Explain how carbon-14 level can be used for estimating ages of archeological artifacts. O Level of carbon-14 increases in atmosphere, remains relatively constant in living organisms, and gradually decreases in lifeless objects. O Level of carbon-14 remains relatively constant in atmosphere, increases in living organisms, and gradually decreases in lifeless objects. O Level of carbon-14 gradually decreases in atmosphere and in living organisms, and increases in lifeless objects. O Level of carbon-14 in living organisms is equal to the level in atmosphere, and gradually decreases in lifeless objects.

Human Anatomy & Physiology (11th Edition)
11th Edition
ISBN:9780134580999
Author:Elaine N. Marieb, Katja N. Hoehn
Publisher:Elaine N. Marieb, Katja N. Hoehn
Chapter1: The Human Body: An Orientation
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Problem 1RQ: The correct sequence of levels forming the structural hierarchy is A. (a) organ, organ system,...
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Explain how carbon-14 level can be used for estimating ages of archeological artifacts.
O Level of carbon-14 increases in atmosphere, remains relatively constant in living organisms, and gradually decreases in lifeless objects.
O Level of carbon-14 remains relatively constant in atmosphere, increases in living organisms, and gradually decreases in lifeless objects.
O Level of carbon-14 gradually decreases in atmosphere and in living organisms, and increases in lifeless objects.
O Level of carbon-14 in living organisms is equal to the level in atmosphere, and gradually decreases in lifeless objects.
Transcribed Image Text:Explain how carbon-14 level can be used for estimating ages of archeological artifacts. O Level of carbon-14 increases in atmosphere, remains relatively constant in living organisms, and gradually decreases in lifeless objects. O Level of carbon-14 remains relatively constant in atmosphere, increases in living organisms, and gradually decreases in lifeless objects. O Level of carbon-14 gradually decreases in atmosphere and in living organisms, and increases in lifeless objects. O Level of carbon-14 in living organisms is equal to the level in atmosphere, and gradually decreases in lifeless objects.
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