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==Fossil record== |
==Fossil record== |
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| − | Those crustaceans that have soft [[exoskeleton]]s reinforced with [[calcium carbonate]], such as [[crab]]s and [[lobster]]s, tend to preserve well as fossils, but many crustaceans have only thin exoskeletons. Most of the fossils known are from |
+ | Those crustaceans that have soft [[exoskeleton]]s reinforced with [[calcium carbonate]], such as [[crab]]s and [[lobster]]s, tend to preserve well as fossils, but many crustaceans have only thin exoskeletons. Most of the fossils known are from coral reef or shallow sea-floor environments, but many crustaceans live in open seas, on deep sea-floors or in [[burrow]]s. Crustaceans tend, therefore, to be rarer in the [[fossil record]] than trilobites. Some crustaceans are reasonably common in [[Cretaceous]] and [[Caenozoic]] rocks, but barnacles have a particularly poor fossil record, with very few specimens from before the [[Mesozoic]] era. |
| − | The [[Late Jurassic]] |
+ | The [[Late Jurassic]] lithographic limestone of Solnhofen, Bavaria, which are famous as the home of ''Archaeopteryx'', are relatively rich in [[Decapoda|decapod]] crustaceans, such as ''Eryon'' (an [[Eryonoidea|eryonoid]]), ''Aeger'' (a [[prawn]]) or ''Pseudastacus'' (a [[lobster]]). The "lobster bed" of the Greensand formation from the [[Cretaceous]] period which occurs at Atherfield on the Isle of Wight contains many well preserved examples of the small [[Glypheoidea|glypheoid]] lobster ''Mecochirus magna''. Crabs have been found at a number of sites, such as the Cretaceous Gault clay and the [[Eocene]] London clay. |
| − | ==Consumption== |
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| − | [[Image:2005crustacean.PNG|thumb|Crustacean output in 2005]] |
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| − | Many crustaceans are consumed by humans, and nearly 10,000,000 [[ton]]s were produced in 2005 <ref name="FAO">{{cite web |url=http://www.fao.org/figis/servlet/TabLandArea?tb_ds=Production&tb_mode=TABLE&tb_act=SELECT&tb_grp=COUNTRY |publisher=[[Food and Agriculture Organization]] |accessdate=2007-06-18 |title=FIGIS: Global Production Statistics 1950–2005}}</ref>. The vast majority of this output is of [[Decapoda|decapod crustaceans]]: [[crab]]s, [[lobster]]s, [[shrimp]] and [[prawn]]s. Over 70% by weight of all crustaceans caught for consumption are shrimp and prawns, and over 80% is produced in Asia, with China alone producing nearly half the world's total. Non-decapod crustaceans are not widely consumed, with only 130,000 tons of [[krill]] being caught, despite krill having one of the greatest [[biomass]]es on the planet. |
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==References== |
==References== |
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[[Category:Crustaceans| ]] |
[[Category:Crustaceans| ]] |
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+ | [[Category:Arthropoda]] |
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The nauplius larva of a dendrobranchiate | ||||||||||||
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Porcellio scaber, the common rough woodlouse, a terrestrial crustacean | ||||||||||||
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Pollicipes polymerus, the gooseneck barnacle | ||||||||||||
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Glyphea pseudastacus, a fossil glypheoid |
The crustaceans (Crustacea) are a large group of arthropods, comprising approximately 52,000 described species [1], and are usually treated as a subphylum [2]. They include various familiar animals, such as lobsters, crabs, shrimp, crayfish and barnacles. The majority are aquatic, living in either fresh water or marine environments, but a few groups have adapted to terrestrial life, such as terrestrial crabs, terrestrial hermit crabs and woodlice. The majority are motile, moving about independently, although a few taxa are parasitic and live attached to their hosts (including sea lice, fish lice, whale lice, tongue worms, and Cymothoa exigua, all of which may be referred to as "crustacean lice"), and adult barnacles live a sessile life — they are attached head-first to the substrate and cannot move independently.
The scientific study of crustaceans is known as carcinology. Other names for carcinology are malacostracology, crustaceology and crustalogy, and a scientist who works in carcinology is a carcinologist, crustaceologist or crustalogist.
Structure of crustaceans
Crustaceans have three distinct body parts: head, thorax, and abdomen (or pleon), although the head and thorax may fuse to form a cephalothorax, an excellent example of tagmatization. The head bears two pairs of antennae, one pair of compound eyes and three pairs of mouthparts. The thorax and pleon bear a number of lateral appendages, including the gills, and the tail ends with a telson. Smaller crustaceans respire through their body surface by diffusion [3], and larger crustaceans respire with gills or, as shown by Birgus latro, with abdominal lungs [4]. Both systems (diffusion and gills) were being used by various crustaceans as early as the Middle Cambrian [5].
In common with other arthropods, crustaceans have a stiff exoskeleton which must be shed to allow the animal to grow (ecdysis or moulting). Various parts of the exoskeleton may be fused together; this is particularly noticeable in the carapace, the thick dorsal shield seen on many crustaceans. Crustacean appendages are typically biramous, meaning they are divided into two parts; this includes the second pair of antennae, but not the first, which is uniramous. There is some doubt whether this is a derived state, as had been traditionally assumed, or whether it may be a primitive state, with the branching of the limbs being lost in all extant arthropod groups except the crustaceans. One piece of evidence supporting the latter view is the biramous nature of trilobite limbs [6].
Despite their diversity of form, crustaceans are united by the special larval form known as the nauplius.
Although a few are hermaphroditic, most crustaceans have separate sexes, which are distinguished by appendages on the abdomen called swimmerets or, more technically, pleopods. The first (and sometimes the second) pair of pleopods are specialised in the male for sperm transfer. Many terrestrial crustaceans (such as the Christmas Island red crab) mate seasonally and return to the sea to release the eggs. Others, such as woodlice lay their eggs on land, albeit in damp conditions. In many decapods, the eggs are retained by the females until they hatch into free-swimming larvae.
Taxonomy
Although the classification of crustaceans has been quite variable, the system used by Martin and Davis [1] is the most authoritative, and largely supersedes earlier works.
Six classes of crustaceans are generally recognised:
- Branchiopoda — including brine shrimp (Artemia) and Triops (Notostraca)
- Remipedia — a small class restricted to deep caves connected to salt water, called anchialine caves
- Cephalocarida — horseshoe shrimp
- Maxillopoda — various groups, including barnacles and copepods. It contains Mystacocarida and Branchiura, which are sometimes treated as their own classes.
- Ostracoda — small animals with bivalve shells
- Malacostraca — the largest class, with the largest and most familiar animals, such as crabs, lobsters, shrimp, krill and woodlice.
The exact relationships of the Crustacea to other taxa are not yet entirely clear. Under the Pancrustacea hypothesis [7], Crustacea and Hexapoda (insects and allies) are sister groups. Studies using DNA sequences tend to show a paraphyletic Crustacea, with the insects (but not necessarily other hexapods) nested within that clade.
Fossil record
Those crustaceans that have soft exoskeletons reinforced with calcium carbonate, such as crabs and lobsters, tend to preserve well as fossils, but many crustaceans have only thin exoskeletons. Most of the fossils known are from coral reef or shallow sea-floor environments, but many crustaceans live in open seas, on deep sea-floors or in burrows. Crustaceans tend, therefore, to be rarer in the fossil record than trilobites. Some crustaceans are reasonably common in Cretaceous and Caenozoic rocks, but barnacles have a particularly poor fossil record, with very few specimens from before the Mesozoic era.
The Late Jurassic lithographic limestone of Solnhofen, Bavaria, which are famous as the home of Archaeopteryx, are relatively rich in decapod crustaceans, such as Eryon (an eryonoid), Aeger (a prawn) or Pseudastacus (a lobster). The "lobster bed" of the Greensand formation from the Cretaceous period which occurs at Atherfield on the Isle of Wight contains many well preserved examples of the small glypheoid lobster Mecochirus magna. Crabs have been found at a number of sites, such as the Cretaceous Gault clay and the Eocene London clay.
References
.
- ↑ 1.0 1.1 J. W. Martin & G. E. Davis (2001). An Updated Classification of the Recent Crustacea, 132 pp, Natural History Museum of Los Angeles County.
- ↑ Crustacea (TSN 83677). Integrated Taxonomic Information System. Accessed on 1 May 2006.
- ↑ R. F. Pirow, F. Wollinger & R. J. Paul (1999). The sites of respiratory gas exchange in the planktonic crustacean Daphnia magna: An in vivo study employing blood haemoglobin as an internal oxygen probe. Journal of Experimental Zoology 202 (22): 3089–3099.
- ↑ C. A. Farrelly & P. Greenaway (2005). The morphology and vasculature of the respiratory organs of terrestrial hermit crabs (Coenobita and Birgus): gills, branchiostegal lungs and abdominal lungs. Arthropod Structure and Development 34 (1): 63–87.
- ↑ Vannier, J., M. Williams & D. J. Siveter (1997). The Cambrian origin of the circulatory system of crustaceans. Lethaia 30 (3): 169–184.
- ↑ N. C. Hughes (2003). Trilobite tagmosis and body patterning from morphological and developmental perspectives. Integrative and Comparative Biology 43 (1): 185–206.
- ↑ J. Zrzavý & P. Štys (1997). The basic body plan of arthropods: insights from evolutionary morphology and developmental biology. Journal of Evolutionary Biology 10: 353-367.
General references
- Frederick Schram (1986). Crustacea, 620 pp, Oxford University Press. ISBN 0-19-503742-1.
External links
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