It was found in Africa, Australia, India, South America, and Antarctica. All of these regions once were connected and had similar climates.
And all of these landforms have a similar section of when they were connected
The presence of glossopteris fossils in regions that are now widely separated provided evidence for continental drift. This plant species was found in South America, Africa, India, Antarctica, and Australia, suggesting that these landmasses were once part of a single supercontinent. The distribution of glossopteris fossils supported the theory of continental drift proposed by Alfred Wegener.
continental drift
One day while scientists were exploring the sea floor, they discovered sea-floor spreading, thus proving Wegener's hypothesis to be correct.
The continental drift hypothesis was proposed by Alfred Wegener, a German meteorologist and geophysicist, in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea and had since drifted apart to their current positions.
The man who pioneered the continental drift hypothesis was Alfred Wegener. He proposed the theory in 1912, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart.
The presence of the fossil fern Glossopteris supported Wegener's hypothesis of continental drift. Glossopteris fossils were found on multiple continents that are now widely separated, indicating that these landmasses were once connected and later drifted apart.
His hypothesis of continental drift
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
Because identical fossils were found on two continents far apart, it suggested that at one time the two landmasses were joined together. In other cases of lands separated by far less distance, plants did not propagate across the divide.
Alfred wegener
Wegener used the presence of Glossopteris fossils, a type of fern-like plant, to support his idea of continental drift. These fossils were found across multiple continents that currently have widely separated coastlines, suggesting they were once part of a single landmass.
The idea known as "Continental Drift."
Because identical fossils were found on two continents far apart, it suggested that at one time the two landmasses were joined together. In other cases of lands separated by far less distance, plants did not propagate across the divide.
The presence of glossopteris fossils in regions that are now widely separated provided evidence for continental drift. This plant species was found in South America, Africa, India, Antarctica, and Australia, suggesting that these landmasses were once part of a single supercontinent. The distribution of glossopteris fossils supported the theory of continental drift proposed by Alfred Wegener.
Alfred Wegener
continental drift
Alfred Wegener