CC BY-SA 4.0 · via Wikidata/Commons. 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
GryphaeostreaPBDB
Diet
suspension feederPBDB, for Gryphaeidae
Life habit
epifaunalPBDB, for Gryphaeidae
Motility
stationary, attachedPBDB, for Gryphaeidae
Vision
blindPBDB, for Bivalvia
Environment
marine,brackishPBDB, for Ostreida

Time the record covers

At most 11 million years on record.

Every occurrence read is dated to somewhere between 72.2 Mya and 61.66 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Late Cretaceous — about 1 of 3 occurrencesLate CretaceousPaleocene — about 2 of 3 occurrencesPaleocene72–72 Mya — about 0.0 occurrences72–72 Mya — about 0.1 occurrences72–71 Mya — about 0.1 occurrences71–71 Mya — about 0.1 occurrences71–70 Mya — about 0.1 occurrences70–70 Mya — about 0.1 occurrences70–70 Mya — about 0.1 occurrences70–69 Mya — about 0.1 occurrences69–69 Mya — about 0.1 occurrences69–68 Mya — about 0.1 occurrences68–68 Mya — about 0.1 occurrences68–68 Mya — about 0.1 occurrences68–67 Mya — about 0.1 occurrences67–67 Mya — about 0.1 occurrences67–67 Mya — about 0.1 occurrences67–66 Mya — about 0.1 occurrences66–66 Mya — about 0.1 occurrences66–65 Mya — about 0.2 occurrences65–65 Mya — about 0.2 occurrences65–65 Mya — about 0.2 occurrences65–64 Mya — about 0.2 occurrences64–64 Mya — about 0.2 occurrences64–63 Mya — about 0.2 occurrences63–63 Mya — about 0.2 occurrences63–63 Mya — about 0.2 occurrences63–62 Mya — about 0.2 occurrences62–62 Mya — about 0.2 occurrences62–62 Mya — about 0.1 occurrences72.7 Mya61.2 Mya

3 occurrences of Gryphaeostrea callophyla on record, most of them in the Paleocene. 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

3 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

1 formation

  • Roca Formation · Malargüe GroupLa Pampa, Neuquén, Río Negro · AR · 72.2–61.66 Mya3
Roca — 37.67°S, 67.50°WRoca — 37.55°S, 69.70°WRoca — 39.00°S, 67.56°W

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

Gryphaeostrea callophyla and its relatives

Paleocene

Where Gryphaeostrea callophyla and its relatives were recorded in the Paleocene.

Found in the same rock

62 taxa

The Paleobiology Database records 3 sites for Gryphaeostrea callophyla, 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 3 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 Gryphaeostrea callophyla

Credit
Maricelsevi96
Licence
CC BY-SA 4.0
Commercial use
the licence allows it

No 3D scan of Gryphaeostrea callophyla 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. (Ihering 1903)