Isopoda: Temporal Range: Latest Carboniferous To Present
Isopoda: Temporal Range: Latest Carboniferous To Present
Isopoda: Temporal Range: Latest Carboniferous To Present
Suborders
Contents
Asellota
Description
Calabozoida
Diversity and classification
Cymothoida
Evolutionary history
Limnoriidea
Locomotion
Feeding and nutrition Microcerberidea
The seven free segments of the thorax each bear a pair of unbranched pereopods (limbs). In most species
these are used for locomotion and are of much the same size, morphology and orientation, giving the order
its name "Isopoda", from the Greek equal foot. In a few species, the front pair are modified into gnathopods
with clawed, gripping terminal segments. The pereopods are not used in respiration, as are the equivalent
limbs in amphipods, but the coxae (first segments) are fused to the tergites (dorsal plates) to form epimera
(side plates). In mature females, some or all of the limbs have appendages known as oostegites which fold
underneath the thorax and form a brood chamber for the eggs. In males, the gonopores (genital openings)
are on the ventral surface of segment eight and in the females, they are in a similar position on segment
six.[9]
One or more of the abdominal segments, starting with the sixth segment, is fused to the telson (terminal
section) to form a rigid pleotelson.[9][10][11] The first five abdominal segments each bear a pair of biramous
(branching in two) pleopods (lamellar structures which serve the function of gas exchange, and in aquatic
species serve as gills and propulsion),[3][12] and the last segment bears a pair of biramous uropods
(posterior limbs). In males, the second pair of pleopods, and sometimes also the first, are modified for use in
transferring sperm. The endopods (inner branches of the pleopods) are modified into structures with thin,
permeable cuticles (flexible outer coverings) which act as gills for gas exchange.[9] In some terrestrial
isopods, these resemble lungs.[3]
Evolutionary history
Isopods first appeared in the fossil record during the Carboniferous period of the Paleozoic some 300
million years ago.[23] They were primitive, short-tailed members of the suborder Phreatoicidea. At that
time, Phreatoicideans were marine organisms with a cosmopolitan distribution. Nowadays, the members of
this formerly widespread suborder form relic populations in freshwater environments in South Africa, India
and Oceania, the greatest number of species being in Tasmania. Other primitive, short-tailed suborders
include Asellota, Microcerberidea, Calabozoidea and the terrestrial Oniscidea.[14]
The short-tailed isopods have a short pleotelson and terminal, stylus-like uropods and have a sedentary
lifestyle on or under the sediment on the seabed. The long-tailed isopods have a long pleotelson and broad
lateral uropods which can be used in swimming. They are much more active and can launch themselves off
the seabed and swim for short distances. The more advanced long-tailed isopods are mostly endemic to the
southern hemisphere and may have radiated on the ancient supercontinent of Gondwana soon after it broke
away from Laurasia 200 million years ago. The short-tailed forms may have been driven from the shallow
seas in which they lived by increased predatory pressure from marine fish, their main predators. The
development of the long-tailed forms may also have provided competition that helped force the short-tailed
forms into refugia. The latter are now restricted to environments such as the deep sea, freshwater,
groundwater and dry land. Isopods in the suborder Asellota are by far the most species-rich group of deep
sea isopods.[14]
Locomotion
Unlike the amphipods, marine and freshwater isopods are entirely benthic. This gives them little chance to
disperse to new regions and may explain why so many species are endemic to restricted ranges. Crawling is
the primary means of locomotion, and some species bore into the seabed, the ground or timber structures.
Some members of the Flabellifera can swim to a limited extent and have their front three pairs of pleopods
modified for this purpose, with their respiratory structures limited to the hind pleopods. Most terrestrial
species are slow-moving and conceal themselves under objects or hide in crevices or under bark. The semi-
terrestrial sea slaters (Ligia spp.) can run rapidly on land and many terrestrial species can roll themselves
into a ball when threatened, a feature that has evolved independently in different groups and also in the
marine sphaeromatids.[9]
Parasitic species are mostly external parasites of fish or crustaceans and feed on blood. The larvae of the
Gnathiidae family and adult cymothoidids have piercing and sucking mouthparts and clawed limbs adapted
for clinging onto their hosts. In general, isopod parasites have diverse lifestyles and include Cancricepon
elegans, found in the gill chambers of crabs; Athelges tenuicaudis, attached to the abdomen of hermit crabs;
Crinoniscus equitans living inside the barnacle Balanus perforatus; cyproniscids, living inside ostracods
and free-living isopods; bopyrids, living in the gill chambers or on the carapace of shrimps and crabs and
causing a characteristic bulge which is even recognisable in some fossil crustaceans; and entoniscidae living
inside some species of crab and shrimp.[9][26] Cymothoa exigua is a parasite of the spotted rose snapper
Lutjanus guttatus in the Gulf of California; it causes the tongue of the fish to atrophy and takes its place in
what is believed to be the first instance discovered of a parasite functionally replacing a host structure in
animals.[27]
The eggs, which may number up to several hundred, are brooded by the female in the marsupium, a
chamber formed by flat plates known as oostegites under the thorax. This is filled with water even in
terrestrial species.[9] The eggs hatch as mancae, a post-larval stage which resembles the adult except for the
absence of the last pair of pereopods. The lack of a swimming phase in the life cycle is a limiting factor in
isopod dispersal, and may be responsible for the high levels of endemism in the order.[14] As adults,
isopods differ from other crustaceans in that moulting occurs in two stages known as "biphasic
moulting".[3] First they shed the exoskeleton from the posterior part of their body and later shed the anterior
part. The giant Antarctic isopod Glyptonotus antarcticus is an exception, and moults in a single process.[28]
Terrestrial isopods
The majority of crustaceans are aquatic and the isopods are one of the few groups of which some members
now live on land.[29][30] The only other crustaceans which include a small number of terrestrial species are
amphipods (like sandhoppers) and decapods (crabs, shrimp, etc.).[29] Terrestrial isopods play an important
role in many tropical and temperate ecosystems by aiding in the decomposition of plant material through
mechanical and chemical means, and by enhancing the activity of microbes.[31] Macro-detritivores,
including terrestrial isopods, are absent from arctic and sub-arctic
regions, but have the potential to expand their range with increased
temperatures in high latitudes.[32]
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External links
Media related to Isopoda at Wikimedia Commons
Data related to Isopoda at Wikispecies
World List of Marine Freshwater and Terrestrial Isopod Crustaceans (http://www.marinespeci
es.org/isopoda/)