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.
If particular continents broke up, it would lead to significant geological, environmental, and ecological changes. Tectonic activity would increase, potentially resulting in earthquakes and volcanic eruptions. The separation could also alter ocean currents and weather patterns, impacting climates and ecosystems. Additionally, the fragmentation could affect biodiversity, as species would become isolated and evolve independently.
Pangaea broke into Gondwanaland and Laurasia.
Pangaea was a supercontinent that existed around 300 million years ago. It eventually broke apart into the continents we have today due to the movement of tectonic plates. The continents have since drifted to their current positions, shaping the Earth's geography.
yes
Glossopteris was a plant whose fossils have been found across South America, Africa, India, Antarctica, and Australia, suggesting that these continents were once connected as part of the supercontinent Gondwana. This supports the idea that these continents broke up around 180 million years ago during the Jurassic Period.
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.
The presence of Glossopteris fossils in present-day southern continents such as South America, Africa, India, Antarctica, and Australia suggests that these landmasses were once joined together in a supercontinent known as Gondwana. The breakup of Gondwana began around 180 million years ago during the Jurassic period.
This isn't the full answer sorry but The globetrotters plant
This isn't the full answer sorry but The globetrotters plant
This suggests that these continents broke up around 200 million years ago during the Mesozoic era. This breakup eventually led to the formation of the Atlantic Ocean.
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
This isn't the full answer sorry but The globetrotters plant
The trilobite fossil is found on all continents, suggesting they were once connected in a supercontinent called Pangaea about 300 million years ago. The distribution of trilobite fossils across land masses helps support the theory of continental drift, which states that continents were once joined together before drifting apart due to tectonic plate movements.
The two continents that formed when Pangaea broke apart are Laurasia in the north and Gondwana in the south. These two supercontinents eventually broke up further to form the continents we have today.
The single mass which eventually broke into the continents is referred to as Pangaea.