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Vesna [10]
3 years ago
13

Please Help! A.S.A.P!! Will Mark Brainliest!

Biology
2 answers:
saveliy_v [14]3 years ago
6 0

Answer:

Newer layers of earth form <u>on</u><u> </u><u>top</u> of older layers, so as we dig, we can see further back in time. Comparing the fossils between the layers can offer evidence of change.

<u>Phyletic</u><u> </u><u>gradualism</u> - slow, but constant gradual change; supported by transitional species in the fossil record

<u>Punctuated</u><u> </u><u>equilibrium</u>- long periods of no change followed by short periods of rapid change.  Can also be supported by the fossil record when no transitional species are found.

kirza4 [7]3 years ago
6 0

Answer: Newer layers of earth form on top  of older layers, so as we dig, we can see further back in time. Comparing the fossils between the layers can offer evidence of change. Phyletic gradualism  slow, but constant gradual change; supported by transitional species in the fossil record Punctuated equilibrium long periods of no change followed by short periods of rapid change.  Can also be supported by the fossil record when no transitional species are found. hope this helps p :) but, i just looked up the sentences and it gave me the answers.

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The theory of evolution first formulated in Darwin's book is the process by which organisms change over time as a result of changes in heritable physical or behavioral traits that allow them to better adapt to its environment, survive and have more offspring.

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Population Speciation

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Natural selection

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