Chione (Chionopsis) traftoni

No picture of Chione (Chionopsis) traftoni 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 Chione (Chionopsis) traftoni, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
ChionopsisPBDB
Diet
suspension feederPBDB, for Chionopsis
Life habit
infaunalPBDB, for Chionopsis
Motility
facultatively mobilePBDB, for Chionopsis
Vision
blindPBDB, for Bivalvia

Time the record covers

At most 1.9 million years on record.

The one occurrence read is dated to somewhere between 2.58 Mya and 774 ka, which is a dating window rather than a span.

Pliocene — about 0 of 1 occurrencePleistocene — about 1 of 1 occurrencePleistocene2.6–2.5 Mya — about 0.0 occurrences2.5–2.4 Mya — about 0.1 occurrences2.4–2.3 Mya — about 0.1 occurrences2.3–2.2 Mya — about 0.1 occurrences2.2–2.1 Mya — about 0.1 occurrences2.1–2.1 Mya — about 0.1 occurrences2.1–2.0 Mya — about 0.1 occurrences2.0–1.9 Mya — about 0.1 occurrences1.9–1.8 Mya — about 0.1 occurrences1.8–1.7 Mya — about 0.1 occurrences1.7–1.6 Mya — about 0.1 occurrences1.6–1.5 Mya — about 0.1 occurrences1.5–1.4 Mya — about 0.1 occurrences1.4–1.3 Mya — about 0.1 occurrences1.3–1.2 Mya — about 0.1 occurrences1.2–1.1 Mya — about 0.1 occurrences1.1–1.0 Mya — about 0.1 occurrences1.0–929 ka Mya — about 0.1 occurrences929 ka–835 ka Mya — about 0.1 occurrences835 ka–742 ka Mya — about 0.0 occurrences3.08 Mya274 ka

1 occurrence of Chione (Chionopsis) traftoni on record, most of them in the Pleistocene. 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

1 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

Armuelles — 8.03°N, 82.92°W

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The named rock units Chione (Chionopsis) traftoni has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Chione (Chionopsis) traftoni and its relatives

Pleistocene

Where Chione (Chionopsis) traftoni and its relatives were recorded in the Pleistocene.

Found in the same rock

107 taxa

The Paleobiology Database records 1 site for Chione (Chionopsis) traftoni, 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

1 reference

Each of the 1 occurrence 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 content0

No picture of Chione (Chionopsis) traftoni 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 Chione (Chionopsis) traftoni, or no answer at all. This entry cannot say which.

No 3D scan of Chione (Chionopsis) traftoni 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 itChionopsis through timeFormations of the PleistoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Pilsbry and Olsson 1941