Vertebrate - Biblioteka.sk

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Vertebrate
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Vertebrate
Temporal range:
Cambrian Stage 3Present,
518–0 Ma[1]
Diversity of vertebrates: Acipenser oxyrinchus (Actinopterygii), an African bush elephant (Tetrapoda), a tiger shark (Chondrichthyes) and a river lamprey (Agnatha).
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Superphylum: Deuterostomia
Phylum: Chordata
Clade: Olfactores
Subphylum: Vertebrata
J-B. Lamarck, 1801[2]
Infraphyla
Synonyms

Ossea Batsch, 1788[2]

Vertebrates (/ˈvɜːrtəbrɪts, -ˌbrts/)[3] are deuterostomal animals with bony or cartilaginous axial endoskeleton — known as the vertebral column, spine or backbone — around and along the spinal cord, including all fish, amphibians, reptiles, birds and mammals. The vertebrates consist of all the taxa within the subphylum Vertebrata (/ˌvɜːrtəˈbrtə/)[4] (chordates with backbones) and represent the overwhelming majority of the phylum Chordata, with currently about 69,963 species described.[5]

Vertebrates comprise groups such as the following infraphyla and classes:

Extant vertebrates vary in body lengths ranging from the frog species Paedophryne amauensis, at as little as 7.7 mm (0.30 in), to the blue whale, at up to 33 m (108 ft). Vertebrates make up less than five percent of all described animal species; the rest are described as invertebrates, an informal polyphyletic group comprising all that lack vertebral columns, which include non-vertebrate chordates such as lancelets.

The vertebrates traditionally include the hagfish, which do not have proper vertebrae due to their loss in evolution,[7] though their closest living relatives, the lampreys, do.[8] Hagfish do, however, possess a cranium. For this reason, the vertebrate subphylum is sometimes referred to as Craniata or "craniates" when discussing morphology. Molecular analysis since 1992 has suggested that hagfish are most closely related to lampreys,[9] and so also are vertebrates in a monophyletic sense. Others consider them a sister group of vertebrates in the common taxon of Craniata.[10]

Etymology

The word vertebrate derives from the Latin word vertebratus (Pliny), meaning joint of the spine.[11] A similarly derived word is vertebra, which refers to any of the irregular bones or segments of the spinal column.[12]

Anatomy and morphology

All vertebrates are built along the basic chordate body plan: a rigid axial endoskeleton (vertebral column and/or notochord) running along the length of the animal,[13] dorsal to the gut tube, with a hollow dorsal nerve cord (the neural tube, which develops into the brain and spinal cord) running more dorsal to it. The endoskeleton continues beyond the anus and often forms an elongated tail (post-anal tail).[14] All vertebrates also possess pharyngeal arches, as well as an iodine-concentrating organ called the endostyle, which develops into the thyroid in adults.

Vertebral column

Fossilized skeleton (cast) of Diplodocus carnegii, showing an extreme example of the backbone that characterizes the vertebrates.

With only one exception, the defining characteristic of all vertebrate is the vertebral column, in which the embryonic notochord found in all chordates is replaced by a segmented series of mineralized elements called vertebrae separated by fibrocartilaginous intervertebral discs, which are derived embryonically and evolutionarily from the notochord. Hagfish are the only extant vertebrate whose notochord persists and is not integrated/ replaced by the vertebral column.

A few vertebrates have secondarily lost this feature and retain the notochord into adulthood, such as the sturgeon[15] and coelacanth. Jawed vertebrates are typified by paired appendages (fins or limbs, which may be secondarily lost), but this trait is not required to qualify an animal as a vertebrate.

Gills

Gill arches bearing gills in a pike

All basal vertebrates are aquatic and breathe with gills. The gills are carried right behind the head, bordering the posterior margins of a series of openings from the pharynx to the exterior. Each gill is supported by a cartilaginous or bony gill arch.[16] The bony fish have three pairs of arches, cartilaginous fish have five to seven pairs, while the primitive jawless fish have seven. The vertebrate ancestor no doubt had more arches than this, as some of their chordate relatives have more than 50 pairs of gills.[14] In jawed vertebrates, the first gill arch pair evolved into the jointed jaws and form an additional oral cavity ahead of the pharynx. Research also suggests that the sixth branchial arch contributed to the formation of the vertebrate shoulder, which separated the head from the body.[17]

In amphibians and some primitive bony fishes, the larvae bear external gills, branching off from the gill arches.[18] These are reduced in adulthood, their function taken over by the gills proper in fishes and by lungs in most amphibians. Some amphibians retain the external larval gills in adulthood, the complex internal gill system as seen in fish apparently being irrevocably lost very early in the evolution of tetrapods.[19]

While the more derived vertebrates lack gills, the gill arches form during fetal development, and form the basis of essential structures such as jaws, the thyroid gland, the larynx, the columella (corresponding to the stapes in mammals) and, in mammals, the malleus and incus.[14]

Central nervous system

The central nervous system of vertebrates is based on the hollow dorsal nerve cord running along the dorsal aspect of the notochord. Of particular importance and unique to vertebrates is the presence of neural crest cells, which are progenitor cells critical to coordinating the functions of cellular components.[20] Neural crest cells migrate through the body from the dorsal nerve cord during development, and initiate the formation of neuronal ganglia and structures such as the jaws and skull.[21][22][23] The peripheral nervous system forms when neural crest cells branch out laterally from the dorsal nerve cord and migrate together with the mesodermal somites to innervate the various different structures that develop in the body.

The vertebrates are the only chordate group with neural cephalization, and their neural functions are centralized towards a series of vesicular enlargements in the head, which give rise to a brain. A slight swelling of the anterior end of the nerve cord is found in invertebrate chordates such as lancelets (a sister subphylum known as the cephalochordates), though it lacks eyes and other complex special sense organs comparable to those of vertebrates. Other chordates do not show any trends towards cephalization.[14]

The rostral end of the neural tube is expanded by a thickening of the walls and expansion of the central canal of spinal cord into three primary brain vesicles: the prosencephalon (forebrain), mesencephalon (midbrain) and rhombencephalon (hindbrain), which are further differentiated in the various vertebrate groups.[24] Two laterally placed retinas and optical nerves form around outgrowths from the midbrain, except in hagfish, though this may be a secondary loss.[25][26] The forebrain is more well-developed in most tetrapods and subdivided into the telencephalon and diencephalon, while the midbrain dominates in many fish and some salamanders. Vesicles of the brain are usually bilaterally symmetrical, giving rise to the paired cerebral hemispheres in mammals.[24]

The resulting anatomy of the central nervous system with a single hollow nerve cord dorsal to the gut tube, headed by a series of (typically paired) brain vesicles, is unique to vertebrates. Other invertebrates with well-developed central nervous systems such as arthropods and cephalopods, have a ventral nerve cord made of segmental ganglia on the opposite side of the gut tube, with a split brain stem circumventing the foregut around each side to form a brain on the dorsal side of the mouth.[14]

Another distinct neural feature of vertebrates is the axonal/dendritic myelination in both central (via oligodendrocytes) and peripheral nerves (via neurolemmocytes). Although myelin insulation is not unique to vertebrates — many annelids and arthropods also have myelin sheath formed by glia cells, with the Kuruma shrimp having twice the conduction velocity of any vertebrates — vertebrate myelination is annular and non-fenestrated, and the combination of myelination and encephalization have given vertebrates a unique advantage in developing higher neural functions such as complex motor coordination and cognition. It also allows vertebrates to evolve larger sizes while still maintaining considerable body reactivity, speed and agility (in contrast, invertebrates typically become sensorily slower and motorically clumsier with larger sizes), which are crucial for the eventual adaptive success of vertebrates in seizing dominant niches of higher trophic levels in both terrestrial and aquatic ecosystems.

Molecular signatures

In addition to the morphological characteristics used to define vertebrates (i.e. the presence of a notochord, the development of a vertebral column from the notochord, a dorsal nerve cord, pharyngeal gills, a post-anal tail, etc.), molecular markers known as conserved signature indels (CSIs) in protein sequences have been identified and provide distinguishing criteria for the subphylum Vertebrata.[27] Specifically, 5 CSIs in the following proteins: protein synthesis elongation factor-2 (EF-2), eukaryotic translation initiation factor 3 (eIF3), adenosine kinase (AdK) and a protein related to ubiquitin carboxyl-terminal hydrolase are exclusively shared by all vertebrates and reliably distinguish them from all other metazoan.[27] The CSIs in these protein sequences are predicted to have important functionality in vertebrates.

A specific relationship between Vertebrates and Tunicates is also strongly supported by two CSIs found in the proteins Rrp44 (associated with exosome complex) and serine palmitoyltransferase, that are exclusively shared by species from these two subphyla but not Cephalochordates, indicating Vertebrates are more closely related to Tunicates than Cephalochordates.[27]

Evolutionary history

External relationships

Originally, the "Notochordata hypothesis" suggested that the Cephalochordata is the sister taxon to Craniata (Vertebrata). This group, called the Notochordata, was placed as sister group to the Tunicata (Urochordata). Although this was once the leading hypothesis,[28] studies since 2006 analyzing large sequencing datasets strongly support Olfactores (tunicates + vertebrates) as a monophyletic clade,[29][30][27] and the placement of Cephalochordata as sister-group to Olfactores (known as the "Olfactores hypothesis"). As chordates, they all share the presence of a notochord, at least during a stage of their life cycle.

The following cladogram summarizes the systematic relationships between the Olfactores (vertebrates and tunicates) and the Cephalochordata.

 Chordata 
 Cephalochordata 

 Amphioxiformes (lancelets) 

Olfactores

 Tunicata/Urochordata (sea squirts, salps, larvaceans

 Craniata 

 Vertebrata 

First vertebrates

The early vertebrate Haikouichthys

Vertebrates originated during the Cambrian explosion, which saw a rise in organism diversity. The earliest known vertebrates belongs to the Chengjiang biota[31] and lived about 518 million years ago.[1] These include Haikouichthys, Myllokunmingia,[31] Zhongjianichthys,[32] and probably Haikouella.[33] Unlike the other fauna that dominated the Cambrian, these groups had the basic vertebrate body plan: a notochord, rudimentary vertebrae, and a well-defined head and tail.[34] All of these early vertebrates lacked jaws in the common sense and relied on filter feeding close to the seabed.[35][page needed] A vertebrate group of uncertain phylogeny, small eel-like conodonts, are known from microfossils of their paired tooth segments from the late Cambrian to the end of the Triassic.[36]

From fish to amphibians

Acanthostega, a fish-like early labyrinthodont.

The first jawed vertebrates may have appeared in the late Ordovician (~445 mya) and became common in the Devonian period, often known as the "Age of Fishes".[37] The two groups of bony fishes, the actinopterygii and sarcopterygii, evolved and became common.[38] The Devonian also saw the demise of virtually all jawless fishes save for lampreys and hagfish, as well as the Placodermi, a group of armoured fish that dominated the entirety of that period since the late Silurian as well as the eurypterids, dominant animals of the preceding Silurian, and the anomalocarids. By the middle of the Devonian, several droughts, anoxic events and oceanic competition lead a lineage of sarcopterygii to leave water, eventually establishing themselves as terrestrial tetrapods in the succeeding Carboniferous.

Mesozoic vertebrates

Amniotes branched from amphibious tetrapods early in the Carboniferous period. The synapsid amniotes were dominant during the late Paleozoic, the Permian, while diapsid amniotes became dominant during the Mesozoic. In the sea, the teleosts and sharks became dominant. Mesothermic synapsids called cynodonts gave rise to endothermic mammals and diapsids called dinosaurs eventually gave rise to endothermic birds, both in the Jurassic.[39] After all dinosaurs except birds went extinct by the end of the Cretaceous, birds and mammals diversified and filled their niches.

After the Mesozoic

The Cenozoic world saw great diversification of bony fishes, amphibians, reptiles, birds and mammals.[40][41]

Over half of all living vertebrate species (about 32,000 species) are fish (non-tetrapod craniates), a diverse set of lineages that inhabit all the world's aquatic ecosystems, from snow minnows (Cypriniformes) in Himalayan lakes at elevations over 4,600 metres (15,100 feet) to flatfishes (order Pleuronectiformes) in the Challenger Deep, the deepest ocean trench at about 11,000 metres (36,000 feet). Many fish varieties are the main predators in most of the world's freshwater and marine water bodies . The rest of the vertebrate species are tetrapods, a single lineage that includes amphibians (with roughly 7,000 species); mammals (with approximately 5,500 species); and reptiles and birds (with about 20,000 species divided evenly between the two classes). Tetrapods comprise the dominant megafauna of most terrestrial environments and also include many partially or fully aquatic groups (e.g., sea snakes, penguins, cetaceans).

Classification

There are several ways of classifying animals. Evolutionary systematics relies on anatomy, physiology and evolutionary history, which is determined through similarities in anatomy and, if possible, the genetics of organisms. Phylogenetic classification is based solely on phylogeny.[42] Evolutionary systematics gives an overview; phylogenetic systematics gives detail. The two systems are thus complementary rather than opposed.[43]

Traditional classification

Traditional spindle diagram of the evolution of the vertebrates at class level

Conventional classification has living vertebrates grouped into seven classes based on traditional interpretations of gross anatomical and physiological traits. This classification is the one most commonly encountered in school textbooks, overviews, non-specialist, and popular works. The extant vertebrates are:[14]

In addition to these, there are two classes of extinct armoured fishes, the Placodermi and the Acanthodii, both considered paraphyletic.

Other ways of classifying the vertebrates have been devised, particularly with emphasis on the phylogeny of early amphibians and reptiles. An example based on Janvier (1981, 1997), Shu et al. (2003), and Benton (2004)[44] is given here († = extinct):

Diversity of various groups of vertebrates through the geologic ages. The width of the bubbles signifies the diversity (number of families).

While this traditional classification is orderly, most of the groups are paraphyletic, i.e. do not contain all descendants of the class's common ancestor.[44] For instance, descendants of the first reptiles include modern reptiles, mammals and birds; the agnathans have given rise to the jawed vertebrates; the bony fishes have given rise to the land vertebrates; the traditional "amphibians" have given rise to the reptiles (traditionally including the synapsids or mammal-like "reptiles"), which in turn have given rise to the mammals and birds. Most scientists working with vertebrates use a classification based purely on phylogeny,[45] organized by their known evolutionary history and sometimes disregarding the conventional interpretations of their anatomy and physiology.

Phylogenetic relationships

In phylogenetic taxonomy, the relationships between animals are not typically divided into ranks but illustrated as a nested "family tree" known as a phylogenetic tree. The cladogram below is based on studies compiled by Philippe Janvier and others for the Tree of Life Web Project and Delsuc et al.,[46][47] and complemented (based on[48],[49] and [50]). A dagger (†) denotes an extinct clade, whereas all other clades have living descendants.

The galeaspid Nochelaspis maeandrine from the Devonian period
The placoderm Dunkleosteus terrelli from the Devonian period
The acanthodian fish Diplacanthus acus from the Devonian period
The early ray-fin Cheirolepis canadensis from the Devonian period
The tetrapodomorph Tiktaalik roseae from the Devonian period
The early tetrapod Seymouria from the Permian period
The synapsid "mammal-like reptile" Dimetrodon limbatus from the Permian period
The bird-like dinosaur Archaeopteryx lithographica from the Jurassic period
Vertebrata/

Euconodonta

Myllokunmingiida

 

Pteraspidomorphi

Thelodonti

Anaspida

Galeaspida

Zdroj:https://en.wikipedia.org?pojem=Vertebrate
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