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66      PART II • Tectonic-Scale Climate Change


                                  500                       over the South Pole by 125 Myr ago, yet no ice sheet
                                           South Pole       developed. Antarctica remained directly over the pole
                                 450        position        but largely ice-free from 125 Myr ago until near 35 Myr
                                                            ago, when ice reappeared. Here again we face the mys-
                                                            tery encountered earlier: How could a landmass cen-
                                                            tered on a pole remain ice-free (or largely so) for almost
                                430      Arabia             100 Myr?
           South America                                       Clearly the polar position hypothesis cannot fully
                              Africa
                                          India             explain the sequence of glaciated and unglaciated
                         380                                intervals over the last 500 Myr. Yet the hypothesis is
                                                            successful to this extent: ice sheets developed only
                                                            on landmasses that were at polar or near-polar posi-
                                   300
                                                            tions, consistent with their polar locations today.
                       330
                                                            This correlation (see Table 4-1) confirms that over
                             Antarctica                     the last 500 Myr continents had to occupy polar posi-
                                        250
              Direction                          Australia  tions for large-scale glaciation to occur. But the same
              of ice flow                                   record also tells us that the presence of continents in a
                                                            polar position does not guarantee that ice sheets will
                                                            form.
        FIGURE 4-8 Gondwana glaciation and the South Pole
        Changes in the position of the south magnetic pole in relation
        to the continent of Gondwana are largely the result of the
        slow movement of Gondwana. Glaciations occurred in the
        northern Sahara about 440 Myr ago and in southern
        Gondwana (South Africa, Antarctica, India, South America,
        and Australia) 325–240 Myr ago. The (shallow) water shown
        between the modern continental outlines was land during
        Pangaean times. (Adapted from T. J. Crowley et al.,
        “Gondwanaland’s Seasonal Cycle,” Nature 329 [1987]: 803–7,
        based on P. Morel and E. Irving, “Tentative Paleocontinental Maps
        for the Early Phanerozoic and Proterozoic,” Journal of Geology 86
        [1978]: 535–61].)



            From 325 to 240 Myr ago, Gondwana continued its
         slow journey across the South Pole, and a huge region
         centered on the south-central part of the continent was
         glaciated (see Figure 4-8). The ice sheets were centered
         on modern Antarctica and South Africa, and they spread
         out into adjoining regions of South America, Australia,
         and India. Because of the correspondence between the
         area of Gondwana that was glaciated and its position at
         or near the south magnetic pole, this long interval of
         glaciation is fully consistent with the polar position
         hypothesis.
            By 240 Myr ago, Gondwana had moved northward
         and the glaciation had ended. The absence of ice after
         that time agrees with the positioning of the land away
         from the South Pole. By that time, the northern part
         of Gondwana had begun to merge with the northern
         continents and form the even larger supercontinent
         Pangaea.                                           FIGURE 4-9 Glacial striations Sediment rubble carried in
            After 180 Myr ago Pangaea began to break up. Its  the bottom layers of ice sheets about 440 Myr ago gouged
         southernmost part, which included the modern conti-  striations in North African bedrock similar to those in modern
         nents of Antarctica, India, and Australia, moved back  ice in Alaska, shown here. (Carr Clifton.)
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