This isn't the full answer sorry but The globetrotters plant
This isn't the full answer sorry but The globetrotters plant
The trilobite fossil occurs on the most landmasses. This suggests that trilobites were widespread and inhabited different parts of the world before continents broke apart, when the supercontinent Pangaea existed. Trilobites demonstrate how species can be widespread across continents that were once connected.
This isn't the full answer sorry but The globetrotters plant
The fossil that occurs on the most landmasses is the Glossopteris, a seed fern found in South America, Africa, Antarctica, India, and Australia. Its widespread distribution suggests that these continents were once part of a single supercontinent, Gondwana, which existed during the late Paleozoic era. The presence of Glossopteris on multiple continents indicates that they were connected until relatively recently in geological history, supporting the theory of continental drift and suggesting that these landmasses began to separate during the Mesozoic era.
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.
Fossils found on separated continents provide evidence that those landmasses were once connected. Similar fossils on continents that are now far apart suggest a shared history and support the idea of continental drift. Additionally, the distribution of fossils across continents can help reconstruct the movement of landmasses over geological time.
Fossils of similar plants and animals found on continents that are now widely separated suggest that these landmasses were once connected. The distribution of these fossils across different continents supports the theory of Pangaea, which posits that all current continents were once joined together in a supercontinent. This evidence helps explain how species were able to migrate and evolve across different landmasses before continental drift separated them.
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 symbols and mountain belts were important because they provided geologic evidence of past connections between continents and helped to support the theory of plate tectonics. Fossils of similar organisms found on different continents suggested that these landmasses were once connected. Mountain belts formed through tectonic collisions of continents gave clues about the movement and positions of landmasses over time. This information helped geologists determine the past positions of continents and how they have shifted over millions of years.
Continental drift can affect fossil remains by causing them to be dispersed across different continents as landmasses move. It can also result in changes to the environmental conditions where fossils are found, impacting preservation and fossil formation processes. Additionally, the movement of continents can lead to the creation of new habitats or barriers, influencing the distribution and evolution of species.
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.
Support for Wagner's hypothesis of continental drift includes evidence of fossil records, matching coastlines and geologic formations across continents, and the distribution of certain species that suggest connected landmasses in the past. These pieces of evidence helped bolster the idea that continents were once joined together and have since drifted apart.