Davalliaceae

Davallia is a genus of about 40 species of fern. In the Pteridophyte Phylogeny Group classification of 2016, it is the only genus in the family Davalliaceae, which is placed in the suborder Polypodiineae, order Polypodiales. Alternatively, the family may be placed in a very broadly defined family Polypodiaceae sensu lato as the subfamily Davallioideae.

Davalliaceae

No machine-readable author provided. MPF assumed (based on copyright claims). · CC BY 2.5 · via Wikipedia/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
PolypodiineaePBDB
Diet
"photoautotroph"PBDB, for Streptophyta

Time the record covers

At least 174 million years on record.

The record covers at least 174.7 Mya to 11.7 ka. No occurrence read is dated outside 184.2 Mya to 0 Mya.

Early Jurassic — about 1 of 34 occurrencesMiddle Jurassic — about 0 of 34 occurrencesLate Jurassic — about 1 of 34 occurrencesLate JurassicEarly Cretaceous — about 0 of 34 occurrencesLate Cretaceous — about 0 of 34 occurrencesPaleocene — about 0 of 34 occurrencesEocene — about 0 of 34 occurrencesOligocene — about 0 of 34 occurrencesMiocene — about 2 of 34 occurrencesMiocenePliocene — about 0 of 34 occurrencesPleistocene — about 28 of 34 occurrences188–182 Mya — about 0.3 occurrences182–175 Mya — about 0.7 occurrences175–169 Mya — about 0.1 occurrences157–150 Mya — about 0.4 occurrences150–144 Mya — about 0.5 occurrences144–138 Mya — about 0.1 occurrences25–19 Mya — about 1 occurrence13–6.3 Mya — about 0.9 occurrences6.3–0 Mya — about 30 occurrences174.7 Mya11.7 ka188 Mya0 Mya

34 occurrences of Davalliaceae on record, most of them in the Pleistocene. The Paleobiology Database records this as a living group. 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

34 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

Bangmai — 23.90°N, 100.02°EFoulden Hills Diatomite — 45.53°S, 170.22°E

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The named rock units Davalliaceae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 32 occurrences have no formation on record, which is common for older literature.

Davalliaceae and its relatives

Pleistocene

Where Davalliaceae and its relatives were recorded in the Pleistocene.

Found in the same rock

465 taxa

The Paleobiology Database records 34 sites for Davalliaceae, 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

7 references

Each of the 34 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 Davalliaceae

Credit
No machine-readable author provided. MPF assumed (based on copyright claims).
Licence
CC BY 2.5
Commercial use
the licence allows it

No 3D scan of Davalliaceae 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Schomb 1848