The answer is A
pollen
nobody knows
Clues to ancient climates include fossilized plants and animals, sediment records, ice core data, and geological formations such as ancient shorelines or glacial deposits. Isotopic analysis of these samples can provide information on temperature, precipitation, and atmospheric conditions during different time periods. Additionally, ancient climate can be inferred from past sea levels, vegetation distributions, and the presence of specific minerals or rock formations.
Alfred Wegener's evidence for continental drift came in the form of similarities in the ancient climates of continents that are now widely separated. Geological evidence, such as matching rock formations and fossil distributions, supported his theory that continents were once connected in a single landmass. Wegener proposed that these continents drifted apart over time, leading to the climate variations observed today.
Fossils serve as vital indicators of past climates by providing evidence of the types of organisms that existed in specific environments. For instance, the presence of certain plant or animal species, such as tropical ferns or corals, suggests warmer, more humid conditions, while others, like polar species, indicate colder climates. Additionally, fossilized remains can reveal information about the ecological conditions and atmospheric composition during the time they lived, allowing scientists to reconstruct ancient climates and understand climate change over geological time.
continents in the Southern Hemisphere today were once centered over the North Pole
pollen
comparisons of modern seashells and fossil shells
One piece of evidence that indicates ancient mammals are related to each other and to modern whales would be:each species had traits that allowed it to survive in a particular time and place in Earth's history.
Mediterranean.
Wegener showed evidence of similar rock formations and mountain ranges on different continents, evidence of matching plant and animal fossils on different continents, evidence of matching glacial deposits on different continents, and evidence of matching ancient climates on different continents to support his theory of continental drift.
Evidence of ancient climates, such as glacial deposits in regions that are now near the equator, support continental drift theory because they suggest that these regions were once located at higher latitudes where glaciers were common. This is consistent with the idea that continents were once joined together in different configurations and have since drifted to their current positions. Additionally, similarities in fossil distributions and rock formations across continents also support the theory of continental drift.
is there evidence of ancient aliens?
hi
Ancient Evidence - 2003 was released on: USA: 1 October 2003
The evidence for moving continents, known as continental drift, includes the fit of the coastlines of continents like South America and Africa, the similarity of rock formations and fossils on different continents, and the presence of ancient glaciation patterns on continents that are now located in warmer climates. These pieces of evidence formed the basis for the theory of plate tectonics.
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