The discovery of Glossopteris supports Wegner's continental drift by sowing that the continents were once put together but drifted apart over time. This is how Glossopteris was found on 5 different continents.
Fossils of the glossopteris fern, which have been found across South America, Africa, India, Antarctica, and Australia. Fossil eveidence of a triassic land reiple lystrosaurus are also found across Africa, India, Antarctica and Australia.
Fossil, climate, and rock.
The layers of rock formations, particularly the similarity of certain geological features and fossil distributions found in Africa, South America, India, and Australia, support the Continental Drift hypothesis. For instance, the presence of identical fossilized species, such as the Mesosaurus and Glossopteris, across these continents suggests that they were once connected. Additionally, matching rock strata and mountain ranges, like the Appalachian and Caledonian mountains, further indicate that these landmasses were part of a single supercontinent before drifting apart. This geological and paleontological evidence reinforces the idea of continental movement over time.
The layers of rock and fossil evidence found in Africa, South America, India, and Australia provide crucial support for the continental drift hypothesis by demonstrating the historical connectivity of these continents. Similar rock formations and fossilized species, such as the Mesosaurus and Glossopteris, are found across these regions, indicating they were once part of a single landmass. The alignment of geological features, such as mountain ranges and coal deposits, further reinforces the idea that these continents have drifted apart from a unified supercontinent, Gondwana. This geological consistency across disparate continents is a key piece of evidence for the theory of plate tectonics.
The clincher was that the fossil record on the coastlines of both continents were identical.
meosopia
Fossils of the glossopteris fern, which have been found across South America, Africa, India, Antarctica, and Australia. Fossil eveidence of a triassic land reiple lystrosaurus are also found across Africa, India, Antarctica and Australia.
Glossopteris is a fossil plant that has been found on multiple continents, including South America, Africa, Australia, Antarctica, and India. It is an important indicator of the past connections between these landmasses when they were part of the supercontinent Gondwana.
Because at one time - millions of years ago - all the continents were joined in a giant continent called Pangea.
The fossil of the Glossopteris, a prehistoric plant, occurs on the most landmasses. Its remains have been found in South America, Africa, Antarctica, Australia, and India, providing significant evidence for the theory of continental drift. The widespread distribution of Glossopteris fossils supports the idea that these continents were once connected as part of the supercontinent Gondwana.
south America
During the Paleozoic Era, Africa was part of the supercontinent called Gondwana. Gondwana was located in the Southern Hemisphere and covered present-day continents such as Africa, South America, Antarctica, Australia, and the Indian subcontinent. Africa was situated towards the center of Gondwana during this time.
The first fossil discovered in Antarctica was a Nodosaurid Ankylosaur. It was found in 1986.
No. There are no wild flamingos in Australia today. Australia is the only continent without flamingos (apart from Antarctica). However, fossil evidence show that, from the Oligocene until the Pleistocene, Australia did have it's own species of flamingos, inhabiting Lake Eyre, they became extinct when Australia became more arid and the network of inland water bodies that supported them dried up.
I believe his first observation was the way the continents of South America and Africa "fit" together like a jigsaw puzzle (although he was not the first to realize this). He also made note of fossil discoveries in Africa which corresponded to those in South America. Finally, he began his own research which actually alligned rock formation/componants from one side of the Atlantic with the other.
Peter Barrett is credited with finding the first tetrapod fossil in Antarctica in 1967.
Glossopteris, a seed fern found in fossil records across several continents, played a crucial role in Alfred Wegener's hypothesis of continental drift. Its widespread distribution in now-separated landmasses, such as South America, Africa, Antarctica, and Australia, provided evidence that these continents were once joined. The presence of Glossopteris in these diverse locations suggested that they must have been connected in a single landmass, which Wegener named Gondwana. This fossil evidence supported his argument for the movement of continents over geological time.