Diaphus mollis

Diaphus mollis, the soft lanternfish, is a species of lanternfish found in the Atlantic and Indian Oceans.

No picture of Diaphus mollis 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 Diaphus mollis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
DiaphusPBDB
Diet
carnivorePBDB, for Myctophiformes
Life habit
nektonicPBDB, for Myctophiformes
Motility
actively mobilePBDB, for Myctophiformes

Time the record covers

At most 1.1 million years on record.

Every occurrence read is dated to somewhere between 3.6 Mya and 2.58 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Pliocene — about 3 of 3 occurrencesPliocenePleistocene — about 0 of 3 occurrences3.6–3.6 Mya — about 0.1 occurrences3.6–3.5 Mya — about 0.2 occurrences3.5–3.4 Mya — about 0.2 occurrences3.4–3.4 Mya — about 0.2 occurrences3.4–3.3 Mya — about 0.2 occurrences3.3–3.2 Mya — about 0.2 occurrences3.2–3.2 Mya — about 0.2 occurrences3.2–3.1 Mya — about 0.2 occurrences3.1–3.0 Mya — about 0.2 occurrences3.0–3.0 Mya — about 0.2 occurrences3.0–2.9 Mya — about 0.2 occurrences2.9–2.8 Mya — about 0.2 occurrences2.8–2.8 Mya — about 0.2 occurrences2.8–2.7 Mya — about 0.2 occurrences2.7–2.6 Mya — about 0.2 occurrences2.6–2.6 Mya — about 0.1 occurrences4.1 Mya2.08 Mya

3 occurrences of Diaphus mollis on record, most of them in the Pliocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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

2 formations

Shinzato — 26.12°N, 127.74°EShinzato — 26.36°N, 127.98°ENobori — 33.37°N, 134.06°E

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

Diaphus mollis and its relatives

Pliocene

Where Diaphus mollis and its relatives were recorded in the Pliocene.

Found in the same rock

21 taxa

The Paleobiology Database records 3 sites for Diaphus mollis, 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 content0

No picture of Diaphus mollis 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 Diaphus mollis, or no answer at all. This entry cannot say which.

No 3D scan of Diaphus mollis 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.

The description on this site

Licence
CC BY-SA 4.0

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itDiaphus through timeFormations of the PlioceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Tåning 1928