Fimbria

Fimbria is a genus of marine bivalve molluscs in the family Lucinidae. Fimbria contains two living species, Fimbria fimbriata and Fimbria soverbii. Several other species are known from fossils.

Fimbria

George Brettingham Sowerby II · Public Domain · 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
FimbriinaePBDB
Diet
chemosymbioticPBDB, for Lucinidae
Life habit
deep infaunalPBDB, for Lucinidae
Motility
facultatively mobilePBDB, for Lucinidae
Vision
blindPBDB, for Bivalvia

Time the record covers

At least 233 million years on record.

The record covers at least 233.6 Mya to 129 ka. No occurrence read is dated outside 237 Mya to 11.7 ka.

Middle Triassic — about 0 of 245 occurrencesLate Triassic — about 25 of 245 occurrencesLate TriassicEarly Jurassic — about 2 of 245 occurrencesEarly JurassicMiddle Jurassic — about 85 of 245 occurrencesLate Jurassic — about 18 of 245 occurrencesEarly Cretaceous — about 19 of 245 occurrencesEarly CretaceousLate Cretaceous — about 28 of 245 occurrencesLate CretaceousPaleocene — about 24 of 245 occurrencesEocene — about 37 of 245 occurrencesEoceneOligocene — about 1 of 245 occurrencesMiocene — about 3 of 245 occurrencesPliocene — about 0 of 245 occurrencesPleistocene — about 3 of 245 occurrences242–234 Mya — about 11 occurrences234–226 Mya — about 13 occurrences226–218 Mya — about 0.5 occurrences218–210 Mya — about 0.5 occurrences210–201 Mya — about 0.5 occurrences201–193 Mya — about 0.9 occurrences193–185 Mya — about 0.8 occurrences185–177 Mya — about 0.2 occurrences177–169 Mya — about 4 occurrences169–161 Mya — about 82 occurrences161–153 Mya — about 10 occurrences153–145 Mya — about 7 occurrences145–137 Mya — about 0.1 occurrences137–129 Mya — about 7 occurrences129–121 Mya — about 2 occurrences121–113 Mya — about 6 occurrences113–105 Mya — about 3 occurrences105–97 Mya — about 3 occurrences97–89 Mya — about 3 occurrences89–81 Mya — about 2 occurrences81–73 Mya — about 1 occurrence73–64 Mya — about 25 occurrences64–56 Mya — about 18 occurrences56–48 Mya — about 6 occurrences48–40 Mya — about 7 occurrences40–32 Mya — about 25 occurrences32–24 Mya — about 0.7 occurrences24–16 Mya — about 2 occurrences16–8.1 Mya — about 1 occurrence8.1–0 Mya — about 3 occurrences233.6 Mya129 ka242 Mya0 Mya

245 occurrences of Fimbria on record, most of them in the Middle Jurassic. 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

245 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

60 formations

Dhruma — 22.62°N, 46.00°EDhruma — 22.53°N, 46.17°EDhruma — 23.97°N, 46.17°EDhruma — 21.88°N, 45.67°EDhruma — 25.53°N, 45.00°EDhruma — 26.92°N, 44.00°EDhruma — 25.05°N, 45.67°EDhruma — 25.37°N, 45.50°EDhruma — 25.70°N, 45.67°EDhruma — 25.78°N, 45.25°EDhruma — 25.97°N, 45.00°EDhruma — 26.20°N, 44.83°EDhruma — 26.33°N, 44.83°ETataouine — 33.00°N, 10.47°ECalcaires pseudo-oolithiques superieurs — 49.83°N, 4.20°ECalcaires pseudo-oolithiques superieurs — 49.88°N, 4.09°ECalcaires pseudo-oolithiques superieurs — 49.63°N, 4.92°ECalcaires pseudo-oolithiques superieurs — 49.88°N, 4.04°ECalcaires pseudo-oolithiques superieurs — 49.68°N, 4.61°ECalcaires pseudo-oolithiques superieurs — 49.60°N, 4.96°ECalcaires pseudo-oolithiques superieurs — 49.64°N, 4.73°ECalcaires pseudo-oolithiques inferieurs — 49.85°N, 4.31°ECalcaires pseudo-oolithiques inferieurs — 49.88°N, 4.23°ECalcaires pseudo-oolithiques inferieurs — 49.68°N, 4.61°ECalcaires pseudo-oolithiques inferieurs — 49.76°N, 4.45°ECalcaires pseudo-oolithiques inferieurs — 49.86°N, 4.14°ECalcaires pseudo-oolithiques inferieurs — 49.60°N, 4.96°ECalcaires pseudo-oolithiques inferieurs — 49.72°N, 4.50°ECalcaires marno-crayeux inferieurs — 49.83°N, 4.20°ECalcaires marno-crayeux inferieurs — 49.88°N, 4.09°ECalcaires marno-crayeux inferieurs — 49.88°N, 4.04°ECalcaires marno-crayeux inferieurs — 49.85°N, 4.16°ECalcaires marno-crayeux inferieurs — 49.78°N, 4.40°ECalcaires marno-crayeux inferieurs — 49.65°N, 4.64°ECalcaires marno-crayeux inferieurs — 49.60°N, 4.80°ECalcaires marno-crayeux superieurs — 49.83°N, 4.20°ECalcaires marno-crayeux superieurs — 49.88°N, 4.09°ECalcaires marno-crayeux superieurs — 49.85°N, 4.16°ECalcaires marno-crayeux superieurs — 49.78°N, 4.40°ECalcaires marno-crayeux superieurs — 49.65°N, 4.64°ECalcaires marno-crayeux superieurs — 49.60°N, 4.80°ECalcaires marneux inferieurs — 49.83°N, 4.20°ECalcaires marneux inferieurs — 49.88°N, 4.09°ECalcaires marneux inferieurs — 49.63°N, 4.92°ECalcaires marneux inferieurs — 49.70°N, 4.42°ECalcaires marneux inferieurs — 49.60°N, 4.96°ECalcaires marneux inferieurs — 49.72°N, 4.50°ECalcaires marneux inferieurs — 49.64°N, 4.73°EInglis Limestone — 29.23°N, 82.70°WInglis Limestone — 29.02°N, 82.62°WInglis Limestone — 29.03°N, 82.67°WGosport Sand — 31.50°N, 87.80°WGosport Sand — 31.54°N, 87.52°WGosport Sand — 31.55°N, 87.91°WCassian — 46.55°N, 11.93°ECassian — 46.57°N, 11.94°ERaibl — 47.41°N, 11.12°ERaibl — 47.71°N, 12.68°ERaibl — 47.64°N, 11.80°EPoudingue de Ciply — 50.42°N, 3.95°ECalcaire de Eisden — 50.98°N, 5.70°EJuncal — 34.55°N, 118.73°WJuncal — 34.51°N, 119.58°WRaibl — 47.43°N, 11.19°ERaibl — 47.36°N, 11.48°ERaibl — 47.33°N, 11.46°ERaibl — 47.35°N, 11.32°EEwekoro — 6.92°N, 3.19°ERukesa Shales — 4.05°N, 41.02°ERukesa Shales — 3.98°N, 41.08°EGatuncillo — 9.20°N, 79.55°WGatuncillo — 9.18°N, 79.52°WGrès verts helvétiques — 45.99°N, 6.69°EGrès verts helvétiques — 45.99°N, 6.58°EGrès verts helvétiques — 46.03°N, 6.47°ESanta Susana — 34.24°N, 118.74°WSanta Susana — 34.25°N, 118.71°WCalcaire de Mons — 50.45°N, 3.93°ETroy Limestone — 18.07°N, 76.75°WTroy Limestone — 18.32°N, 77.13°WPromina — 43.95°N, 16.07°EPromina — 43.93°N, 16.10°ECabrillo — 32.68°N, 117.24°WCabrillo — 32.81°N, 117.27°W

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The named rock units Fimbria has been recovered from, largest first. Drawn where the rock is now, not where it formed. 36 further formations hold fewer occurrences each and are not listed. 76 occurrences have no formation on record, which is common for older literature.

Fimbria and its relatives

Middle Jurassic

Where Fimbria and its relatives were recorded in the Middle Jurassic.

Found in the same rock

3,726 taxa

The Paleobiology Database records 194 sites for Fimbria, and this reads all of them. Of that, one read hit the database's own return limit, so every count below is a floor rather than a total. 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

72 references

Each of the 245 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. 60 further references are not listed. 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 content3

Picture of Fimbria

Credit
George Brettingham Sowerby II
Licence
Public Domain
Commercial use
the licence allows it

CT scan

Licence
In Copyright
Commercial use
cannot be read from the licence given — check the record
Specimen
Anoplopoma fimbria · OS:Fishes:14231

3D model

Source
Sketchfab
Licence
CC Attribution
Commercial use
cannot be read from the licence given — check the record

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. Mühlfeldt 1811