BIO210Y5 Lecture Notes - Cambrian, Cambrian Explosion, Sirius Passet

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2 Aug 2012
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Chapter 21- the history of life on earth. Fossils- the preserved remains of ancient organisms. Age of rocks cannot be determined by just looking at them, but the age of rocks can only be determined when comparing one another. Strata- oldest layers in rocks; are known to lie at the bottom, and successively higher strata are progressively younger. Radioactivity- a method of dating rocks; discovered at the beginning of the twentieth century. Half-life- a successive time interval in which half of the remaining radioactive material of the radioisotope decays, either changing into another element or becoming the stable isotope of the same element. For 14c, production in the upper atmosphere is about equal to its natural decay. When an organism dies, it is no longer incorporating 14c from the environment. The 14c that was present in the body decays with no replacement and the ratio of 14c to 12c decreases.

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