Isopoda
Isopoda is an order of crustaceans. Members of this group are collectively called isopods and include both aquatic species such as gribbles and terrestrial species such as woodlice. All have rigid, segmented exoskeletons, two pairs of antennae, seven pairs of jointed limbs on the thorax, and five pairs of branching appendages on the abdomen that are used in respiration. Females brood their young in a pouch under their thorax called the marsupium.

Hans Hillewaert · CC BY-SA 4.0 · 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- Also called
- isopodPBDB
- Sits inside
- MancoidaPBDB
- Diet
- omnivorePBDB, for Malacostraca
- Life habit
- epifaunalPBDB, for Malacostraca
- Motility
- actively mobilePBDB, for Malacostraca
- Vision
- well-developedPBDB, for Malacostraca
Time the record covers
At least 307 million years on record.
The record covers at least 307.4 Mya to 129 ka. No occurrence read is dated outside 309.8 Mya to 0 Mya.
163 occurrences of Isopoda on record, most of them in the Early Cretaceous. 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
163 occurrences- Carboniferous2%
- Permian4%
- Middle Triassic3%
- Late Triassic1%
- Middle Jurassic12%
- Late Jurassic4%
- Early Cretaceous21%
- Late Cretaceous14%
- Paleoceneunder 1%
- Eocene10%
- Oligocene8%
- Miocene13%
- Pliocene2%
- Pleistocene6%
- Holoceneunder 1%
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
58 formations
- Sierra Madre Formation6
- Opalinus Clay Formation6
- Escucha Formation6
- Opalinuston Formation5
- Makah Formation5
- Le Mans Formation5
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The named rock units Isopoda has been recovered from, largest first. Drawn where the rock is now, not where it formed. 34 further formations hold fewer occurrences each and are not listed. 56 occurrences have no formation on record, which is common for older literature.
Isopoda and its relatives
Early CretaceousWhere Isopoda and its relatives were recorded in the Early Cretaceous.
Found in the same rock
2,293 taxa- Palaega jurassica13 sites
- Palaega goedertorum11 sites
- Cirolanidae8 sites
- Ostracoda5 sites
- Araneae4 sites
- Bivalvia4 sites
- Bositra buchi4 sites
- Coleoptera4 sites
- Palaeocrangon problematicus4 sites
- Planolites4 sites
- Jurapseudes friedericianus3 sites
- Lenticulina dorbignyi dorbignyi3 sites
- Macroacaena alseanus3 sites
- Oniscidea3 sites
- Reinholdella3 sites
- Reophax3 sites
- Ablator triguttatus2 sites
- Adorator hispidus2 sites
- Allacrotelsa dubia2 sites
- Ammobaculites subcretaceus2 sites
- Antrimpos atavus2 sites
- Anyphaena fuscata2 sites
- Archaea paradoxa2 sites
- Archaeoniscus aranguthyorum2 sites
The Paleobiology Database records 119 sites for Isopoda, 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
86 references- Palaega goedertorum, a fossil isopod (Crustacea) from Late Eocene to Early Miocene rocks of Washington state11
- Isopoden und Tanaidaceen (Crustacea, Malacostraca) aus dem unteren Opalinuston der Nordschweiz7
- Terrestrial isopods from Spanish amber (Crustacea: Oniscidea): insights into the Cretaceous soil biota6
- Diversity of the Crinocheta (Crustacea, Isopoda, Oniscidea) from Early Miocene Chiapas amber, Mexico6
- New report of decapod and isopod crustaceans from the Lower-Middle Pleistocene of Montalbano Jonico, Matera (Basilicata, southern Italy)5
- Isopod crustacean fossils from the Cenomanian stratotype: five new species in suborders Cymothoida, Asellota and Valvifera5
- New species of fossil Cirolanidae (Isopoda, Cymothoida) from the Lower Cretaceous (Aptian) Sierra Madre Formation plattenkalk dolomites of El Espinal quarries, Chiapas, SE Mexico4
- Lower Cretaceous marine isopods (Isopoda: Cirolanidae, Sphaeromatidae) from the San Juan Raya and Tlayúa formations, Puebla, Mexico4
- Mesozoic and Cenozoic fossil isopods of North America4
- Paläontologische Untersuchungen im unteren Opalinuston der Nordschweiz4
- Two new species of the terrestrial isopod genus Pseudarmadillo from Dominican amber (Amber-Collection Stuttgart: Crustacea, Isopoda, Pseudarmadillidae)4
- Triassic Isopoda - three new species from Central Europe shed light on the early diversity of the group3
Each of the 163 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. 74 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 Isopoda
- Source
- Wikipedia/Commons
- Credit
- Hans Hillewaert
- Licence
- CC BY-SA 4.0
- Commercial use
- the licence allows it

CT scan
- Source
- MorphoSource
- Credit
- MCZ Invertebrate Zoology
- Licence
- In Copyright
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Isopoda indet. · mcz:iz:90105
3D model
- Source
- Sketchfab
- Licence
- CC Attribution-NonCommercial-ShareAlike
- Commercial use
- the licence does not allow it
The description on this site
- Source
- Wikipedia, “Isopoda”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itMancoida through timeFormations of the Early CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Latreille 1817