Palaeastacus sussexiensis

Palaeastacus sussexiensis

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
PalaeastacusPBDB
Diet
carnivorePBDB, for Decapoda
Life habit
infaunalPBDB, for Erymidae
Motility
actively mobilePBDB, for Malacostraca
Vision
well-developedPBDB, for Malacostraca

Time the record covers

At least 69 million years on record.

The record covers at least 125.77 Mya to 56 Mya. No occurrence read is dated outside 137.05 Mya to 48.07 Mya.

Early Cretaceous — about 4 of 9 occurrencesEarly CretaceousLate Cretaceous — about 4 of 9 occurrencesLate CretaceousPaleocene — about 0 of 9 occurrencesEocene — about 1 of 9 occurrencesEocene139–136 Mya — about 0.1 occurrences136–133 Mya — about 0.3 occurrences133–130 Mya — about 0.3 occurrences130–126 Mya — about 0.3 occurrences126–123 Mya — about 0.1 occurrences123–120 Mya — about 0.6 occurrences120–117 Mya — about 1 occurrence117–114 Mya — about 1.0 occurrences114–111 Mya — about 0.3 occurrences102–99 Mya — about 0.9 occurrences99–96 Mya — about 1 occurrence96–93 Mya — about 0.9 occurrences93–89 Mya — about 0.1 occurrences89–86 Mya — about 0.1 occurrences86–83 Mya — about 0.1 occurrences83–80 Mya — about 0.1 occurrences80–77 Mya — about 0.1 occurrences77–74 Mya — about 0.1 occurrences74–71 Mya — about 0.1 occurrences71–68 Mya — about 0.1 occurrences68–65 Mya — about 0.1 occurrences59–56 Mya — about 0.1 occurrences56–52 Mya — about 0.4 occurrences52–49 Mya — about 0.4 occurrences49–46 Mya — about 0.2 occurrences125.77 Mya56 Mya139 Mya46 Mya

9 occurrences of Palaeastacus sussexiensis on record, most of them in the Early Cretaceous. 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

6 formations

Lower Chalk — 52.18°N, 0.17°ERio Mayer — 48.92°S, 71.50°WLondon Clay — 51.42°N, 0.90°EBenassal — 40.27°N, 0.24°ESpartan Glacier — 71.99°S, 60.27°WAtherfield Clay — 50.60°N, 1.32°W

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The named rock units Palaeastacus sussexiensis 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.

Palaeastacus sussexiensis and its relatives

Early Cretaceous

Where Palaeastacus sussexiensis and its relatives were recorded in the Early Cretaceous.

Found in the same rock

52 taxa

The Paleobiology Database records 9 sites for Palaeastacus sussexiensis, 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

8 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. 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 Palaeastacus sussexiensis

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

No 3D scan of Palaeastacus sussexiensis 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.

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. (Mantell 1824)