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iAmphibians
Fossil range: Carboniferous - Recent
White's Tree Frog (Litoria caerulea)
White's Tree Frog (Litoria caerulea)
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Subphylum: Vertebrata
Class: Amphibia
Linnaeus, 1758
Subclasses and Orders

Order Temnospondyli - extinct
Subclass Lepospondyli - extinct
Subclass Lissamphibia
  Anura
  Caudata
  Gymnophiona

Amphibians (class Amphibia; from Greek αμφις "both" and βιος "life") are a taxon of animals that include all living tetrapods (four-legged vertebrates) that do not have amniotic eggs, are ectotherms, and generally spend part of their time on land. Most amphibians do not have the adaptations to an entirely terrestrial existence found in most other modern tetrapods (amniotes). There are around 6,000 described, living species of amphibians. The study of amphibians and reptiles is known as herpetology. Amphibians are able to breathe through their skin, making them very sensitive to anything they come in contact with, including human hands. When observing amphibians, one should never touch them.

History of amphibians

Amphibians developed with the characteristics of pharyngeal slits/gills, a dorsal nerve cord, a notochord, and a post-anal tail at different stages of their life. Though early tetrapods (which appeared 390 million years ago in the Devonian period) are often referred to as "amphibians", the first true amphibians (of the order Temnospondyli) appeared during the early Carboniferous period. During the late Carboniferous, Permian and Triassic periods, amphibians were extremely diverse, including many large forms, some newt and salamander-like, others resembling snakes or eels, and some large-snouted forms that were very like small (about 1.5 meter long) crocodiles (e.g. Archegosaurus). The drying out of the coal swamps during the latest Carboniferous and again at the end of the Early Permian diminished many of the environments of these Paleozoic amphibians, with the result that many types died out, and they were supplanted by reptiles. However both large and small amphibians still continued to flourish in rivers and lakes of the Late Permian, alongside the diverse therapsids that were the dominant land animals of that time. During the following, Triassic period, there were many genera with large, sometimes very flattened heads and very weak limbs; some of these, like Paracyclotosaurus, Cyclotosaurus and Mastodonsaurus were several meters in length. Apart from a few stragglers, all these large amphibians died out at the Triassic-Jurassic extinction event, and the majority of Jurassic amphibians belonged to modern groups, and would look familiar today.

The names of many of these Palaeozoic basal tetrapods and amphibians end in -gyrinus. This is from Greek γυρινος = "tadpole", although among amphibians it would be difficult to find something looking much less like a modern tadpole.

Throughout their history, amphibians have ranged in size from large forms, such as the above mentioned Triassic genera, the five foot (150cm) long Eryops of the Permian period, and the Giant Japanese and Chinese Salamanders of today, down to the tiny Brachycephalus didactylus (Brazilian Gold Frog) and Eleutherodactylus iberia (leptodactylid frog) from Cuba, with a total length of 9.6-9.8 millimeters (0.4 inches). Amphibians have mastered almost every climate on earth from the hottest deserts to the frozen arctic.

Classification

Salamandra salamandra CZ

Fire Salamander (Salamandra salamandra)

Traditionally the amphibians have included all tetrapods that are not amniotes. They are divided into three subclasses:

  • Subclass Labyrinthodontia (diverse Paleozoic and early Mesozoic group)
  • Subclass Lepospondyli (small Paleozoic group)
  • Subclass Lissamphibia (frogs, salamanders, etc)

Of these only the last includes recent species.

With the cladistic revolution, this classification has been modified, and the Labyrinthodontia discarded as being a paraphyletic group without unique defining features apart from shared primitive characteristics. Classification varies according to the preferred phylogeny of the author, and whether they use a stem or node-based classification. Generally amphibians are defined as the group that includes the common ancestors of all living amphibians (frogs, salamanders, etc) and all their descendants. This may also include extinct groups like the temnospondyls (traditionally placed in the disbanded subclass "labyrinthodontia"), and the Lepospondyls. This means that there are a now large number of basal Devonian and Carboniferous tetrapod groups, described as "amphibians" of earlier books, that are no longer placed in the formal Amphibia.

All recent amphibians are included in the Lissamphibia, which is usually considered a clade (which means that it is thought that all Lissamphibians evolved from a common ancestor apart from other extinct groups), although it has also been suggested also that salamanders arose separately from a temnospondyl-like ancestor (Carroll, 1988).

Authorities also disagree on whether Salientia is a Superorder that includes the order Anura, or whether Anura is a sub-order of the order Salientia. In effect Salientia includes all the Anura plus a single Triassic proto-frog species, Triadobatrachus massinoti. Practical considerations seem to favour using the former arrangement now.

The Lissamphibia are traditionally divided into three orders, but an extinct salamander-like group, the Albanerpetontidae, is now considered in addition to the other three groups.

  • Family Albanerpetontidae - Jurassic to Miocene (extinct)
  • Superorder Salientia
    • Triadobatrachus (Triassic)
    • Order Anura (frogs and toads) Jurassic to recent - 5,296 recent species
  • Order Caudata or Urodela (salamanders): Jurassic to recent - 555 recent species
  • Order Gymnophiona or Apoda (caecilians): Jurassic to recent - 171 recent species

Reproduction

Caecilian

Caecilian from the San Antonio zoo

For the purpose of reproduction most amphibians are bound to fresh water. A few tolerate brackish water, but there are no true seawater amphibians. Several hundred frog species in adaptive radiations (e.g., Eleutherodactylus, the Pacific Platymantines, the Australo-Papuan microhylids, and many other tropical frogs), however, do not need any water whatsoever. They reproduce via direct development, an ecological and evolutionary adaptation that has allowed them to be completely independent from free-standing water. Almost all of these frogs live in wet tropical rainforests and their eggs hatch directly into miniature versions of the adult, passing through the tadpole stage within the egg. Several species have also adapted to arid and semi-arid environments, but most of them still need water to lay their eggs. Symbiosis with single celled algae that lives in the jelly-like layer of the eggs has evolved several times. The larvae (tadpoles or polliwogs) breathe with exterior gills. After hatching, they start to transform gradually into the adult's appearance. This process is called metamorphosis. Typically, the animals then leave the water and become terrestrial adults, but there are many interesting exceptions to this general way of reproduction.

The most obvious part of the amphibian metamorphosis is the formation of four legs in order to support the body on land. But there are several other changes:

  • The gills are replaced by other respiratory organs, i.e., lungs.
  • The skin changes and develops glands to avoid dehydration.
  • The eyes develop eyelids and adapt to vision outside the water.
  • An eardrum is developed to lock the middle ear.
  • In frogs and toads, the tail disappears.

Amphibian conservation

Main article: Decline in amphibian populations
Bufo periglenes1

The Golden Toad of Monteverde, Costa Rica was among the first casualties of amphibian declines. Formerly abundant, it was last seen in 1989.

Dramatic declines in amphibian populations, including population crashes and mass localized extinction, have been noted in the past two decades from locations all over the world, and amphibian declines are thus perceived as one of the most critical threats to global biodiversity. A number of causes are believed to be involved, including habitat destruction and modification, over-exploitation, pollution, introduced species, climate change, and disease. However, many of the causes of amphibian declines are still poorly understood, and amphibian declines are currently a topic of much ongoing research.

See also

References

  • Carroll, R. 1988. Vertebrate Paleontology and Evolution. W.H. Freeman & Co., New York
  • Duellman/Trueb, Biology of Amphibians
  • Frost, Darrel R.; Taran Grant, Julián Faivovich, Raoul H. Bain, Alexander Haas, Célio F.B. Haddad, Rafael O. De Sá, Alan Channing, Mark Wilkinson, Stephen C. Donnellan, Christopher J. Raxworthy, Jonathan A. Campbell, Boris L. Blotto, Paul Moler, Robert C. Drewes, Ronald A. Nussbaum, John D. Lynch, David M. Green, Ward C. Wheeler (March 2006). "The Amphibian Tree of Life". Bulletin of the American Museum of Natural History 297: 1-291.
  • Pounds, J. Alan; Martín R. Bustamante, Luis A. Coloma, Jamie A. Consuegra, Michael P. L. Fogden, Pru N. Foster, Enrique La Marca, Karen L. Masters, Andrés Merino-Viteri, Robert Puschendorf, Santiago R. Ron, G. Arturo Sánchez-Azofeifa, Christopher J. Still and Bruce E. Young (January 2006). "Widespread amphibian extinctions from epidemic disease driven by global warming". Nature 439: 161-167. DOI:10.1038/nature04246.
  • San Mauro, Diego; Miguel Vences, Marina Alcobendas, Rafael Zardoya and Axel Meyer (May 2005). "Initial diversification of living amphibians predated the breakup of Pangaea". American Naturalist 165: 590-599.
  • Solomon Berg Martin, Biology
  • Stuart, Simon N.; Janice S. Chanson, Neil A. Cox, Bruce E. Young, Ana S. L. Rodrigues, Debra L. Fischman, Robert W. Waller (December 2004). "Status and trends of amphibian declines and extinctions worldwide". Science 306 (5702): 1783-1786. DOI:10.1126/science.1103538.

External links


Smallwikipedialogo.png This page uses content from Wikipedia. The original article was at Amphibian. The list of authors can be seen in the page history. As with Paleontology Wiki, the text of Wikipedia is available under the GNU Free Documentation License.
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