Petrified tree's in the standing position, clam shells on mt. Everest, coal in Antarctica. The most likely explanation would be a world wide flood that happened some time ago caused the planet to undergo a magnificent change in climate and landmass, causing erosion and incredible pressure on plants and animals creating the coal and oil we use today.
Fossils of warm-weather plants found in Antarctica are typically related to the region's ancient climate, which was significantly warmer than it is today. These fossils, including remains of trees like beech and various types of ferns, suggest that Antarctica once had a temperate climate that supported diverse ecosystems. The presence of such fossils helps scientists understand past climate changes and the evolutionary history of plant life in response to shifting environmental conditions.
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.
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.
Fossils of plants found in Greenland suggest that it had a warmer climate in the past when those plants existed. This provides evidence that Greenland was once covered in forests and supported a diverse range of plant life. The fossils also offer insights into the history of the Earth's climate and environmental conditions.
Yes, Antarctica has experienced warmer periods in its geological history. Around 40-50 million years ago, Antarctica was covered in forests and had a climate suitable for plant and animal life. This warmer period is known as the Eocene epoch.
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 (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.
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.
Fossils of warm-weather plants found in Antarctica are typically related to the region's ancient climate, which was significantly warmer than it is today. These fossils, including remains of trees like beech and various types of ferns, suggest that Antarctica once had a temperate climate that supported diverse ecosystems. The presence of such fossils helps scientists understand past climate changes and the evolutionary history of plant life in response to shifting environmental conditions.
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