Fossil distribution supports the theory of continental drift by showing similar species of plants and animals that lived on different continents that are now separated by oceans. This suggests that these continents were once joined together and over time drifted apart to their current positions. The presence of identical fossils on continents that are now separated is evidence that they were once part of the same landmass.
The fossil of Mesosaurus, a small aquatic reptile, was found in both South America and Africa. Its presence on different continents was used as evidence to support the theory of continental drift, as it suggested that the continents were once connected and later drifted apart.
Scientists use evidence such as matching fossil records, rock formations, and geological structures across continents, as well as the fit of the continents themselves, to support the theory of continental drift. Additionally, studies of oceanic crust age and magnetic patterns on the seafloor provide further evidence for plate tectonics and continental movement.
Evidence of ancient climates, such as glacial deposits in regions that are now near the equator, support continental drift theory because they suggest that these regions were once located at higher latitudes where glaciers were common. This is consistent with the idea that continents were once joined together in different configurations and have since drifted to their current positions. Additionally, similarities in fossil distributions and rock formations across continents also support the theory of continental drift.
Alfred Wegener used several lines of evidence to support his theory of continental drift, including the jigsaw-like fit of the continents, similarities in rock formations and fossil remains across continents, and the matching geological features along coastlines of different continents, such as mountain ranges and ancient glacial deposits.
Alfred Wegener used evidence such as the fit of the continents, matching geological formations across continents, identical fossil species found on different continents, and similarities in rock types and mountain ranges as support for his theory of continental drift.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
mesosaurus
The fossil of Mesosaurus, a small aquatic reptile, was found in both South America and Africa. Its presence on different continents was used as evidence to support the theory of continental drift, as it suggested that the continents were once connected and later drifted apart.
It is generally thought to support the Theory of Evolution.
1 mesosaur 2 cygnonathus 3 glossopteris 4 lystrosaurus
The fossil that was found on different continents and used to support the theory of continental drift is the Mesosaurus. This extinct freshwater reptile had limited swimming abilities, making it unlikely that it could have crossed vast oceans. Its distribution on both sides of the Atlantic Ocean provided evidence of land connections that later formed the basis for the theory of continental drift.
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.
There was a lot of fossils that were found but the most interesting one is the plant called Glossopteris, it was the only seed-fern plant fossil found.
yes
they couldn't agree on how it separated or what made it separate.
Scientists use evidence such as matching fossil records, rock formations, and geological structures across continents, as well as the fit of the continents themselves, to support the theory of continental drift. Additionally, studies of oceanic crust age and magnetic patterns on the seafloor provide further evidence for plate tectonics and continental movement.
Four pieces of evidence used by Alfred Wegener to support his theory of continental drift were the fit of the continents, matching geological formations across continents, similar fossil distributions, and glacial evidence in tropical regions.