Glossopteris is a fossil plant:-
The Glossopteridales arose around the beginning of the Permian on the great southern continent of Gondwana. These plants (which have distinctive spathulate fossil leaves with reticulate venation) went on to become the dominant elements of the southern flora through the rest of the Permian but disappeared in almost all places at the end of the Permian. The only convincing early Triassic records are leaves from Nidpur in India, but even these records are somewhat questionable owing to faulting and complex juxtapositioning of Permian and Triassic strata at Nidpur.
Glossopteris is a plant fossil that was found in multiple continents that were once part of the supercontinent Gondwana. The widespread distribution of Glossopteris across these continents suggests that they were once connected, providing evidence for the existence of Gondwana.
It was found in Africa, Australia, India, South America, and Antarctica. All of these regions once were connected and had similar climates. And all of these landforms have a similar section of when they were connected
The presence of glossopteris fossils in regions that are now widely separated provided evidence for continental drift. This plant species was found in South America, Africa, India, Antarctica, and Australia, suggesting that these landmasses were once part of a single supercontinent. The distribution of glossopteris fossils supported the theory of continental drift proposed by Alfred Wegener.
it shows that Pangaea existed. "Wegener inferred that these reptiles lived on a single landmass that has since split apart."
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.
The glossopteris was a seed fern that was shaped like a tongue. The glossopteris became extinct about 252 million years ago, at the end of the Permian era.
glossopteris
Glossopteris is a plant fossil that was found in multiple continents that were once part of the supercontinent Gondwana. The widespread distribution of Glossopteris across these continents suggests that they were once connected, providing evidence for the existence of Gondwana.
it said to be a plant animal XD
Glossopteris
The presence of the fossil fern Glossopteris supported Wegener's hypothesis of continental drift. Glossopteris fossils were found on multiple continents that are now widely separated, indicating that these landmasses were once connected and later drifted apart.
It was found in Africa, Australia, India, South America, and Antarctica. All of these regions once were connected and had similar climates. And all of these landforms have a similar section of when they were connected
Glossopteris plants lived during the Permian and Carboniferous periods, approximately 360 to 250 million years ago. These plants were dominant in the southern hemisphere when the continents were connected as part of the supercontinent Gondwana.
Glossopteris is important because it is a genus of extinct seed fern that played a significant role in the theory of continental drift. Fossils of glossopteris plants have been found on multiple continents, providing evidence to support the idea that these landmasses were once connected as part of the supercontinent Gondwana.
plant fossils (glossopteris) were found there.
The presence of glossopteris fossils in regions that are now widely separated provided evidence for continental drift. This plant species was found in South America, Africa, India, Antarctica, and Australia, suggesting that these landmasses were once part of a single supercontinent. The distribution of glossopteris fossils supported the theory of continental drift proposed by Alfred Wegener.
Antarctica would not support glossopteris growth today because it has a polar climate with cold temperatures and limited sunlight, which are not conducive to the growth of glossopteris trees that thrived in warm, temperate climates millions of years ago.