animals
an intrusive fossil
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.
Continental drift can affect fossil remains by causing them to be dispersed across different continents as landmasses move. It can also result in changes to the environmental conditions where fossils are found, impacting preservation and fossil formation processes. Additionally, the movement of continents can lead to the creation of new habitats or barriers, influencing the distribution and evolution of species.
No, most animals and plants that have lived on Earth do not leave fossil evidence. Fossilization is a rare process that only occurs under specific conditions, so many organisms decompose before they can become fossils. This is why the fossil record is incomplete and biased towards certain types of organisms.
This isn't the full answer sorry but The globetrotters plant
The trilobite fossil occurs on the most landmasses. This suggests that trilobites were widespread and inhabited different parts of the world before continents broke apart, when the supercontinent Pangaea existed. Trilobites demonstrate how species can be widespread across continents that were once connected.
This isn't the full answer sorry but The globetrotters plant
the glossoptersis plant
animals
This isn't the full answer sorry but The globetrotters plant
Africa
Africa
an intrusive fossil
The intersection of a common fossil on two different landmasses' borders allowed scientists to reconstruct Pangaea.
Yes, about 29% of Earth's surface is land, while the remaining 71% is covered by water. Landmasses include continents and islands.
Based on scientific knowledge and geological evidence, landmasses fit together in a way that supports the theory of plate tectonics. The shapes and boundaries of continents and oceanic plates align based on factors like fossil records, rock formations, and seismic activity patterns, supporting the idea of continental drift and the historical movement of landmasses over time.