Phylogenetic bracketing is a method of inference used in biological sciences. It is used to infer the likelihood of unknown traits in organisms based on their position in a phylogenetic tree. One of the main applications of phylogenetic bracketing is on extinct organisms, known only from fossils, going back to the last universal common ancestor (LUCA). The method is often used for understanding traits that do not fossilize well, such as soft tissue anatomy, physiology and behaviour. By considering the closest and second-closest well-known (usually extant) organisms, traits can be asserted with a fair degree of certainty, though the method is extremely sensitive to problems from convergent evolution.
Extant Phylogenetic Bracketing requires that the species forming the brackets be extant. More general forms of phylogenetic bracketing do not require this and may use a mix of extant and extinct taxa to form the bracket. These more generalized forms of phylogenetic bracketing have the advantage in that they can be applied to a wider array of phylogenetic cases. However, since these forms of bracketing are also more generalized and may rely on inferring traits in extinct animals, they also offer lower explanatory power compared to the EPB.
This is a popular form of phylogenetic bracketing first introduced by Witmer in 1995. [1] It works by comparing an extinct taxon to its nearest living relatives. [1] [2] [3] For example, Tyrannosaurus , a theropod dinosaur, is bracketed by birds and crocodiles. A feature found in both birds and crocodiles would likely be present in Tyrannosaurus, such as the capability to lay an amniotic egg, whereas a feature both birds and crocodiles lack, such as hair, would probably not be present in Tyrannosaurus. Sometimes this approach is used for the reconstruction of ecological traits as well. [4]
The extant phylogenetic bracket approach allows researchers to infer traits in extinct animals with varying levels of confidence. This is referred to as the levels of inference. [1] There are three levels of inference, with each higher level indicating less confidence for the inference. [1]
Level 1 — The inference of a character that leaves a bony signature on the skeleton in both members of the extant sister groups. Example: Saying that Tyrannosaurus rex had an eyeball is a level 1 inference because both extant members of the groups encompassing Tyrannosaurus rex have eyeballs, and eyeball sockets (orbital excavations) in the skull, the homology of which is well established, and the fossils of Tyrannosaurus rex skulls have similar morphology. [1]
Level 2 — The inference of a character that leaves a signature on the skeleton of only one of the extant sister groups. [1] For example, saying that Tyrannosaurus rex had air sacs running through its skeleton is a level 2 inference as birds are the only extant sister group to Tyrannosaurus rex to show such air sacs. However the underlying pneumatic fossae, air sacs, in the bones of extant birds are remarkably similar to the cavities seen in the fossil vertebrae of Tyrannosaurus rex. The high degree of similarity between the pneumatic fossae in Tyrannosaurus rex and extant birds makes this a fairly strong inference, yet not as strong as a level 1 inference.
Level 3 — The inference of a character that leaves a bony signature on the skeleton but is not present in either extant sister group to the taxon in question. [1] For example, saying that ceratopsian dinosaurs such as Triceratops horridus had horns in life would be a level 3 inference. Neither extant crocodylians, nor extant birds have horns today, but the osteological evidence for horns in ceratopsians is without question. Thus a level 3 inference receives no support from the extant phylogenetic bracket, but can still be used with confidence based on the merits of the fossil data itself.
The Extant Phylogenetic Bracket can be used to infer the presence of soft tissues even when those tissues do not interact with the skeleton. As before, there are three different levels of inference. These levels are designated as prime levels. They descend in confidence as they move up a level. [1]
Level 1′ — The inference of a character that is shared by both extant sister groups, but does not leave behind a bony signature. [1] For example, saying that Tyrannosaurus rex had a four-chambered heart would be a level 1′ inference as both extant sister groups (Crocodylia and Aves) have four-chambered hearts, but this trait does not leave behind any bony evidence.
Level 2′ — The inference of a character that is found in only one sister group to the taxon in question and that does not leave behind any bony evidence. [1] For instance saying that Tyrannosaurus rex was warm-blooded would be a level 2′ inference as extant birds are warm-blooded but extant crocodylians are not. Further, since warm-bloodedness is a physiological trait rather than an anatomical one, it does not leave behind any bony signatures to indicate its presence.
Level 3′ — The inference of a character that is found in neither sister group to the taxon in question and that does not leave behind any bony signatures. [1] For example, saying that the large sauropod dinosaur Apatosaurus ajax gave birth to live young similar to mammals and many lizards [5] would be a level 3′ inference as neither crocodylians nor birds give birth to live young and these traits do not leave impressions on the skeleton.
In general the primes are always less confident than their underlying levels; however, the confidence between levels is less clear cut. For instance it is unclear if a level 1′ would be less confident than a level 2. The same would go for a level 2′ versus a level 3. [1]
The Late Cretaceous Kryptobaatar and the extant monotremes (family Tachyglossidae and Ornithorhynchidae) all sport extratarsal spurs on their hind feet. Greatly simplified, the phylogeny is as follows, with taxa known to have extratarsal spurs in bold: [6]
Mammalia |
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Assuming that the Kryptobaatar and monotreme spurs are homologous, they were a feature of their mammalian last common ancestor, so we can tentatively conclude that they were present among the Early Cretaceous Eobaataridae—its descendants—as well.
A fragmentary fossil with a known phylogeny can be compared to more complete fossil specimen to give an idea about general build and habit. The body of labyrinthodonts can usually be inferred to be broad and squat with a sideways compressed tail, although only the skull has been known for many taxa, based on the shape of more well-known labyrinthodont finds.
Phylogenetic bracketing is based on the notion of anatomical conservationism. The general body shape of an animal can be fairly constant through large groups, but not always.
The large theropod dinosaur Spinosaurus was until 2014 only known from fragmentary remains, mainly of the skull and vertebrae. It was assumed that the remaining skeleton would look more or less like that of related animals like Baryonyx and Suchomimus , who sport a traditional theropod anatomy of long, strong hind legs and relatively small front legs. A 2014 find, however, included a set of hind legs. [7] The new reconstruction indicate earlier Spinosaurus reconstructions were wrong, and the animal was mainly aquatic and had relatively weak hind legs. It is possible it walked on all fours when on land, the only theropod to do so. [8]
Tyrannosaurus is a genus of large theropod dinosaur. The type species Tyrannosaurus rex, often shortened to T. rex or colloquially T-Rex, is one of the best represented theropods. It lived throughout what is now western North America, on what was then an island continent known as Laramidia. Tyrannosaurus had a much wider range than other tyrannosaurids. Fossils are found in a variety of rock formations dating to the latest Campanian-Maastrichtian ages of the late Cretaceous period, 72.7 to 66 million years ago. It was the last known member of the tyrannosaurids and among the last non-avian dinosaurs to exist before the Cretaceous–Paleogene extinction event.
Tyrannosauridae is a family of coelurosaurian theropod dinosaurs that comprises two subfamilies containing up to fifteen genera, including the eponymous Tyrannosaurus. The exact number of genera is controversial, with some experts recognizing as few as three. All of these animals lived near the end of the Cretaceous Period and their fossils have been found only in North America and Asia.
Theropoda whose members are known as theropods, is an extant dinosaur clade that is characterized by hollow bones and three toes and claws on each limb. Theropods are generally classed as a group of saurischian dinosaurs. They were ancestrally carnivorous, although a number of theropod groups evolved to become herbivores and omnivores. Theropods first appeared during the Carnian age of the late Triassic period 231.4 million years ago (Ma) and included the majority of large terrestrial carnivores from the Early Jurassic until at least the close of the Cretaceous, about 66 Ma. In the Jurassic, birds evolved from small specialized coelurosaurian theropods, and are today represented by about 11,000 living species.
Spinosaurus is a genus of spinosaurid dinosaur that lived in what now is North Africa during the Cenomanian stage of the Late Cretaceous period, about 100 to 94 million years ago. The genus was known first from Egyptian remains discovered in 1912 and described by German palaeontologist Ernst Stromer in 1915. The original remains were destroyed in World War II, but additional material came to light in the early 21st century. It is unclear whether one or two species are represented in the fossils reported in the scientific literature. The best known species is S. aegyptiacus from Egypt, although a potential second species, S. maroccanus, has been recovered from Morocco. The contemporary spinosaurid genus Sigilmassasaurus has also been synonymized by some authors with S. aegyptiacus, though other researchers propose it to be a distinct taxon. Another possible junior synonym is Oxalaia from the Alcântara Formation in Brazil.
Irritator is a genus of spinosaurid dinosaur that lived in what is now Brazil during the Albian stage of the Early Cretaceous Period, about 113 to 110 million years ago. It is known from a nearly complete skull found in the Romualdo Formation of the Araripe Basin. Fossil dealers had acquired this skull and sold it to the State Museum of Natural History Stuttgart. In 1996, the specimen became the holotype of the type species Irritator challengeri. The genus name comes from the word "irritation", reflecting the feelings of paleontologists who found the skull had been heavily damaged and altered by the collectors. The species name is a homage to the fictional character Professor Challenger from Arthur Conan Doyle's novels.
Carcharodontosaurus from the “Carcharodon” lizard “This lizard was named for the Greek Carcharodon, the great white shark.” Named by German paleontologist Ernst Stromer von Reichenbach in 1931, is a genus of carnivorous theropod dinosaur that lived in North Africa from about 100 to 94 million years ago during the Cenomanian age of the Late Cretaceous. Two teeth of the genus, now lost, were first described from Algeria by French paleontologists Charles Depéret and Justin Savornin as Megalosaurus saharicus. A partial skeleton was collected by crews of German paleontologist Ernst Stromer during a 1914 expedition to Egypt. Stromer did not report the Egyptian find until 1931, in which he dubbed the novel genus Carcharodontosaurus, making the type species C. saharicus. Unfortunately, this skeleton was destroyed during the Second World War. In 1995 a nearly complete skull of C. saharicus, the first well-preserved specimen to be found in almost a century, was discovered in the Kem Kem Beds of Morocco; it was designated the neotype in 1996. Fossils unearthed from the Echkar Formation of northern Niger were described and named as another species, C. iguidensis, in 2007.
Suchomimus is a genus of spinosaur dinosaur that lived between 125 and 112 million years ago in what is now Niger, North Africa, during the Aptian to early Albian stages of the Early Cretaceous period. It was named and described by paleontologist Paul Sereno and colleagues in 1998, based on a partial skeleton from the Elrhaz Formation. Suchomimus's long and shallow skull, similar to that of a crocodile, earns it its generic name, while the specific name Suchomimus tenerensis alludes to the locality of its first remains, the Ténéré Desert.
Spinosauridae is a clade or family of tetanuran theropod dinosaurs comprising ten to seventeen known genera. Spinosaurid fossils have been recovered worldwide, including Africa, Europe, South America and Asia. Their remains have generally been attributed to the Early to Mid Cretaceous.
Tyrannosauroidea is a superfamily of coelurosaurian theropod dinosaurs that includes the family Tyrannosauridae as well as more basal relatives. Tyrannosauroids lived on the Laurasian supercontinent beginning in the Jurassic Period. By the end of the Cretaceous Period, tyrannosauroids were the dominant large predators in the Northern Hemisphere, culminating in the gigantic Tyrannosaurus. Fossils of tyrannosauroids have been recovered on what are now the continents of North America, Europe and Asia, with fragmentary remains possibly attributable to tyrannosaurs also known from South America and Australia.
Cristatusaurus is a genus of theropod dinosaur that lived during the Early Cretaceous Period of what is now Niger, 112 million years ago. It was a baryonychine member of the Spinosauridae, a group of large bipedal carnivores with well-built forelimbs and elongated, crocodile-like skulls. The type species Cristatusaurus lapparenti was named in 1998 by scientists Philippe Taquet and Dale Russell, on the basis of jaw bones and some vertebrae. Two claw fossils were also later assigned to Cristatusaurus. The animal's generic name, which means "crested reptile", alludes to a sagittal crest on top of its snout; while the specific name is in honor of the French paleontologist Albert-Félix de Lapparent. Cristatusaurus is known from the Albian to Aptian Elrhaz Formation, where it would have coexisted with sauropod and iguanodontian dinosaurs, other theropods, and various crocodylomorphs.
Poposaurus is an extinct genus of pseudosuchian archosaur from the Late Triassic of the southwestern and eastern United States. It belongs to the clade Poposauroidea, an unusual group of Triassic pseudosuchians that includes sail-backed, beaked, and aquatic forms. Fossils have been found in Wyoming, Utah, Arizona, Texas, and Virginia. Except for the skull, most parts of the skeleton are known. The type species, P. gracilis, was described and named by Maurice Goldsmith Mehl in 1915. A second species, P. langstoni, was originally the type species of the genus Lythrosuchus. Since it was first described, Poposaurus has been variously classified as a dinosaur, a phytosaur, and a "rauisuchian".
The scientific question of within which larger group of animals birds evolved has traditionally been called the "origin of birds". The present scientific consensus is that birds are a group of maniraptoran theropod dinosaurs that originated during the Mesozoic Era.
Lawrence M. Witmer is an American paleontologist and paleobiologist. He is a Professor of Anatomy and a Chang Ying-Chien Professor of Paleontology at the Department of Biomedical Sciences at the Heritage College of Osteopathic Medicine in Ohio University. Witmer is considered to be one of the world's foremost experts on soft-tissue anatomy of the skull in extinct animals such as dinosaurs and pterosaurs. One of Witmer's largest contributions to vertebrate paleontology was the creation of the Extant Phylogenetic Bracket approach to ancestral character state reconstruction. This methodology incorporates extensive comparative anatomy using physical and digital dissections of extant animals.
Reptiles arose about 320 million years ago during the Carboniferous period. Reptiles, in the traditional sense of the term, are defined as animals that have scales or scutes, lay land-based hard-shelled eggs, and possess ectothermic metabolisms. So defined, the group is paraphyletic, excluding endothermic animals like birds that are descended from early traditionally-defined reptiles. A definition in accordance with phylogenetic nomenclature, which rejects paraphyletic groups, includes birds while excluding mammals and their synapsid ancestors. So defined, Reptilia is identical to Sauropsida.
Oxalaia is a genus of spinosaurid dinosaur that lived in what is now the Northeast Region of Brazil during the Cenomanian stage of the Late Cretaceous period, sometime between 100.5 and 93.9 million years ago. Its only known fossils were found in 1999 on Cajual Island in the rocks of the Alcântara Formation, which is known for its abundance of fragmentary, isolated fossil specimens. The remains of Oxalaia were described in 2011 by Brazilian palaeontologist Alexander Kellner and colleagues, who assigned the specimens to a new genus containing one species, Oxalaia quilombensis. The species name refers to the Brazilian quilombo settlements. Oxalaia quilombensis is the eighth officially named theropod species from Brazil and the largest carnivorous dinosaur discovered there. It is closely related to the African genus Spinosaurus, and/or may be a junior synonym of this taxon.
Vegaviidae is an extinct family of birds of uncertain phylogenetic placement, which existed during the Late Cretaceous and possibly the Paleocene. Definitive fossils attributed to the family have only been found in Antarctica, though other fossils from the Southern Hemisphere including Chile and New Zealand may represent this group. The putative Campanian vegaviid from Canada known as Maaqwi, more likely belongs to the Procellariformes.
Halszkaraptor is a genus of waterfowl-like dromaeosaurid dinosaurs from Mongolia that lived during the Late Cretaceous period. It contains only one known species, Halszkaraptor escuilliei.
This article records new taxa of fossil archosaurs of every kind that are scheduled described during the year 2019, as well as other significant discoveries and events related to paleontology of archosaurs that are scheduled to occur in the year 2019.
Wulong is a genus of microraptorine dromaeosaurid dinosaurs from the Early Cretaceous (Aptian) Jiufotang Formation of China. The genus includes a single species, Wulong bohaiensis. The skeletal remains, which include preserved feathers, represent a juvenile.
Ceratosuchops is a genus of spinosaurid from the Early Cretaceous (Barremian) of Britain.