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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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Q: What does glossoptetsis suggest about when these particular continents broke up?
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Related questions

Which fossil occurs on the landmasses what does this suggest about when these particular continents broke up?

This isn't the full answer sorry but The globetrotters plant


What fossils occur on the most landmasses when does this suggest about when these particular continents broke up?

This isn't the full answer sorry but The globetrotters plant


Which fossil occurs on the most landmasses what does this suggest about when these particular broke up?

This isn't the full answer sorry but The globetrotters plant


Which fossil occurs on the most landmasses and what does this suggest about these particular continents broke up?

This isn't the full answer sorry but The globetrotters plant


What are the united continents called?

The single mass which eventually broke into the continents is referred to as Pangaea.


What happened when pangaea broke apart?

When Pangaea broke apart we got continents which what we have today.


What is the great landmass that broke into different continents?

Pangea


Did larger continents broke through the oceanic crust?

No, they float on it.


What was the name of the continent that then broke up into 7 continents?

Pangea


What was the name of the supercontinent before all of the continents broke up?

Pangea.


What were the two continents called when Pangaea broke into two?

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.


What is drifted to their present positions when land mass broke apart?

Continents and tectonic plates drifted to their present positions due to the process of plate tectonics. This movement is driven by the slow shifting of the Earth's lithosphere on the more fluid asthenosphere beneath it. The movement of these plates over millions of years has resulted in the present configuration of the continents and ocean basins.