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The Isthmus of Panama is a land bridge whose appearance 3 million years ago allowed the Great American Interchange.

A land bridge, in biogeography, is an isthmus or wider land connection between otherwise separate areas, which allows terrestrial animals and plants to cross over and colonise new lands. Land bridges can be created by marine regression, in which sea levels fall, exposing shallow, previously submerged sections of continental shelf; or when new land is created by plate tectonics; or occasionally when the sea floor rises due to post-glacial rebound after an ice age.

Contents

Prominent examples

Land bridge theory

In the 19th century a number of scientists noted puzzling geological and zoological similarities between widely separated areas. To solve these problems, "…whenever geologists and paleontologists were at a loss to explain the obvious transoceanic similarities of life that they deduced from the fossil records, they sharpened their pencils and sketched land bridges between appropriate continents."[1] The concept was first proposed by Jules Marcou in Lettres sur les roches du Jura.[2]

These hypothetical land bridges included:[3]

  • Lemuria in the Indian Ocean
  • Archiboreis in the North Atlantic
  • Archatlantis from the West Indies to North Africa
  • Archhelenis from Brazil to South Africa
  • Archigalenis from Central America thru Hawaii to Northeast Asia
  • Archinotis from South America to Antarctica

All of these became obsolete with the gradual acceptance of continental drift and the development of plate tectonics by the mid-20th century.

See also

Notes

  1. ^ William R. Corliss, Mysteries Beneath the Sea, Chapter 5: "Up-and-Down Landbridges"
  2. ^ William R. Corliss, op. cit., "The basic idea is usually attributed to Jules Marcou…"
  3. ^ All examples taken from Corliss, op. cit.
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.]] A land bridge, in biogeography, is an isthmus or wider land connection between otherwise separate areas, which allows terrestrial animals and plants to cross over and colonise new lands. Land bridges can be created by marine regression, in which sea levels fall, exposing shallow, previously submerged sections of continental shelf; or when new land is created by plate tectonics; or occasionally when the sea floor rises due to post-glacial rebound after an ice age.

Contents

Prominent examples

Land bridge theory

In the 19th century a number of scientists noted puzzling geological and zoological similarities between widely separated areas. To solve these problems, "…whenever geologists and paleontologists were at a loss to explain the obvious transoceanic similarities of life that they deduced from the fossil records, they sharpened their pencils and sketched land bridges between appropriate continents."[1] The concept was first proposed by Jules Marcou in Lettres sur les roches du Jura.[2]

These hypothetical land bridges included:[3]

  • Lemuria in the Indian Ocean
  • Archiboreis in the North Atlantic
  • Archatlantis from the West Indies to North Africa
  • Archhelenis from Brazil to South Africa
  • Archigalenis from Central America through Hawaii to Northeast Asia
  • Archinotis from South America to Antarctica

All of these became obsolete with the gradual acceptance of continental drift and the development of plate tectonics by the mid-20th century.

See also

Notes

  1. ^ William R. Corliss, Mysteries Beneath the Sea, Chapter 5: "Up-and-Down Landbridges"
  2. ^ William R. Corliss, op. cit., "The basic idea is usually attributed to Jules Marcou…"
  3. ^ All examples taken from Corliss, op. cit.


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