Homalopoma wattsi

Homalopoma wattsi

via iDigBio · CC BY-NC-SA · via iDigBio. 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
HomalopomaPBDB
Diet
grazerPBDB, for Turbinidae
Life habit
epifaunalPBDB, for Turbinidae
Motility
actively mobilePBDB, for Turbinidae
Vision
limitedPBDB, for Gastropoda

Time the record covers

At least 22 million years on record.

The record covers at least 56 Mya to 33.9 Mya. No occurrence read is dated outside 59.24 Mya to 27.3 Mya.

Paleocene — about 1 of 13 occurrencesPaleoceneEocene — about 11 of 13 occurrencesEoceneOligocene — about 1 of 13 occurrencesOligocene60–59 Mya — about 0.1 occurrences59–58 Mya — about 0.3 occurrences58–57 Mya — about 0.3 occurrences57–55 Mya — about 0.8 occurrences55–54 Mya — about 1 occurrence54–53 Mya — about 1 occurrence53–52 Mya — about 1 occurrence52–51 Mya — about 1 occurrence51–50 Mya — about 1 occurrence50–49 Mya — about 1 occurrence49–48 Mya — about 0.9 occurrences48–47 Mya — about 0.2 occurrences47–45 Mya — about 0.2 occurrences45–44 Mya — about 0.2 occurrences44–43 Mya — about 0.2 occurrences43–42 Mya — about 0.2 occurrences42–41 Mya — about 0.2 occurrences41–40 Mya — about 0.3 occurrences40–39 Mya — about 0.3 occurrences39–38 Mya — about 0.3 occurrences38–37 Mya — about 0.0 occurrences34–33 Mya — about 0.1 occurrences33–32 Mya — about 0.2 occurrences32–31 Mya — about 0.2 occurrences31–30 Mya — about 0.2 occurrences30–29 Mya — about 0.2 occurrences29–28 Mya — about 0.2 occurrences28–27 Mya — about 0.1 occurrences56 Mya33.9 Mya59.9 Mya26.7 Mya

13 occurrences of Homalopoma wattsi 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

13 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

10 formations

Roseburg — 43.01°N, 123.91°WCapay — 39.20°N, 121.82°WCapay — 38.54°N, 122.05°WSilverado — 33.87°N, 117.71°WJuncal — 34.40°N, 118.48°WLodo — 36.36°N, 120.44°WManiobra — 33.59°N, 115.67°WFlournoy — 43.02°N, 123.93°WTyee — 42.04°N, 123.86°WCowlitz — 46.40°N, 122.93°WLincoln Creek — 46.41°N, 122.93°W

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

Homalopoma wattsi and its relatives

Eocene

Where Homalopoma wattsi and its relatives were recorded in the Eocene.

Found in the same rock

295 taxa

The Paleobiology Database records 12 sites for Homalopoma wattsi, 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

9 references

Each of the 13 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 Homalopoma wattsi

Source
iDigBio
Credit
via iDigBio
Licence
CC BY-NC-SA
Commercial use
the licence does not allow it

No 3D scan of Homalopoma wattsi was found in MorphoSource and Sketchfab.

Smithsonian Open Access 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

Occurrence data from the Paleobiology Database, CC BY 4.0. (Dickerson 1916)