Eucrenonaspides | |
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Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Arthropoda |
Class: | Malacostraca |
Order: | Anaspidacea |
Family: | Psammaspididae |
Genus: | Eucrenonaspides Knott & Lake, 1980 |
Species: | E. oinotheke |
Binomial name | |
Eucrenonaspides oinotheke Knott & Lake, 1980 | |
Eucrenonaspides oinotheke is a species of crustacean in the family Psammaspididae, endemic to Tasmania, the only species described in the genus Eucrenonaspides. Eucrenonaspides is in the order Anaspidacea. [2] It was described from a spring at 9 Payton Place, Devonport, Tasmania in 1980, making it "the first spring-dwelling syncarid recorded from the Australian region". It is listed as a vulnerable species on the IUCN Red List. A further undescribed species is known from south-western Tasmania. [3]
Eucrenonaspides oinotheke is a type of crustacean and part of the Anaspidacea order. Eucrenonaspides oinotheke has its own unique structure that encompasses a head and thorax. These do not have a shieldlike carapace and the first thoracic segment is tightly joined with the head. They also have pairs of maxillipeds, and thoracic limbs associated with the mouth. The head of Eucrenonaspides oinotheke is sub-rectangular and divided into two unequal regions by transverse mandibular grooves. Each side of the head is a mandibular groove which meet in the midline. These mandibular groove's pass obliquely backward to a level near the posterior margin of the head and defines an inferior plate. Eucrenonaspides oinotheke's head appendages and the antennule, a small antenna in a crustacean, includes a peduncle of three segments, a comparatively robust outer flagellum which is approximately half the total body length. [4] Further, the antennule comprises a peduncle of three segments, a comparatively robust outer flagellum which is approximately half the total body length. There is a side boundary of the large basal segment which is curved convexly at the base. The male antennule available for study does not show a sensory modification on the basal outer flagellum segment, but all specimens have a small, triangular projection on the dorsal margin of this segment which supports a long seta. The number of segments per outer flagellum varies from 17 to 29 and from 6 to 10 for the inner one. The outer flagellum is approximately twice the length of the inner one. The number of segments in the flagellum varies from 8 to 21. [4] The pleon is known as the abdomen of a crustacean. [5] In Eucrenonaspides oinotheke, the pleon is slightly flattened where along the posterior margin there is a row of long setospines. Pleonites can bear one pair of pleopods where the exopodites are long and multisegmented or short. The pleopods do not have endopodites. [4]
Additionally, Eucrenonaspides oinotheke contains pairs of thoracic legs which are either unbranched or branched. In biramous legs, the inner branch is called the endopod, and the outer branch is called the exopod. They also have flaplike gills, used for breathing underwater, which are located on the bases of the legs. The movements of the exopods keep oxygen-carrying water flowing over the gills. The abdomen also has segments where there are five pairs of pleopods or limblike structures attached to the underside of the abdomen. The tip of the abdomen has a pair of long appendages called uropods which are found on either side of a central tail segment, or telson. They also have an abdomen has a pair of long appendages called uropods. The uropods are found on either side of a central tail segment, or telson. [5] Eucrenonaspides oinotheke does not have eyes with a slender body that does not reflect a colour and is classified as transparent. [4]
Eucrenonaspides oinotheke is part of crustacean fauna and a larger species of the Anaspidaceans. Their main habitat is caves, cave streams, lakes and terrestrial woodlice along with millipede located in Tasmania. They are predominantly found in drip pools, seepages and similar habitats out of the main flow of water. [6] However, Eucrenonaspides oinotheke do not exist in groundwaters of the mainland. [7]
Eucrenonaspides oinotheke in particular was found near the centre of a large town, the spring at Payton Place, Devonport. Although springs are common in and about Devonport, particularly in areas of basalt substrates, efforts to find other sources of the species or related forms have proved unsuccessful. The distribution of Psammaspids and thus Eucrenonaspides oinotheke are only known to occur at 3 widely separated localities of New South Wales, Tasmania and Camperdown, Western Victoria. This has shown the family of the Psammaspids were once, distributed across the whole of southern Australia. This area experienced a wet climate, that could stem from the Triassic until midway through the Tertiary, although part of this area was inundated by marine transgressions during the early Cretaceous. Subsequently, there is a chance that they may be found elsewhere in southern Australia, such as in springs in Western Australia. [8]
Eucrenonaspides ointheke found in Tasmanian caves are exposed to many threats. This is because caves are dependent for their fundamental energy and vulnerable to the environment around them. Cave ecosystems are predominately at risk from development pressure on land and harm from humans such as quarrying or pollution. Additionally, water mainly carries in food to the temperate caves, making their fauna at risk from land use practices which affect the quality of water entering them. This would threaten the drinking and liveable water for Eucrenonaspides. Human harm can also threaten Eucrenonaspides ointheke that are living in seepage pools as these can be destroyed by footsteps. [9]
As Eucrenonaspides ointheke lives in a habitat of cave dwelling classified as pools, or streamways there are numerous threats. These pools, and their associated seepage waters, may be colonised by a fauna which is distinct from that in larger streamways. These small and patchily distributed habitats are sensitive to trampling impacts that include human footsteps that can degrade and destroy them. This is harmful as streams are a vital macro-habitat as they support an abundant aquatic fauna and transport the food supply for much of the terrestrial fauna. Food sources transported by streams include plant detritus such as wood and leaf litter, and accidental species. [10]
Trout are another threat to Eucrenonaspides ointheke. The trout there introduced by Australian colonists from Europe and thus Eucrenonaspides ointheke does not have natural defences against this species. They therefore can only survive in isolated branches of streams and rivers that are out of reach from the trout. The conservation status of Eucrenonaspides ointheke is vulnerable or facing high rate of extinction in the wild, listed by the World conservation Union (IUCN). [9]
Eucrenonaspides oinotheke use their thoractic legs to crawl in their habitat which constantly circulates oxygen-carrying water over their flaplike gills. Their thoracic and abdominal limbs move together in a smooth, rhythmic motion. [6] They are not strong swimmers, in its place they typically walk over the substrate. The exopods of the thoracic legs are in constant motion to circulate fresh, oxygen-bearing water past the flattened epipods. When they are startled, they are capable of jumping upwards. [11]
Males and females are known, but there is no research on mating. Unlike most crustaceans that carry their eggs or young, female Anaspidaceans and thus Eucrenonaspides oinotheke lay their eggs individually on plants or stones. Subsequently, they do not guard or provide care for their young. The eggs hatch between 30 and 60 days as larvae that encompass antennae and mouthparts only. Adulthood is reached through a series of molts, or sheddings of the exoskeleton and appendages are added with each molt. [8]
The eggs are attached to bits of bark or plant or laid in crevices where in living forms, development is slow. Eggs are laid in spring or early summer and take 32–35 weeks to hatch; those laid in the fall take 60 weeks to hatch because of a period of winter inactivity. There are two peaks occur for hatching: April–May and July–August. Animals hatch as juveniles, and the ability to distinguish between the two hatching peaks by size departs after the first year. [8]
The digestive system of Eucrenonaspides oinotheke consists of a short esophagus which leads to the cardiac stomach and an esophagus plug which extends into the cardiac stomach. The ceca arise as a mass of long strands at the forward end of the midgut and extend the length of the thorax. [8] There are also single short median dorsal ceca in the first and fifth pleomeres. The proctodeum extends inwards from the anus to the level of the sixth pleomere. There are no gastric mill, ossicles or teeth in the foregut. This small stomach framework thus constrains the diet. [8]
The circulatory system contains the heart which extends from the first thoracomere to the fourth pleomere. One pair of ostia is found in the third thoracomere, and anterior and posterior dorsal aortae extend outward from the heart. There are seven pairs of lateral arteries containing visceral and podial branches. [8] The first pair arises from the anterior end of the heart and extends into the head. The second pair is found in the last thoracomere, with one of the branches forming a ventral aorta to supply the thoracopods and the third pair arises in the first pleomere to supply the thoracic viscera. The rest supply the viscera and the pleopods. [8]
Additionally, the nervous system centers on a large supra-esophageal ganglion, without a large, fused, subesophageal ganglion; the post-oral ganglia in the trunk are all separate and distinct. The nerve cord includes a band of fibers connecting the segmental ganglia and two sets of lateral, giant fibers. [8] These occur on either side in the nerve cord which are effective in eliciting a caridoid escape reaction. This is where the entire series of trunk segments flexes at once, exhibiting an evasive reaction, but does not move the animal away from danger. Additional sensory organs include statocysts in the antennules and distinctive dorsal organs on the head where the eyes are absent. [8]
Eucrenonaspides oinotheke eat plant and animal materials and are thus considered omnivores. They search constantly for food, chewing on large pieces of plants or scraping the surfaces of pebbles with its mouth. The streams that Eucrenonaspides oinotheke live in play a large role in their diet. This is because the macro-habitat transports the food supply. The food sources transported by streams include plant detritus such as wood and leaf litter, and accidental species. [10]
Eucrenonaspides oinotheke came from a ground spring in a house wine cellar at 6 Payton Place, Devonport. Researchers from the San Diego Natural History Museum tried to recollect this locality in 1990 however due to a drought sighting was found difficult and further research on the history of Eucrenonaspides oinotheke is unknown. [8]
Dendrobranchiata is a suborder of decapods, commonly known as prawns. There are 540 extant species in seven families, and a fossil record extending back to the Devonian. They differ from related animals, such as Caridea and Stenopodidea, by the branching form of the gills and by the fact that they do not brood their eggs, but release them directly into the water. They may reach a length of over 330 millimetres (13 in) and a mass of 450 grams (1.0 lb), and are widely fished and farmed for human consumption.
Malacostraca is the second largest of the six classes of pancrustaceans just behind hexapods, containing about 40,000 living species, divided among 16 orders. Its members, the malacostracans, display a great diversity of body forms and include crabs, lobsters, crayfish, shrimp, krill, prawns, woodlice, amphipods, mantis shrimp, tongue-eating lice and many other less familiar animals. They are abundant in all marine environments and have colonised freshwater and terrestrial habitats. They are segmented animals, united by a common body plan comprising 20 body segments, and divided into a head, thorax, and abdomen.
The Decapoda or decapods are an order of crustaceans within the class Malacostraca, and includes crabs, lobsters, crayfish, shrimp, and prawns. Most decapods are scavengers. The order is estimated to contain nearly 15,000 extant species in around 2,700 genera, with around 3,300 fossil species. Nearly half of these species are crabs, with the shrimp and Anomura including hermit crabs, porcelain crabs, squat lobsters making up the bulk of the remainder. The earliest fossils of the group date to the Devonian.
Mysida is an order of small, shrimp-like crustaceans in the malacostracan superorder Peracarida. Their common name opossum shrimps stems from the presence of a brood pouch or "marsupium" in females. The fact that the larvae are reared in this pouch and are not free-swimming characterises the order. The mysid's head bears a pair of stalked eyes and two pairs of antennae. The thorax consists of eight segments each bearing branching limbs, the whole concealed beneath a protective carapace and the abdomen has six segments and usually further small limbs.
Isopoda is an order of crustaceans. Members of this group are called Isopods and include both terrestrial and aquatic 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.
The decapod is made up of 20 body segments grouped into two main body parts: the cephalothorax and the pleon (abdomen). Each segment may possess one pair of appendages, although in various groups these may be reduced or missing. They are, from head to tail:
The Cephalocarida are a class in the subphylum Crustacea comprising only 12 species. Both the nauplii and the adults are benthic. They were discovered in 1955 by Howard L. Sanders, and are commonly referred to as horseshoe shrimp. They have been grouped together with the Remipedia in the Xenocarida. Although a second family, Lightiellidae, is sometimes used, all cephalocaridans are generally considered to belong in just one family: Hutchinsoniellidae. Fossil records of cephalocaridans has been found in 462 million year old deposits.
Leptostraca is an order of small, marine crustaceans. Its members, including the well-studied Nebalia, occur throughout the world's oceans and are usually considered to be filter-feeders. It is the only extant order in the subclass Phyllocarida. They are believed to represent the most primitive members of their class, the Malacostraca, and first appear in the fossil record during the Cambrian period.
Eumalacostraca is a subclass of crustaceans, containing almost all living malacostracans, or about 40,000 described species. The remaining subclasses are the Phyllocarida and possibly the Hoplocarida. Eumalacostracans have 19 segments. This arrangement is known as the "caridoid facies", a term coined by William Thomas Calman in 1909. The thoracic limbs are jointed and used for swimming or walking. The common ancestor is thought to have had a carapace, and most living species possess one, but it has been lost in some subgroups.
Cumacea is an order of small marine crustaceans of the superorder Peracarida, occasionally called hooded shrimp or comma shrimp. Their unique appearance and uniform body plan makes them easy to distinguish from other crustaceans. They live in soft-bottoms such as mud and sand, mostly in the marine environment. There are more than 1,500 species of cumaceans formally described. The species diversity of Cumacea increases with depth.
Triops longicaudatus is a freshwater crustacean of the order Notostraca, resembling a miniature horseshoe crab. It is characterized by an elongated, segmented body, a flattened shield-like brownish carapace covering two thirds of the thorax, and two long filaments on the abdomen. The genus name Triops comes from Greek ὤψ or ṓps, meaning "eye" prefixed with Latin tri-, "three", in reference to its three eyes. Longicaudatus is a Latin neologism combining longus ("long") and caudatus ("tailed"), referring to its long tail structures. Triops longicaudatus is found in fresh water ponds and pools, often in places where few higher forms of life can exist.
Diastylidae is one of the eight most commonly recognised families of crustaceans of the order Cumacea. They are marine creatures especially common around the 30th parallel north.
Gynodiastylidae is one of the eight most commonly recognised families of crustaceans of the order Cumacea. They are especially prevalent in the southern hemisphere, with some types described from Japan, Thailand and the Persian Gulf. Most are found at less than 100 metres (330 ft) depth.
Leuconidae is a family of marine hooded shrimp. The family was established by Georg Ossian Sars in his 1878 study of Mediterranean cumaceans.
Crustaceans may pass through a number of larval and immature stages between hatching from their eggs and reaching their adult form. Each of the stages is separated by a moult, in which the hard exoskeleton is shed to allow the animal to grow. The larvae of crustaceans often bear little resemblance to the adult, and there are still cases where it is not known what larvae will grow into what adults. This is especially true of crustaceans which live as benthic adults, more-so than where the larvae are planktonic, and thereby easily caught.
Phylogeny of Malacostraca is the evolutionary relationships of the largest of the six classes of crustaceans, containing about 40,000 living species, divided among 16 orders. Its members display a great diversity of body forms. Although the class Malacostraca is united by a number of well-defined and documented features, which were recognised a century ago by William Thomas Calman in 1904, the phylogenetic relationship of the orders which compose this class is unclear due to the vast diversity present in their morphology. Molecular studies have attempted to infer the phylogeny of this clade, resulting in phylogenies which have a limited amount of morphological support. To resolve a well-supported eumalacostracan phylogeny and obtain a robust tree, it will be necessary to look beyond the most commonly utilized sources of data.
Periclimenes pholeter, is a species of shrimp belonging to the family Palaemonidae. The species is closest to Periclimenes indicus, P. obscurus and P. toloensis, resembling these species in the presence of an epigastric tooth on the carapace, the shape of the abdomen, the spinulation of the carapace, and the unarmed fingers of the first chelipeds. P. pholeter most resembles P. indicus by the elongatecarpus and long fingers of the second pereiopods, differing in these features from P. toloensis, which has the fingers slightly less than half as long as the palm. In P. obscurus the fingers are shorter than the palm, but the carpus is about as long as the palm. From P. indicus, this species differs: by the greater size; by the much higher rostrum and the greater number of ventral rostral teeth; by the shorter eye; by the less slender antennular peduncle; by the more deeply cleft upper antennular flagellum; by the more robust scaphocerite; by the fingers of the first pereiopods ; by the more slender pereiopods, especially the fifth, which is much longer than the ischium.
Crustaceans are a group of arthropods that are a part of the subphylum Crustacea, a large, diverse group of mainly aquatic arthropods including decapods, seed shrimp, branchiopods, fish lice, krill, remipedes, isopods, barnacles, copepods, opossum shrimps, amphipods and mantis shrimp. The crustacean group can be treated as a subphylum under the clade Mandibulata. It is now well accepted that the hexapods emerged deep in the Crustacean group, with the completed group referred to as Pancrustacea. The three classes Cephalocarida, Branchiopoda and Remipedia are more closely related to the hexapods than they are to any of the other crustaceans.
Perimecturus is an extinct genus of mantis shrimp that lived during the Early Carboniferous period in what is now Scotland and the United States. The first known specimens were collected near the River Esk in Glencartholm, Scotland, and the genus was named in 1908 by Ben Peach, making it the second genus of Paleozoic mantis shrimp to be described. While many species have been classified in the genus since then, taxonomic revisions in the late 20th and 21st centuries have reassigned most of these to different genera, leaving two named species currently assigned to this genus. The type species, P. parki, was first named in 1882 as a species of Anthrapalaemon and is known from the Viséan-aged Glencartholm Volcanic Beds of Scotland. Fossils of a later species, P. rapax, have been found in the Bear Gulch Limestone of Montana and were first described by Frederick Schram.
Nodosculda is an extinct genus of mantis shrimp that lived in North America during the late Albian stage of the Early Cretaceous period, between 105 and 100 million years ago. The only species is Nodosculda fisherorum, known from several specimens uncovered in the Paw Paw Formation of Texas.