Information about Megalodon

Megalodon
Fossil range: Miocene - Pleistocene
Enlarge picture
Megalodon tooth with 2 great white shark teeth

Megalodon tooth with 2 great white shark teeth
Conservation status
Extinct (fossil)
Scientific classification
Kingdom:Animalia
Phylum:Chordata
Class:Chondrichthyes
Subclass:Elasmobranchii
Order:Lamniformes
Family:Lamnidae
Genus:Carcharodon
Species:C. megalodon
Binomial name
Carcharodon megalodon
Agassiz, 1843


Carcharodon megalodon (or Carcharocles megalodon), (from ancient Greek μέγας = "big" + 'οδούς (genitive 'οδόντος) = "tooth") was a giant prehistoric shark that probably lived between about 20 to 2 million years ago. It is the biggest known carnivorous fish to have ever lived. It is often widely referred to as "The Megalodon", or "Megatooth Shark".

Known physiology

C. megalodon is known principally from fossil teeth and a few fossilized vertebral centra. As with all other sharks, the megalodon skeleton was formed of cartilage and not bone, resulting in the poor skeletal fossil record. However, the shark's large teeth have survived the ages. The teeth are in many ways similar to great white shark teeth but are much larger and can measure up to more than 18 cm (7 inch) long in slant.



Recent studies cited by Roesch (see external links below) suggest megalodon was a "close relative" of the great white shark. However, a growing number of researchers dispute this close great white shark–megalodon relationship, instead citing convergent evolution as the reason for the dental similarity. Nevertheless, it is extrapolations from the tooth size of C. megalodon to modern sharks that provide us with our conceptions about what this ancient super-predator was like.

Estimating the maximum size of megalodon is a highly controversial subject. However, three shark experts, M. D. Gottfried, Leonard Compagno and S.C. Bowman, have tried to solve this issue by developing a special method for measuring the size of sharks (including megalodon) with much greater accuracy. By using this new method, the maximum size of this creature has been calculated to be at 15.9 m (52.1 feet) long and the body mass of about 48 tons. But this calculation is based on a 168 mm (6.61 inch) long upper anterior tooth, which is not the biggest specimen found. So these bigger megalodon teeth indicate that this creature probably could grow more than 16 m (52.5 feet) long.

A very old jaw reconstruction (developed by Professor Bashford Dean in 1909) of this shark suggests a size of about 30 m (100 ft) but that jaw reconstruction is now considered to be inaccurate.

Assuming similar metabolic-weight ratios as the great white shark, it is estimated that a large C. megalodon would need to eat about one-fiftieth of its weight of food on average per day. From our knowledge of the food chain during megalodon's existence, it is generally believed that this shark's diet consisted mostly of whales, along with large fish and primitive pinnipeds and sirenians.

Taxonomic dispute

Enlarge picture
Size comparison between Megalodon and diver.
There is some disagreement as to how megalodon should be classified in taxonomy.
  • The older view (more favored by marine biologists) is that megalodon should be classified in the Carcharodon genus with the great white shark, though this has generated debate whether megalodon is a direct ancestor of the great white shark or whether the two species share a common ancestor.
  • Around 1923, the genus, Carcharocles, was proposed to classify the very similar shark Carcharodon auriculatus. Many paleontologists are now favouring Carcharocles for megalodon as well.[1] Carcharocles proponents give C. megalodon's likely ancestor as Otodus obliquus from the Eocene epoch, and the ancestor of the great white shark not megalodon but Isurus hastalis, the "broad tooth mako".

Extinction hypotheses

Enlarge picture
Megalodon and fossil shark teeth
One hypothesis is that the adult C. megalodon fed largely on whales and became extinct as the polar seas became too cold for sharks, allowing whales to swim out of the range of C. megalodon via migration. Other explanations are simpler, suggesting that any prolonged disturbance of the foodchain would wipe out a predator with such massive metabolic requirements. Some cryptozoologists suggest the shark might have died out more recently, or might even still be alive; see "Relict" below. The fossil teeth of the animal are often found in areas that had shallow seas, such as near Bakersfield in California. C. megalodon was probably a specialist that fed mostly on baleen whales in shallow waters. Since the time of its extinction there have been few such shallows supporting constant, large whale populations, and the loss of such habitats caused the animal to gradually become extinct, as the species could no longer find enough food to sustain itself. The process would have been gradual, leading to fewer C. megalodon individuals, more genetic drift and increasingly isolated populations.

The shark also faced competition from the Killer Whale (or Orca) which evolved less than five million years ago. Populations of "transient" Killer Whales exploit sea mammals, and with pack behavior and high intelligence the Orca would have crowded the shark out of the same declining food source. Once that took place, the shark's huge adult size was of no advantage and in fact meant starvation. The large size of the shark meant it probably hunted alone. However, it must be emphasized that only a handful of fossils worldwide can be attributed to early killer whales; while a tempting idea, it is highly speculative.

Relict

Enlarge picture
Carcharodontosaurus tooth from the Sahara Desert with a megalodon tooth


While most mainstream experts contend that available evidence suggests that C. megalodon is extinct, the idea of a relict population seems to have seized the public imagination[2][3], but evidence supporting such ideas is generally seen as both scant and ambiguous.

C. megalodon teeth have been discovered that some argue date as recently as 10,000 to 15,000 years ago. This claim is based on the discovery of two teeth by the HMS Challenger scientific expedition (these teeth were dated by estimating the amount of time it took for manganese to accumulate on them, although it is quite possible the teeth were fossilized before being encrusted). Problems with this dating method include the simple fact that deposition of manganese oxide on the seafloor is not constant, and can only serve as a minimum age. In all likelihood, these teeth are probably much older.

Others have countered that these recent estimates for these teeth are inaccurate, and "claims of post-Pliocene C. megalodon ... are erroneous", being based on outdated testing and methodology. [4] Research has suggested that megalodons were probably coastal sharks, and that deep-sea survival is extremely unlikely.

In fact, it must be emphasized that there are extremely few records of C. megalodon after the early Pliocene. No conclusive Pleistocene records of C. megalodon have ever been demonstrated. Interestingly, early Pliocene occurrences of C. megalodon are astonishingly rare, and only one late Pliocene record (a single, broken tooth from the San Diego Formation at la Joya, Baja California) exists in the literature. This is very possible an anomalous occurrence (e.g. it may have been reworked from older sediments) , and for all intents and purposes it appears that C. megalodon went extinct during the Pliocene.

Some relatively recent reports of large shark-like creatures have been interpreted as surviving C. megalodon, but such reports are usually considered misidentification of basking sharks, whale sharks or Greenland sharks. One well-known example was reported by writer Zane Grey. It is possible, but unlikely, that some of these sightings might be due to abnormally large great white sharks.

References

1. ^ [1]
2. ^ [2]
3. ^ [3]
4. ^ [4]

External links

The Miocene Epoch is a period of time that extends from about 23.03 to 5.332 million years before the present. As with other older geologic periods, the rock beds that define the start and end are well identified but the exact dates of the start and end of the period are uncertain.
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Pleistocene epoch (IPA: /'plaɪstəsi:n/) on the geologic timescale is the period from 1,808,000 to 11,550 years BP. The Pleistocene epoch had been intended to cover the world's recent period of repeated glaciations.
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conservation status of a species is an indicator of the likelihood of that species continuing to survive either in the present day or the future. Many factors are taken into account when assessing the conservation status of a species: not simply the number remaining, but the
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For other uses of the term, see Fossil (disambiguation)


FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
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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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Chondrichthyes
Huxley, 1880

Subclasses and Orders

See text.

The Chondrichthyes or cartilaginous fishes are jawed fish with paired fins, paired nostrils, scales, two-chambered hearts, and skeletons made of cartilage rather than bone.
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Elasmobranchii
Bonaparte, 1838

Superorders

Batoidea (rays and skates)
Selachimorpha (sharks)

Elasmobranchii is the subclass of cartilaginous fish that includes skates, rays (batoidea), and sharks (selachii).
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Lamniformes
Berg, 1958

Families
See text for families, genera and species

Lamniformes is an order of sharks, also known as mackerel sharks (which may also be used to refer to the sub-group of Lamniformes, Lamnidae).
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Lamnidae

Genera
See text for genera and species.

Lamnidae is a family of sharks, commonly known as mackerel sharks or white sharks. They are large, fast-swimming sharks, found in oceans worldwide.
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Lamnidae

Genera
See text for genera and species.

Lamnidae is a family of sharks, commonly known as mackerel sharks or white sharks. They are large, fast-swimming sharks, found in oceans worldwide.
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binomial nomenclature is the formal system of naming species. The system is also called binominal nomenclature (particularly in zoological circles), binary nomenclature (particularly in botanical circles), or the binomial classification system.
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Jean Louis Rodolphe Agassiz (May 28 1807—December 14 1873) was a Swiss-American zoologist, glaciologist, and geologist, the husband of educator Elizabeth Cabot Cary Agassiz, and one of the first world-class American scientists.
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In grammar, the genitive case or possessive case (also called the second case) is the case that marks a noun as being the possessor of another noun.
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Prehistory (Latin, præ = before Greek, ιστορία = history) is a term often used to describe the period before written history. Paul Tournal originally coined the term Pré-historique
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SHARK

General
Vincent Rijmen, Joan Daemen, Bart Preneel, Antoon Bosselaers, Erik De Win
1996

KHAZAD, Rijndael

Cipher detail
Key size(s):| 128 bits

Block size(s):| 64 bits
Substitution-permutation network
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In cryptography,
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For other uses of the term, see Fossil (disambiguation)


FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
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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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The Vertebral Column (singular: vertebra) are the individual irregular bones that make up the spinal column (aka ischis) — a flexuous and flexible column.
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skeleton or skeletal system is the biological system providing physical support in living organisms. (By extension, non-biological outline structures such as gantries or buildings may also acquire skeletons.
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Cartilage is a type of dense connective tissue. It is composed of collagen fibers and/or elastin fibers, and can supply smooth surfaces for the movement of articulating bones.
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Bones are rigid organs that form part of the endoskeleton of vertebrates. They function to move, support, and protect the various organs of the body, produce red and white blood cells and store minerals.
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Carcharodon
Smith, 1838

Species: C. carcharias

Binomial name
Carcharodon carcharias
(Linnaeus, 1758)


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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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In evolutionary biology, convergent evolution is the process whereby organisms not closely related (not monophyletic), independently evolve similar traits as a result of having to adapt to similar environments or ecological niches[1].
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Leonard J. V. Compagno is an international authority on shark taxonomy and the author of many scientific papers and books on the subject, best known of which is his 1984 catalogue of shark species produced for the Food and Agriculture Organization (FAO) of the United Nations.
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Bashford Dean, (1867- December 1928) was an American zoologist, specializing in ichthyology, and at the same time an expert in medieval armor. He is the only person to have held concurrent positions at the American Museum of Natural History and the Metropolitan Museum of Art,
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