Cornus glandulosa

No picture of Cornus glandulosa was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cornus glandulosa, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
CornusPBDB
Diet
"photoautotroph"PBDB, for Angiospermae

Time the record covers

At least 3.3 million years on record.

The record covers at least 41.03 Mya to 37.71 Mya. No occurrence read is dated outside 48.07 Mya to 33.9 Mya.

Eocene — about 3 of 3 occurrencesEoceneOligocene — about 0 of 3 occurrences49–48 Mya — about 0.0 occurrences48–48 Mya — about 0.1 occurrences48–47 Mya — about 0.1 occurrences47–47 Mya — about 0.1 occurrences47–46 Mya — about 0.1 occurrences46–46 Mya — about 0.1 occurrences46–45 Mya — about 0.1 occurrences45–45 Mya — about 0.1 occurrences45–44 Mya — about 0.1 occurrences44–44 Mya — about 0.1 occurrences44–43 Mya — about 0.1 occurrences43–43 Mya — about 0.1 occurrences43–42 Mya — about 0.1 occurrences42–41 Mya — about 0.1 occurrences41–41 Mya — about 0.1 occurrences41–40 Mya — about 0.2 occurrences40–40 Mya — about 0.2 occurrences40–39 Mya — about 0.2 occurrences39–39 Mya — about 0.2 occurrences39–38 Mya — about 0.2 occurrences38–38 Mya — about 0.2 occurrences38–37 Mya — about 0.1 occurrences37–37 Mya — about 0.1 occurrences37–36 Mya — about 0.1 occurrences36–36 Mya — about 0.1 occurrences36–35 Mya — about 0.1 occurrences35–35 Mya — about 0.1 occurrences35–34 Mya — about 0.1 occurrences34–34 Mya — about 0.1 occurrences34–33 Mya — about 0.0 occurrences41.03 Mya37.71 Mya48.6 Mya33.4 Mya

3 occurrences of Cornus glandulosa on record, most of them in the Eocene. 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

Headon Beds — 50.75°N, 1.60°W

Loading coastlines…

The named rock units Cornus glandulosa has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.

Cornus glandulosa and its relatives

Eocene

Where Cornus glandulosa and its relatives were recorded in the Eocene.

Found in the same rock

156 taxa

The Paleobiology Database records 3 sites for Cornus glandulosa, 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

2 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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Cornus glandulosa was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cornus glandulosa, or no answer at all. This entry cannot say which.

No 3D scan of Cornus glandulosa was found in Smithsonian Open Access and Sketchfab.

MorphoSource was 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 itCornus through timeFormations of the EoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Chandler 1926)