One factor that has affected how species are distributed is the motion of Earth's continents.
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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.
Continental drift affect temperature and precipitation patterns around the planet by changing ocean currents
The presence of glossopteris fossils in regions that are now widely separated provided evidence for continental drift. This plant species was found in South America, Africa, India, Antarctica, and Australia, suggesting that these landmasses were once part of a single supercontinent. The distribution of glossopteris fossils supported the theory of continental drift proposed by Alfred Wegener.
Continental drift has led to the separation and isolation of species, creating diverse ecosystems and unique biodiversity in different regions. It has also influenced the evolution of species, promoting speciation and adaptation to new environments. Some species have become endemic to specific regions due to the movement of continents.
Paleoclimatic evidence supporting continental drift includes the matching of certain rock formations, geological structures, and fossil distribution on continents now separated by vast oceans. For example, the presence of glacial deposits and coal seams that match across continents provides evidence that these landmasses were once connected. Additionally, the alignment of ancient climatic belts and the distribution of certain plant and animal species further support the theory of continental drift.
Fossils of the same species can be found on continents that are now today separated by oceans. btw continental drift is a fact.
They got separated.
Alfred Wegener used evidence from the fit of continents, distribution of fossils, rock types, and ancient climate data to support his theory of continental drift.
Evidence for continental drift includes the fit of the continents like a puzzle, similarities in rock formations and fossils across continents, and matching mountain ranges and geologic structures on different landmasses. Additionally, the distribution of certain species and climate indicators supports the theory of continental drift. These pieces of evidence suggest that the continents were once connected and have since moved apart over millions of years.