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CHAPTER 2 • Climate Archives, Data, and Models  23


        Radioactive   Stable        Stable daughter
        isotope       isotope       product
















              24    Parent
           Number of radioactive  isotopes in sample  12  isotope
              18



               6
                    isotope
               0    Daughter
                                            1                         1 2                       12 3
                                                  Time (in half-lives)

        FIGURE 2-8 Radioactive decay Time is determined by measuring the gradual decay of a
        radioactive parent isotope to a daughter isotope. The half-life is the time needed for half the
        parent to decay. The relative abundances of parent and daughter isotopes follow the trends
        shown at the bottom. (D. Merritts et al., Environmental Geology, © 1997 by W. H. Freeman and
        Company.)




        of dating and correlation using fossils or other features  a few areas using nearby igneous rocks, the ages that
        in the sediments. The fossil method relies on the fact  are obtained can be transferred to sediments in other
        that a unique and unrepeated sequence of organisms has  regions that contain the same short-lived fossils but lack
        appeared and disappeared through Earth’s entire his-  radiometric dating. Other physical or chemical features
        tory and has left fossilized remains. The most useful  that show distinctively varying patterns (like ash layers)
        fossils are those that are shortest-lived but geographi-  can be used in a similar way.
        cally most widespread. If the brief existence of these  Radiocarbon In the younger geologic record, a dif-
        species can be reliably dated in sediments in at least  ferent method, radiocarbon dating, is widely used to





          TABLE 2-1   Radioactive Decay Used to Date Climate Records
          Parent isotope      Daughter isotope    Half-life     Useful for ages: Useful for dating:

                                           87
                      87
          Rubidium–87 ( Rb)   Strontium–87 ( Sr)  47 Byr        100 Myr         Granites
          Uranium–238 ( 238 U)  Lead–206 ( 206 Pb)  4.5 Byr     >100 Myr        Many rocks
          Uranium–235 ( 235 U)  Lead–207 ( 207 Pb)  0.7 Byr     >100 Myr        Many rocks
                                        40
                      40
          Potassium–40 ( K)   Argon–40 ( Ar)      1.3 Byr       >100,000 years  Basalts
          Thorium 230 ( 230 Th)  Radon–226*( 226 Ra)  75,000 years  <400,000 years  Corals
                                           14
                    14
          Carbon–14 ( C)      Nitrogen–14* ( N)   5,780 years   <50,000 years   Anything that contains carbon
          *Daughter in this case is a gas that has escaped and cannot be measured.
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