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 fossil fern Glossopteris provided significant support for Alfred Wegener's hypothesis of continental drift. This plant, which thrived during the late Paleozoic era, was found in fossilized form across widely separated continents, including South America, Africa, Antarctica, and Australia. The presence of Glossopteris in these distinct regions suggested that these landmasses were once connected, supporting the idea that continents have moved over geological time. Its distribution helped bolster the argument for the existence of the supercontinent Gondwana.
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
Alfred Wegener used the discovery of the same fossil plant species, such as Glossopteris, found on five continents as supporting evidence for his theory of continental drift. He argued that these plants could not have spread across vast oceans, suggesting that the continents were once joined together in a supercontinent called Pangaea. This finding indicated that the continents had since drifted apart, aligning with his hypothesis about the movement of landmasses over geological time. Wegener's ideas were initially met with skepticism, but fossil evidence played a crucial role in strengthening his arguments for continental movement.
One day while scientists were exploring the sea floor, they discovered sea-floor spreading, thus proving Wegener's hypothesis to be correct.
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
The fossil fern Glossopteris provided significant support for Alfred Wegener's hypothesis of continental drift. This plant, which thrived during the late Paleozoic era, was found in fossilized form across widely separated continents, including South America, Africa, Antarctica, and Australia. The presence of Glossopteris in these distinct regions suggested that these landmasses were once connected, supporting the idea that continents have moved over geological time. Its distribution helped bolster the argument for the existence of the supercontinent Gondwana.
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
Alfred Wegener