Anisocardia islipensis

Anisocardia islipensis

via iDigBio · CC BY-NC-ND · 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
AnisocardiaPBDB
Diet
suspension feederPBDB, for Venerida
Life habit
infaunalPBDB, for Venerida
Motility
facultatively mobilePBDB, for Venerida
Vision
blindPBDB, for Bivalvia

Time the record covers

At most 2.9 million years on record.

Every occurrence read is dated to somewhere between 168.2 Mya and 165.3 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Middle Jurassic — about 9 of 9 occurrencesMiddle Jurassic168–168 Mya — about 0.1 occurrences168–168 Mya — about 0.4 occurrences168–168 Mya — about 0.4 occurrences168–168 Mya — about 0.4 occurrences168–168 Mya — about 0.4 occurrences168–168 Mya — about 0.4 occurrences168–167 Mya — about 0.4 occurrences167–167 Mya — about 0.4 occurrences167–167 Mya — about 0.4 occurrences167–167 Mya — about 0.4 occurrences167–167 Mya — about 0.4 occurrences167–167 Mya — about 0.4 occurrences167–167 Mya — about 0.4 occurrences167–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–166 Mya — about 0.4 occurrences166–165 Mya — about 0.4 occurrences165–165 Mya — about 0.4 occurrences165–165 Mya — about 0.1 occurrences168.7 Mya164.8 Mya

9 occurrences of Anisocardia islipensis on record, most of them in the Middle Jurassic. 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

9 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

Calcaires 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 — 49.60°N, 4.96°ECalcaires marneux inferieurs — 49.72°N, 4.50°ECalcaires marneux inferieurs — 49.64°N, 4.73°EWhite Limestone — 51.75°N, 1.17°WWhite Limestone — 51.00°N, 1.00°W

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

Anisocardia islipensis and its relatives

Middle Jurassic

Where Anisocardia islipensis and its relatives were recorded in the Middle Jurassic.

Found in the same rock

94 taxa

The Paleobiology Database records 9 sites for Anisocardia islipensis, 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

3 references

Each of the 9 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 content1

Picture of Anisocardia islipensis

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

No 3D scan of Anisocardia islipensis 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

What may have been alongside itAnisocardia through timeFormations of the Middle JurassicThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Lycett 1863