The presant Antarctica would be to cold for plants to grow. Coal, which is plants compressed over million of years under heat and pressure could not be created without having plants (grow in warmth), and coal could not form without heat compressing it.
There are fossils of tropical plants there.
Plant fossils and coal seams could only have formed if Antarctic had once been warmer (further north).
ther was alot of vegetation
Plant fossils found in Antarctica suggest that the continent was once covered in vegetation, indicating a warmer climate. Coal beds in Antarctica further support this idea, as they are formed from the remains of ancient plant material that grew in a more temperate environment. These findings provide evidence that Antarctica experienced periods of warmer temperatures in the past.
plant fossils (glossopteris) were found there.
If you go to google images and search Pangaea you will see that scientist guess that Antarctica was close to the equator.
Tropical plant fossils found in Antarctica indicate that the continent once had a much warmer climate, supporting lush vegetation. During the Mesozoic Era, particularly in the Late Cretaceous period, Antarctica was situated closer to the equator and experienced a subtropical climate. Fossils of ferns, cycads, and other tropical plants provide evidence of this prehistoric environment, highlighting significant shifts in global climate and continental positions over millions of years. These findings help scientists understand past climate changes and the evolution of ecosystems.
No.
When liquid, sea water is warmer than ice and more conducive to plant growth.
The first fossils found in Antarctica were discovered in the Transantarctic Mountains in 1909 by geologist Griffith Taylor. These were plant fossils dating back to the Permian period, around 250 million years ago.
a plant that is a fossil
Yes, fossils and rocks support the hypothesis of continental drift. Matching plant and animal fossils found on different continents suggest they were once part of the same landmass. Rocks with similar ages and compositions found across continents also provide evidence for the movement of these landmasses over time.