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.
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The theory of plate tectonics suggests that the Earth's continents were once connected as a single landmass called Pangea. Over millions of years, the landmass broke apart and drifted to their current positions. This process continues today, with continents still slowly moving.
A long long time ago, maybe about 1,000,000 years ago, the mantel which is under the earth's crust (and we're standing on the earth's crust) was just like the earth's crust. But now it is hot melted rock. Over the years the mantel gets hotter. The Mantel gets so hot that it melts through the continents and separates them even more. Answer Plate Tectonics. The earths crust is floating on the molten magma which is what the centre of the Earth is made of. There are currents in the magma which tore the original single land mass (Pangea) apart and dragged the pieces apart. The pieces, called plates, are still drifting. Sometimes they crash into each other like India and Asia.
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.
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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.
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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.
Pangea