Acila (Truncacila) haidana

Acila (Truncacila) haidana

C. Ahlroth, W. P. Popenoe · CC0 · 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
Acila (Truncacila)PBDB
Diet
deposit feeder, suspension feederPBDB, for Nuculidae
Life habit
infaunalPBDB, for Nuculidae
Motility
facultatively mobilePBDB, for Nuculidae
Vision
blindPBDB, for Bivalvia
Environment
coastal,inner shelf,outer shelf,oceanicPBDB, for Nuculidae

Time the record covers

At most 11 million years on record.

Every occurrence read is dated to somewhere between 100.5 Mya and 89.8 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Early Cretaceous — about 0 of 3 occurrencesLate Cretaceous — about 3 of 3 occurrencesLate Cretaceous101–100 Mya — about 0.0 occurrences100–100 Mya — about 0.1 occurrences100–99 Mya — about 0.1 occurrences99–99 Mya — about 0.1 occurrences99–99 Mya — about 0.1 occurrences99–98 Mya — about 0.1 occurrences98–98 Mya — about 0.1 occurrences98–97 Mya — about 0.1 occurrences97–97 Mya — about 0.1 occurrences97–97 Mya — about 0.1 occurrences97–96 Mya — about 0.1 occurrences96–96 Mya — about 0.1 occurrences96–96 Mya — about 0.1 occurrences96–95 Mya — about 0.1 occurrences95–95 Mya — about 0.1 occurrences95–94 Mya — about 0.1 occurrences94–94 Mya — about 0.1 occurrences94–94 Mya — about 0.2 occurrences94–93 Mya — about 0.2 occurrences93–93 Mya — about 0.2 occurrences93–92 Mya — about 0.2 occurrences92–92 Mya — about 0.2 occurrences92–92 Mya — about 0.2 occurrences92–91 Mya — about 0.2 occurrences91–91 Mya — about 0.2 occurrences91–90 Mya — about 0.2 occurrences90–90 Mya — about 0.2 occurrences90–90 Mya — about 0.1 occurrences101 Mya89.3 Mya

3 occurrences of Acila (Truncacila) haidana on record, most of them in the Late Cretaceous. 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

3 formations

Budden Canyon — 40.40°N, 122.53°WRedding — 40.66°N, 122.11°WAntelope — 39.36°N, 122.32°W

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The named rock units Acila (Truncacila) haidana has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Acila (Truncacila) haidana and its relatives

Late Cretaceous

Where Acila (Truncacila) haidana and its relatives were recorded in the Late Cretaceous.

Found in the same rock

9 taxa

The Paleobiology Database records 3 sites for Acila (Truncacila) haidana, 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 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. Each entry links to the Paleobiology Database's own record for the work.

Media and terms

Media content1

Picture of Acila (Truncacila) haidana

Source
GBIF
Credit
C. Ahlroth, W. P. Popenoe
Licence
CC0
Commercial use
the licence allows it

No 3D scan of Acila (Truncacila) haidana 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 itAcila (Truncacila) through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Packard in Schenck 1936)