After Pangaea broke apart, the climate varied by region due to factors such as latitude, ocean currents, and landmass distribution. Overall, the breakup led to the development of diverse climate zones and ecosystems across the newly formed continents. These changes contributed to the evolution and distribution of plant and animal species.
When Pangaea formed around 335 million years ago during the late Paleozoic era, the climate was generally warm and humid, with vast tropical swamps and forests covering large portions of the supercontinent. Over time, as Pangaea drifted and the continents shifted, the climate gradually changed into separate climate zones.
Alfred Wegener proposed the concept of Pangaea after observing similarities in geology, fossils, and climate patterns across continents. He noticed how certain landmasses fit together like pieces of a puzzle and postulated that they were once part of a supercontinent that had since drifted apart.
During the time when Pangaea existed, the climate in the center was likely hot and arid due to its distance from large bodies of water. This central region would have experienced extreme temperature fluctuations and a lack of rainfall, leading to arid conditions.
Earth's original land mass, called Pangaea, was a supercontinent that existed about 335 million years ago. Pangaea comprised almost all of Earth's landmasses, connected in one large landmass. Over time, Pangaea broke apart due to the movement of tectonic plates, eventually leading to the continents we have today.
Plate tectonics. This is the theory that Earth's outer shell is divided into several plates that move and interact with one another, leading to processes like continental drift, earthquakes, and volcanic activity.
all of the continents broke apart
it looks like this.
Before Pangaea broke apart, it was home to a diverse range of organisms, including large reptiles like dinosaurs and various amphibians. Flora included vast forests of ferns, cycads, and conifers, which thrived in the warm, humid climate. Marine life flourished in the surrounding oceans, with numerous species of fish, ammonites, and other invertebrates. The ecosystem was characterized by a mix of terrestrial and aquatic life, reflecting both the expansive landmass and the interconnected seas.
Well the the molten layer pushed the tectonic plates apart splitting Africa to the South-east and pushing south America to the south-west when the molten layer was pushing the other plates you will see that the Continent's was looking like Today
When Pangaea formed around 335 million years ago during the late Paleozoic era, the climate was generally warm and humid, with vast tropical swamps and forests covering large portions of the supercontinent. Over time, as Pangaea drifted and the continents shifted, the climate gradually changed into separate climate zones.
Alfred Wegener proposed the concept of Pangaea after observing similarities in geology, fossils, and climate patterns across continents. He noticed how certain landmasses fit together like pieces of a puzzle and postulated that they were once part of a supercontinent that had since drifted apart.
Evolution was not the cause of the breakup of Pangaea. Pangaea broke up by a process called rifting. Upwelling in Earth's mantle started to pull the conteinent apart. As the curst thinned, it led to the formation of volcanoes, which generated new crust, helping to push the continent apart. Evolution is the process by which groups of organisms change over time. While the breakup of Pangaea undoubtedly affected the course of evolution, evolution had nothing to do with causing the breakup.
Continents are large landmasses on Earth, surrounded by water. They vary in terms of size, shape, and features, but generally have diverse landscapes including mountains, plains, deserts, and forests. Each continent has its own unique geography, climate, and indigenous flora and fauna.
During the time when Pangaea existed, the climate in the center was likely hot and arid due to its distance from large bodies of water. This central region would have experienced extreme temperature fluctuations and a lack of rainfall, leading to arid conditions.
Earth's original land mass, called Pangaea, was a supercontinent that existed about 335 million years ago. Pangaea comprised almost all of Earth's landmasses, connected in one large landmass. Over time, Pangaea broke apart due to the movement of tectonic plates, eventually leading to the continents we have today.
Pangaea was a super-continent which broke up into 10 super continents. All though we are unclear of its exact configuration Rodina predates Pangaea by 800 million years. Before that, smaller continents like Atlantica and Artica were still around. ♥:)♥
Plate tectonics. This is the theory that Earth's outer shell is divided into several plates that move and interact with one another, leading to processes like continental drift, earthquakes, and volcanic activity.