Chapter 17 - The History of Life Flashcards

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1
Q

What does the fossil record provide?

A

evidence about the history of life on Earth

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2
Q

What does the fossil record show in regards to evolution?

A

how different groups of organisms, including species, have changed over time

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3
Q

How is the age of a fossil determined through relative dating?

A

By comparing its placement with that of fossils in other layers of rock

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4
Q

Which rock layer is older, the top or bottom?

A

the bottom

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5
Q

What are index fossils?

A

fossils used to compare the relative ages of fossils

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6
Q

What is a half-life?

A

the length of time required for half of the radioactive atoms in a sample to decay

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7
Q

What is radioactive dating?

A

the use of half-lives to determine the age of a sample

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8
Q

How is the age of a fossil determined through radioactive dating?

A

Scientists calculate the age of a sample based on the amount of remaining radioactive isotopes it contains

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9
Q

What is the half-life of Carbon-14?

A

5730 years

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10
Q

What are the eras following the Precambrian time?

A

Paleozoic, Mesozoic and Cenozoic respectively

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11
Q

What period are we currently in?

A

Quaternary

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12
Q

What is macroevolution?

A

large-scale evolutionary patterns and processes that occur over long periods of time

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13
Q

What are the 6 important topics in macroevolution?

A

extinction, adaptive radiation, convergent evolution, coevolution, punctuated equilibrium, and changes in developmental genes

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14
Q

What is adaptive radiation?

A

when a single species or a small group of species has evolved into diverse forms that live in different ways (ex. finches)

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15
Q

What is convergent evolution?

A

unrelated organisms come to resemble one another (ex. shark, penguins and dolphin)

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16
Q

What is coevolution?

A

process by which two species evolve in response to changes in each other over time

17
Q

What is punctuated equilibrium?

A

pattern of long, stable periods interrupted by brief periods of more rapid change

18
Q

What is gradualism?

A

slow and steady change in a particular line of descent