Amphisbaenia

Despite a superficial resemblance to some primitive snakes, amphisbaenians have many unique features that distinguish them from other reptiles. Internally, their right lung is reduced in size to fit their narrow bodies, whereas in snakes, it is always the left lung. Their skeletal structure and skin are also different from those of other squamates. Both genetic and recent fossil evidence indicate that amphisbaenians lost their legs independently from snakes. The head is stout, not set off from the neck, and either rounded, sloped, or sloped with a ridge down the middle. Most of the skull is solid bone, with a distinctive single median tooth in the upper jaw. It has no outer ears, and the eyes are deeply recessed and covered with skin and scales. These rudimentary eyes have a cornea, lens, and complex ciliary body, which allows them to detect light, but they are reduced in size and do not have an anterior chamber. The body is elongated, and the tail truncates in a manner that vaguely resembles the head. At their tail is a single fracture plane for tail autotomy, between the fifth and eighth caudal rings and is often visible due to coloration. The purpose seems to be to distract predators with the tail acting as a decoy. Their name is derived from Amphisbaena, a mythical serpent with a head at each end—referencing both the manner in which their tail truncates, and their ability to move just as well in reverse as forwards. The four species of Bipes are unusual in having a pair of forelimbs. All other species lack any trace of forelimb skeletal elements, and Rhineura floridana also lack any pectoral girdle skeletal element. The other species have some remnants of the pectoral girdle embedded within the body musculature. A remnant of the pelvic girdle is present in all families, and Bipes and the genus Blanus have also retained a reduced femur. Amphisbaenians have a distinctive skin made up of rings of scales (annuli) that form a tube in which the loosely attached trunk of the body moves. Burrowing is achieved with an accordion-like motion, with longitudinal muscles in the skin bunching up the annuli, anchoring it to the surrounding soil, and trunk muscles moving the body forward or backwards within the integumentary tube. Amphisbaenians are carnivorous, able to tear chunks out of larger prey with their powerful, interlocking teeth. Like lizards, some species are able to shed their tails (autotomy). Most species lay eggs, although at least some are known to be viviparous. Amphisbaenians have often been categorized by their skull shape. The specialized skull shape is hypothesized to be driven by environmental and ecological conditions, such as soil type, and is an instance of convergent evolution. Traditionally four types of skulls are recognized; "shovel-headed", "round-headed", "keel-headed", and "spade-headed", although it doesn't say anything about the relationship between the types. Of these four morphotypes, the round-headed species produce the lowest burrowing forces, the shovel-headed species the second lowest forces, the keel-headed species the second highest forces, and the spade-headed the highest forces. ==Distribution==

Amphisbaenians are found in North America, Europe, Africa, South America, the Middle East, and the Caribbean, a surprisingly large distribution despite being small subterranean animals that rarely ever leave their burrows. Initially, this large distribution was thought to be due to vicariance, or the result of the breakup of Pangaea. This hypothesis was supported by morphological data that dated amphisbaenian diversification to over 200 million years ago (Mya), while Pangaea was still intact. However, a recent study using a combination of molecular and fossil evidence suggests that amphisbaenians originated in North America, where they underwent their first divergence around 107 Mya. They then underwent another major diversification into North American and European forms 40–56 Mya. Finally, the African and South American forms split around 40 Mya. This suggests that worm-lizards crossed the Atlantic Ocean (which had fully formed by 100 Mya) twice, once just after the K–Pg extinction, and then again, later in the Palaeogene. This also implies that limblessness evolved independently three times, a finding that contrasts the morphological theory that limbed amphisbaenians are the most basal. This widespread dispersal is suggested to have occurred by rafting – natural erosion or a storm event loosened a large raft of soil and vegetation that drifted across the ocean until landing on another shore. This oceanic rafting would be feasible due to the subterranean lifestyle and small nutritional requirements of amphisbaenids. After the Chicxulub impact, many predators of amphisbaenians became extinct, which allowed colonist amphisbaenians to thrive in new territories. == Evolution ==

from the Late Cretaceous of Mongolia The fully limbed Slavoia darevskii from the Late Cretaceous (Campanian) of Mongolia may represent an early relative of amphisbaenians. The oldest known modern amphisbaenians include members of Rhineuridae and the extinct family Oligodontosauridae from the Paleocene of North America. Modern amphisbaenians likely originated in North America, before dispersing to South America, Africa and Europe via rafting during the Paleogene. The phylogenetic placement of Amphisbaenia and other limbless clades is historically complex, and musculoskeletal variability within the clade itself has led to much evolutionary confusion. Although many amphisbaenians are limbless, limb retention and developed pelvic structures do exist throughout the clade. The family Bipedidae exhibit fully developed forelimbs, Blanidae and Trogonophidae retain several pectoral girdle elements, and Rhineuridae display a minimal pelvic structure. Through parsimony and Baysian analysis, modern Amphisbaenia was proposed as sister taxon to Cryptolacerta, supported by 19 shared characters. Neither of these were characters shared by Cryptolacerta. The morphological and molecular study and published evaluation of legless origins in amphisbaenia continue to be evolutionarily contested, and scientific classification will continue to shift with additional evidence and scientific reevaluation. == Taxonomy ==

Taxonomic classification of amphisbaenians was traditionally based on morphological characters, such as the number of preanal pores, body annuli, tail annuli, and skull shape. Such characters are vulnerable to convergent evolution; in particular, the loss of the forelimbs and the evolution of specialized shovel-headed and keel-headed morphs appear to have occurred multiple times in the history of the group. Classifications based on mitochondrial DNA sequences and nuclear DNA sequences better reflect their true evolutionary history, and are now being used to distinguish genera of amphisbaenians. The most ancient branch of the tree is the Rhineuridae. The remaining five families form a group to the exclusion of rhineurids. Bipedidae, Blanidae, and Cadeidae represent the most ancient divergences within this grouping, with Trogonophidae and Amphisbaenidae diverging more recently. South American amphisbaenids apparently are derived from African amphisbaenids that rafted across the Atlantic in the Eocene, about 40 million years ago. though many modern studies consider them to be true lizards, as they are closely related to other lizards of the clade Lacertoidea. • Amphisbaenidae Gray, 1865 – Amphisbaenids, tropical worm lizards of South America, some Caribbean islands, and Sub-Saharan Africa. (12 genera, 182 species) • Bipedidae Taylor, 1951 – Only in Mexico and commonly called ajolotes, but not to be confused with axolotls (1 genus, 3 species) • Blanidae Kearney & Stuart, 2004 – Anatolian, Iberian, and Moroccan worm lizards (1 genus, 7 species) • Cadeidae Vidal and Hedges, 2008 – Cuban keel-headed worm lizards (1 genus, 2 species). Traditionally amphisbaenids, but shown by DNA to be closest to Blanidae. (1 genus, 1 species) • Trogonophidae Gray, 1865 – Palearctic worm lizards (4 genera, 6 species) In addition, the following extinct families are also known from fossil remains: • †Chthonophidae Longrich et al., 2015 • †Oligodontosauridae Estes, 1975 • †Polyodontobaenidae Folie, Smith & Smith, 2013 Another fossil family, the †Crythiosauridae, was also previously placed in this group, but has since been removed due to a lack of evidence placing it within the amphisbaenians. Phylogeny The following cladogram shows the relationships between the six amphisbaenian families determined in the phylogenetic analysis of mitochondrial and nuclear genes by Vidal et al. (2008). }} ==References==