What is the continental drift theory and what is Pangaea?
Table of Contents
What is the continental drift theory and what is Pangaea?
The mechanism for the breakup of Pangea is now explained in terms of plate tectonics rather than Wegener’s outmoded concept of continental drift, which simply stated that Earth’s continents were once joined together into the supercontinent Pangea that lasted for most of geologic time.
How did continental drift affect Pangea?
According to the continental drift theory, the supercontinent Pangaea began to break up about 225-200 million years ago, eventually fragmenting into the continents as we know them today.
Where does continental drift take place?
Seafloor spreading is most dynamic along giant underwater mountain ranges known as mid-ocean ridges. As the seafloor grows wider, the continents on opposite sides of the ridge move away from each other. The North American and Eurasian tectonic plates, for example, are separated by the Mid-Atlantic Ridge.
How was Pangea formed?
Finally, about 320 million years ago, there was a major collision, geologically speaking, “when Gondwana, Laurussia, and intervening terranes collided to form the Pangea supercontinent,” according to the chapter, written by Earth scientists Trond Torsvik, Mathew Domeier and Robin Cocks.
How were continents formed from Pangaea?
In 1912, German scientist Alfred Wegener proposed a theory he called continental drift. According to Wegener’s theory, Earth’s continents once formed a single, giant landmass, which he called Pangaea. Over millions of years, Pangaea slowly broke apart, eventually forming the continents as they are today.
How did Pangea affect life on Earth?
As Pangea formed, the extent of shallow water habitats declined, and land barriers inhibited cold polar waters from circulating into the tropics. This is thought to have reduced dissolved oxygen levels in the warm water habitats that remained and contributed to the 95 percent reduction of diversity in marine species.
How do we know Pangea existed?
The rock formations of eastern North America, Western Europe, and northwestern Africa were later found to have a common origin, and they overlapped in time with the presence of Gondwanaland. Together, these discoveries supported the existence of Pangea.
Which land feature supports the theory of continental drift?
Mountain ranges and other landforms provided evidence for continental drift. For example, Wegener noticed that when he pieced together maps of Africa and South America, a mountain range running from east to west in South Africa lines up with a range in Argentina.
What lived in Pangea?
Life on dry land included bacteria, fungi, plants, insects, amphibians, reptiles, saurians, the early mammals, and the first birds. All of this variety evolved over hundreds of millions of years (technically billions if you count the earliest life forms).
What is evidence of Pangea?
When was Pangea formed?
about 280-230 million years ago
From about 280-230 million years ago (Late Paleozoic Era until the Late Triassic), the continent we now know as North America was continuous with Africa, South America, and Europe. They all existed as a single continent called Pangea.
In what ways did continental drift impact the evolution of animals and plants living on Earth at the time explain?
As continents broke apart from Pangaea, species got separated by seas and oceans and speciation occurred. Individuals that were once able to interbreed were reproductively isolated from one another and eventually acquired adaptations that made them incompatible. This drove evolution by creating new species.
Can Pangea happen again?
Pangea broke apart about 200 million years ago, its pieces drifting away on the tectonic plates — but not permanently. The continents will reunite again in the deep future.