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Class MalacostracaThe Malacostraca include about two thirds of all crustacean species, and contains all the larger forms, such as woodlice, shrimps, lobsters and crabs .Their body comprises: head (6 segments) with a pair of antennules (A1) and antennae (A2) and mouthparts, thorax (8 segments and abdomen (6 segments). All thoracic segments and most abdominal segments have a pair of appendages, which are primitively biramous. Gills occur on or close to the bases of the thoracic appendages. The three main orders of malacostracans are the ISOPODA (which includes Asellus the water louse) , the AMPHIPODA (which includes the Freshwater 'shrimps' Gammarus spp.) and the Decapoda which include the marine shrimps and crabs. The DECAPODA are the largest group of crustaceans, numbering some 8,500 known species. Most are marine, but there are a few fresh water species, the crayfish (Astacus sp.) being a well known example. There are also some terrestrial crabs. Body structureCrustaceans are primitively highly segmented animals, each segment bearing a pair of limbs. More advanced crustaceans, however, have fewer limbs which have tended to become specialised.The crustacean head is fairly uniform, having five pairs of appendages comprising two pairs of antennae, a pair of mandibles and two pairs of maxillae. The thorax consists of a series of limb bearing segments, some of which may have become fused with the head so that their appendages have become incorporated into the mouthparts. The abdomen may or may not have appendages. The appendages are typically biramous, that is having two branches, but may become secondarily uniramous* . As in other arthropods, there has been a tendency towards fewer appendages and more specialised function. Crustaceans, unlike most other arthropods, have a calcified cuticle. Prior to moulting the calcium is reabsorbed and then deposited in the new cuticle. This is probably due to the inability of crustaceans to absorb large amounts of calcium rapidly from their surroundings in a relatively short period of time. |