Information about Lungfish

Lungfishes
Fossil range: Early Devonian - Recent

Scientific classification
Kingdom:Animalia
Phylum:Chordata
Subphylum:Vertebrata
Class:Sarcopterygii
Subclass:Dipnoi
Müller, 1844
Orders


See text.
Lungfish are freshwater fish belonging to the order Dipnoi. Lungfish are best-known for retaining characteristics primitive within the Osteichthyes, including the ability to breathe air, and structures primitive within Sarcopterygii, including the presence of lobed fins with a well-developed internal skeleton. Today, they live only in Africa, South America, and Australia. While vicariance would suggest this represents an ancient distribution limited to the Mesozoic supercontinent Gondwana, the fossil record suggests that advanced lungfish had a cosmopolitan freshwater distribution and that the current distribution of modern lungfish species reflects extinction of many lineages following the breakup of both Pangea and subsequently Gondwana and Laurasia.

Anatomy and morphology

All lungfish demonstrate an uninterrupted cartilaginous notochord and an extensively developed palatal dentition. Basal lungfish groups may retain marginal teeth and an ossified braincase, but derived lungfish taxa, including all modern species, show a significant reduction in marginal bones and a cartilaginous braincase. The bones of the skull roof in primitive lungfish are covered in a mineralized tissue called cosmine, but in post-devonian lungfishes, the skull roof is subdermal and the cosmine covering is lost. All modern lungfish show significant reductions and fusions of the bones of the skull roof, and the specific bones of the skull roof show no homology to the skull roof bones of actinopterygiians or tetrapods.

The dentition of lungfish is conspicuously different from that of any other vertebrate group. Odontodes on the palate and lower jaws develop in a series of rows to form a fan-shaped occlusion surface. These odontodes then wear to form a uniform crushing surface. In several groups, including the modern lepidosireniformes, these ridges have been modified to form occluding blades.

The modern lungfishes have a number of larval features, which suggest paedomorphosis. They also demonstrate the largest genome among the vertebrates.

Modern lungfish all have an elongate body with fleshy paired pectoral and pelvic fins and a single unpaired caudal fin replacing the dorsal, caudal, and anal fin of most fishes.

Ecology and life history

Behavior

African and South American lungfish are capable of surviving seasonal desiccation of habitats by burrowing into mud and estivating throughout the dry season. Changes in physiology allow the lungfish to slow its metabolism to as little as 1/60th of the normal metabolic rate, and protein waste is converted from ammonia to less-toxic urea (normally, lungfish excrete nitrogenous waste as ammonia directly into the water). Burrowing is seen in at least one group of fossil lungfish, the Gnathorhizidae. It has been proposed both that burrowing is plesiomorphic for lungfish as well as that gnathorhizids are directly ancestral to modern Lepidosireniformes, but it is possible that the similarity is simply due to convergent evolution or parallel evolution.

Taxonomic history

Taxonomy of lungfishes can be viewed in terms of taxonomic position of lungfishes within Osteichthyes and taxonomic relationships within lungfishes.

The former is well-resolved. In a cladogram of osteichthyan relationships, lungfishes clade closest with Powichthyes, and then with the Porolepiformes. Together, these taxa form the Dipnomorpha. The dipnomorpha form a sister group to the tetrapodomorpha. Together, these are known as the Rhipidistia, and form a sister group to the coelacanths.

The latter is significantly more difficult to resolve. While Devonian lungfish retain enough ossification of the endocranium to determine relationships, post-Devonian lungfish are represented entirely by skull roofs and teeth, as the rest of the skull is cartilaginous. Additionally, many of the taxa that have been identified may not be monophyletic. Current phylogenetic studies support the following relationships of major lungfish taxa:

Subclass Sarcopterygii
Order Dipnoi ,--†Family Diabolichthyidae | ,--†Family Uranolophidae | | __,--†Family Speonesydrionidae '-|-| '--†Family Dipnorhynchidae | ,--†Family Stomiahykidae '---| ___ ,--†Family Chirodipteridae | '-|--†Family Holodontidae†Family Dipteridae | __,--†Family Fleurantiidae '-| '--†Family Rhynchodipteridae '--†Family Phaneropleuridae | ,--†Family Ctenodontidae '-| ,--†Family Sagenodontidae '-|--†Family Gnathorhizidae '--Order Ceratodontiformes†family Asiatoceratodontidae†Family PtychoceratodontidaeFamily Ceratodontidae | '--†Genus Ceratodus | '--†Genus Metaceratodus '--Family Neoceratodontidae | '--†Genus Mioceratodus | '--Genus Neoceratodus - Queensland lungfish '--Order Lepidosireniformes '--Family Lepidosirenidae - South American lungfish '--Family Protopteridae - African lungfish

References

  • Ahlberg, PE, Smith, MM, and Johanson, Z, (2006). Developmental plasticity and disparity in early dipnoan (lungfish) dentitions. Evolution and Development 8(4):331-349.
  • Schultze, HP, and Chorn, J., (1997). The Permo-Herbivorus genus Sagenodus and the beginning of modern lungfish. Contributions to Zoology 61(7):9-70.

External links

Devonian is a geologic period of the Paleozoic era spanning from roughly 416 to 359 million years ago. It is named after Devon, England, where rocks from this period were first studied.
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Ceratodontidae

Genus: Neoceratodus

Species: N. forsteri

Binomial name
Neoceratodus forsteri
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Scientific classification or biological classification is a method by which biologists group and categorize species of organisms. Scientific classification also can be called scientific taxonomy, but should be distinguished from folk taxonomy, which lacks scientific basis.
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Chordata
Bateson, 1885

Typical Classes

See below

Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Vertebrata
Cuvier, 1812

Classes and Clades

See below
Vertebrates are members of the subphylum Vertebrata (within the phylum Chordata), specifically, those chordates with backbones or spinal columns.
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Sarcopterygii

Subclasses
  • Coelacanthimorpha - Coelacanths
  • Dipnoi - Lungfishes
  • Tetrapodomorpha - Tetrapods


Sarcopterygii (from Greek sarx, flesh, and pteryx
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Johannes Peter Müller (July 14, 1801, Koblenz – April 28, 1858, Berlin), was a German physiologist, comparative anatomist, and ichthyologist not only known for his discoveries but also for his ability to synthesize knowledge.
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Osteichthyes
Huxley, 1880

Classes

Actinopterygii
Sarcopterygii

Osteichthyes (IPA: /ˌɒstiːˈɪkθiːz/) are a taxonomic superclass of fish, also called
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Sarcopterygii

Subclasses
  • Coelacanthimorpha - Coelacanths
  • Dipnoi - Lungfishes
  • Tetrapodomorpha - Tetrapods


Sarcopterygii (from Greek sarx, flesh, and pteryx
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Africa is the world's second-largest and second most-populous continent, after Asia. At about 30,221,532 km² (11,668,545 sq mi) including adjacent islands, it covers 6% of the Earth's total surface area, and 20.4% of the total land area.
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South America is a continent of the Americas, situated entirely in the Western Hemisphere and mostly in the Southern Hemisphere. It is bordered on the west by the Pacific Ocean and on the north and east by the Atlantic Ocean; North America and the Caribbean Sea lie
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Anthem
Advance Australia Fair [1]


Capital Canberra

Largest city Sydney
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Allopatric speciation, also known as geographic speciation, is the phenomenon where huge biological populations are physically isolated by an extrinsic barrier and evolve intrinsic (genetic) reproductive isolation, such that if the barrier breaks down, individuals of the
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The Mesozoic Era is one of three geologic eras of the Phanerozoic eon. The division of time into eras dates back to Giovanni Arduino, in the 18th century, although his original name for the era now called the 'Mesozoic' was 'Secondary' (making the modern era the 'Tertiary').
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In geology, a supercontinent is a land mass comprising more than one continental core, or craton. The assembly of cratons and accreted terranes that form Eurasia[1] qualifies as a supercontinent today.
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Gondwana (IPA: /ɡɒnˈdwɑːnə/[1], originally Gondwanaland) included most of the landmasses in today's southern hemisphere, including Antarctica, South America, Africa, Madagascar,
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extinction is the cessation of existence of a species or group of taxa, reducing biodiversity. The moment of extinction is generally considered to be the death of the last individual of that species (although the capacity to breed and recover may have been lost before this point).
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Pangaea or Pangæa (IPA: /pænˈdʒiːə/[1], from παν, pan, meaning entire, and γαια, gaia, meaning Earth
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Laurasia (IPA: /lɔˈreɪʃiə, lɔˈreɪʃiʒə/[1]) was a supercontinent that most recently existed as a part of the split of the Pangaean supercontinent in the late
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The notochord is a flexible, rod-shaped body found in embryos of all chordates. It is composed of cells derived from the mesoderm and defines the primitive axis of the embryo.
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Teeth (singular, tooth) are structures found in the jaws (or mouths) of many vertebrates that are used to tear, scrape, and chew food. Some animals, particularly carnivores, also use teeth for hunting or defense. The roots of teeth are covered by gums.
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A taxon (plural taxa), or taxonomic unit, is a name designating an organism or group of organisms. A taxon is assigned a rank and can be placed at a particular level in a systematic hierarchy reflecting evolutionary
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Devonian is a geologic period of the Paleozoic era spanning from roughly 416 to 359 million years ago. It is named after Devon, England, where rocks from this period were first studied.
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In evolutionary biology, homology is any similarity between characters that is due to their shared ancestry. There are examples in different branches of biology. Anatomical structures that perform the same function in different biological species and evolved from the same structure
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Actinopterygii
Klein, 1885

Subclasses

Chondrostei
Neopterygii
See text for orders.
The Actinopterygii (the plural form of Actinopterygius) comprise the class of the ray-finned fishes.
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Tetrapoda
Broili, 1913

Classes
  • Amphibia
  • Aves
  • Mammalia
  • Sauropsida (Reptilia)
  • Synapsida
Tetrapods (Greek tetrapoda, Latin quadruped
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Vertebrata
Cuvier, 1812

Classes and Clades

See below
Vertebrates are members of the subphylum Vertebrata (within the phylum Chordata), specifically, those chordates with backbones or spinal columns.
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Odontodes, or dermal teeth, are hard structures found on the external surfaces of animals or near internal openings. They are comprised of a soft pulp surrounded by dentine and covered by a mineralized substance such as enamel, a structure similar to that of teeth.
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Occlusion is a term indicating that the state of something, which is normally open, is now totally closed.
  • In medicine, the term is often used to refer to blood vessels, arteries or veins which have become totally blocked to any blood flow.

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