The theory of plate tectonics easily explains the distribution of mesosaurus. When mesosaurus was alive, all of the continents were massed together into the supercontinent Pangaea. Therefor, South America and Africa met because there was no Atlantic Ocean, so the distribution of mesosaurus makes complete sense.
As the sample size increases, and the number of samples taken increases, the distribution of the means will tend to a normal distribution. This is the Central Limit Theorem (CLT). Try out the applet and you will have a better understanding of the CLT.
No
It could be a Gaussian curve (Normal distribution) rotated through a right angle.It could be a Gaussian curve (Normal distribution) rotated through a right angle.It could be a Gaussian curve (Normal distribution) rotated through a right angle.It could be a Gaussian curve (Normal distribution) rotated through a right angle.
Could a traingle and a rectangle ever be congruent? Explain.
The theory of plate tectonics easily explains the distribution of mesosaurus. When mesosaurus was alive, all of the continents were massed together into the supercontinent Pangaea. Therefor, South America and Africa met because there was no Atlantic Ocean, so the distribution of mesosaurus makes complete sense.
The theory of plate tectonics easily explains the distribution of mesosaurus. When mesosaurus was alive, all of the continents were massed together into the supercontinent Pangaea. Therefor, South America and Africa met because there was no Atlantic Ocean, so the distribution of mesosaurus makes complete sense.
Old answer: the scientists found them in the 2 regions andMesosaurus was significant in providing evidence for the theory of continental drift, because its remains were found in southern Africa and eastern South America, two far away places. As Mesosaurus was a small freshwater organism, and therefore could not have crossed the Atlantic Ocean, this distribution indicated that Africa and South America used to be joined together. Indeed, all the world's continents were joined into one supercontinent called Pangaea in the time Mesosaurus existed.
The geographic distribution of the swimming reptile Mesosaurus provides evidence that supports continental drift. Fossils belonging to the Mesosaurus were found far away from each other, in both South Africa and South America.
South America and Africa were once joined.
Mesosaurus fossils
South america and Africa were once joined.
interim distribution
The case of Mesosaurus does not, by itself, prove the theory of continental drift, as it requires additional evidence to establish a comprehensive explanation. While Mesosaurus fossils found in both South America and Africa suggest past connectivity between these continents, they alone cannot confirm the theory without supporting geological and paleontological data. The alignment of other fossil records, geological formations, and the distribution of similar species across continents collectively strengthen the argument for continental drift. Thus, while Mesosaurus contributes to the evidence, it is not definitive proof on its own.
The Mesosaurus lived in Antarctica back 100 million to 200 million years ago : )
Mesosaurus skeletons provide evidence for the theory of continental drift. This ancient freshwater reptile was found in both South America and Africa, suggesting that these continents were once connected. The distribution of Mesosaurus fossils supports the idea that landmasses have moved over geological time, challenging the notion of species evolving independently on separate continents. This evidence played a significant role in the development of the theory proposed by Alfred Wegener in the early 20th century.
The case of Mesosaurus does not by itself prove the theory of continental drift, but it provides significant evidence supporting it. Mesosaurus was a freshwater reptile found in both South America and Africa, suggesting these continents were once joined. The existence of similar fossils on widely separated landmasses is difficult to explain without considering continental movement. However, additional evidence from geology, paleomagnetism, and other fossil types further supports the theory.