Xiphosura

Modern xiphosurans reach up to in adult length, but the Paleozoic species were often far smaller, some as small as long. Their bodies are divided into an anterior prosoma and a posterior opisthosoma, or abdomen. The upper surface of the prosoma is covered by a semicircular carapace, while the underside bears five pairs of walking legs and a pair of pincer-like chelicerae. The mouth is located on underside of the center of the prosoma, between the bases of the walking legs, and lies behind a lip-like structure called the labrum. The exoskeleton consist of a tough cuticle, but do not contain any crystalline biominerals. Like scorpions, xiphosurans have an exocuticular layer of hyaline which exhibits UV fluorescence. Xiphosurans have up to four eyes, located in the carapace. Two compound eyes are on the side of the prosoma, with one or two median ocelli towards the front. The compound eyes are simpler in structure than those of other arthropods, with the individual ommatidia not being arranged in a compact pattern. They can probably detect movement, but are unlikely to be able to form a true image. In front of the ocelli is an additional organ that probably functions as a chemoreceptor. These are thought to be vestiges of the limbs of an absorbed first opisthosomal segment. The underside of the opisthosoma carries the genital openings and five pairs of flap-like gills. The opisthosoma terminates in a long caudal spine, commonly referred to as a telson (though this same term is also used for a different structure in crustaceans). The spine is highly mobile, and is used to push the animal upright if it is accidentally turned over. Internal anatomy The mouth opens into a sclerotised oesophagus, which leads to a crop and gizzard. After grinding up its food in the gizzard, the animal regurgitates any inedible portions, and passes the remainder to the true stomach. The stomach secretes digestive enzymes, and is attached to an intestine and two large caeca that extend through much of the body, and absorb the nutrients from the food. The intestine terminates in a sclerotised rectum, which opens just in front of the base of the caudal spine. Xiphosurans have well-developed circulatory systems, with numerous arteries that send blood from the long tubular heart to the body tissues, and then to two longitudinal sinuses next to the gills. After being oxygenated, the blood flows into the body cavity, and back to the heart. The blood contains haemocyanin, a blue copper-based pigment performing the same function as haemoglobin in vertebrates, and also has blood cells that aid in clotting. The excretory system consists of two pairs of coxal glands connected to a bladder that opens near the base of the last pair of walking legs. The brain is relatively large, and, as in many arthropods, surrounds the oesophagus. In both sexes, the single gonad lies next to the intestine and opens on the underside of the opisthosoma. ==Reproduction==

Xiphosurans move to shallow water to mate. The male climbs onto the back of the female, gripping her with his first pair of walking legs. The female digs out a depression in the sand, and lays from 200 to 300 eggs, which the male covers with sperm. The pair then separates, and the female buries the eggs. Through a series of successive moults, the larva develops additional gills, increases the length of its caudal spine, and gradually assumes the adult form. Modern xiphosurans reach sexual maturity after about three years of growth. == Evolution ==

Evolutionary history The oldest known xiphosurans are specimens from the Early Ordovician Fezouata Formation of Morocco, dating to around 480 million years ago, but these are currently undescribed. Ciurcalimulus is the only Xiphosuran known from the following Silurian. Xiphosurida first appears during the late Devonian. A major radiation of freshwater xiphosurids, the Belinuridae, is known from the Carboniferous, with the oldest representatives of the modern family Limulidae also possibly appearing during this time, though they only appear in abundance during the Triassic. Another major radiation of freshwater xiphosurans, the Austrolimulidae, is known from the Permian and Triassic. As a group they have never showed much diversity in regard of species. Less than 50 fossil species are known from the Carboniferous period, when they were at their most diverse. The last common ancestor of modern limulids has been suggested to date to the Jurassic-Cretaceous boundary based on molecular clock dating though depending on phylogeny the fossil record may suggest a split as old as the Triassic. Taxonomy Xiphosuran classification : Order Xiphosura Latreille, 1802 • †Ciurcalimulus Lamsdell, 2025 (Silurian) • †Lunataspis Rudkin, Young & Nowlan, 2008 (Ordovician) • †Maldybulakia Tesakov & Alekseev, 1998 (Devonian) • †Willwerathia Størmer, 1969 (Devonian) • †Kasibelinuridae Pickett, 1993 (Middle Devonian to Late Devonian) • Suborder Xiphosurida • †Infraorder Belinurina • †Belinuridae Zittel & Eastman, 1913 (Middle Devonian to Upper Carboniferous) • Infraorder Limulina • †Bellinuroopsis Chernyshev, 1933 (Carboniferous) • †Rolfeiidae Selden & Siveter, 1987 (Early Carboniferous to Early Permian) • Superfamily †Paleolimuloidea Anderson & Selden, 1997 • †Paleolimulidae Raymond, 1944 (Carboniferous to Permian) • Superfamily Limuloidea • †Valloisella Racheboeuf, 1992 (Carboniferous) • †Austrolimulidae Riek, 1955 (Early Permian-Early Jurassic) • Limulidae Zittel, 1885 (Triassic to recent) • Limulinae Zittel, 1885 (Late Jurassic-Present) • Tachypleinae Pocock, 1902 (Late Cretaceous-Recent) Two groups were originally included in the Xiphosura, but since have been assigned to separate classes: • Aglaspida Walcott, 1911 (Cambrian to Ordovician) • Chasmataspidida Caster & Brooks, 1956 (Lower Ordovician) == See also ==