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What (who) is isthmus of rhombencephalon - definition
![The closure of the Isthmus led to [[allopatric speciation]] events of marine organisms isolated on each side (blue and green). Terrestrial species also migrated between the two continents (the [[Great American Biotic Interchange]]) upon the formation of a passable land bridge.](https://commons.wikimedia.org/wiki/Special:FilePath/Isthmus of Panama (closure) - Speciation of marine organisms (w annot).png?width=200 "The closure of the Isthmus led to [[allopatric speciation]] events of marine organisms isolated on each side (blue and green). Terrestrial species also migrated between the two continents (the [[Great American Biotic Interchange]]) upon the formation of a passable land bridge.")
![American ranging]]](https://commons.wikimedia.org/wiki/Special:FilePath/Colonel Benjamin Church.jpg?width=200 "American ranging]]")
![Marquis de Boishébert - [[Charles Deschamps de Boishébert et de Raffetot]] (1753)](https://commons.wikimedia.org/wiki/Special:FilePath/Marquis de Boishébert - Charles Deschamps de Boishébert et de Raffetot (1753) McCord Museum McGill.jpg?width=200 "Marquis de Boishébert - [[Charles Deschamps de Boishébert et de Raffetot]] (1753)")
![British Gravestones from the Mi'kmaw Raid on Fort Monckton (1756) - oldest known military gravestones in the [[Maritimes]]](https://commons.wikimedia.org/wiki/Special:FilePath/Raid on Fort Monckton (1756), New Brunswick.jpg?width=200 "British Gravestones from the Mi'kmaw Raid on Fort Monckton (1756) - oldest known military gravestones in the [[Maritimes]]")
Wikipedia
The Isthmus of Panama (Spanish: Istmo de Panamá), also historically known as the Isthmus of Darien (Istmo de Darién), is the narrow strip of land that lies between the Caribbean Sea and the Pacific Ocean, linking North and South America. It contains the country of Panama and the Panama Canal. Like many isthmuses, it is a location of great geopolitical and strategic importance.
The isthmus is thought to have been finally formed around 3 million years ago, separating the Atlantic and Pacific Oceans and causing the creation of the Gulf Stream. This was first suggested in 1910 by North American paleontologist Henry Fairfield Osborn. He based the proposal on the fossil record of mammals in Central America. This conclusion provided a foundation for Alfred Wegener when he proposed the theory of continental drift in 1912.
