Map of Sahul and Sunda, land masses that have provided land bridges at various points throughout the PleistoceneNotable past (purple) and current (orange) land bridges on a bathymetric equirectangular projection centred on 45°E
The botanist Joseph Dalton Hooker, noting similarities of the floras of Australia, New Zealand, and southern South America in his six-volume Flora Antarctica, published between 1844 and 1859, proposed that land bridges had once existed between these land masses.
In the late 19th and early 20th centuries, vanished land bridges were an explanation for observed affinities of plants and animals in distant locations. Such scientists as Joseph Dalton Hooker noted puzzling geological, botanical, and zoological similarities between widely separated areas, and proposed land bridges between appropriate land masses that allowed species to spread between land masses. In geology, the concept was first proposed by Jules Marcou in Lettres sur les roches du Jura et leur distribution géographique dans les deux hémisphères ("Letters on the rocks of the Jura [Mountains] and their geographic distribution in the two hemispheres"), 1857–1860.
Hypothesized land bridges included:
Archatlantis from the West Indies to North Africa
Archhelenis from Brazil to South Africa
Archiboreis in the North Atlantic
Archigalenis from Central America through Hawaii to Northeast Asia
The theory of continental drift provided an alternate explanation that did not require land bridges. However the continental drift theory was not widely accepted until the development of plate tectonics in the early 1960s, which more completely explained the motion of continents over geological time.