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.
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.
Almost all monotreme fossils have been found in Australia. An exception is the fossil of a platypus-like creature named Monotrematus sudamericanum found in Argentina, within a Patagonian rock formation.
Fossil symbols were helpful in deciding where to move the continents because they provided evidence of past connections between landmasses. Similar fossils found on continents that are now far apart suggest that they were once joined together. By using fossil evidence, scientists could determine the past positions of continents and reconstruct ancient supercontinents like Pangaea.
Ferns and their fossil remains have been found on every continent
Glossopteris is a plant fossil that was found in multiple continents that were once part of the supercontinent Gondwana. The widespread distribution of Glossopteris across these continents suggests that they were once connected, providing evidence for the existence of Gondwana.
Wegener's clues for the theory of continental drift included the fit of the continents like a jigsaw puzzle, matching rock formations and mountain ranges across continents, and similarities in plant and animal fossils found on different continents. These clues provided evidence for the movement of the continents over time.
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.
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.
The fossils of animals were found the three different continents, but no animal could've swam that far across the salt water, so there had to be another way. Also, the plant fossil glossopteris was discovered in Antarctica, where no plants could live.
Yes, because he found fossils from a fresh water lizard, in two different continents separated by salt water.
True
mesosaurus
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.
Fossil evidence: Similar fossils of ancient plants and animals have been found on continents that are now widely separated, suggesting they were once connected. Rock formation: Matching rock formations and mountain ranges have been found on different continents, implying they were once part of the same landmass. Climate indicators: Evidence such as glacial deposits and coal beds found in regions that don't have similar climates today support the idea that continents were once positioned differently.
Fossil evidence supporting Wegener's hypothesis of continental drift included identical fossils found on separate continents, showing that these landmasses were once connected. This supported the idea that continents had drifted apart over time. Additionally, the presence of ancient glacial deposits in regions that are now too warm for glaciers to form suggested that these areas were once located closer to the South Pole.
Almost all monotreme fossils have been found in Australia. An exception is the fossil of a platypus-like creature named Monotrematus sudamericanum found in Argentina, within a Patagonian rock formation.
Fossil symbols were helpful in deciding where to move the continents because they provided evidence of past connections between landmasses. Similar fossils found on continents that are now far apart suggest that they were once joined together. By using fossil evidence, scientists could determine the past positions of continents and reconstruct ancient supercontinents like Pangaea.