Page 53 - The Restless Earth Fossils
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52   Fossils


                         boundaries  between  Paleozoic,  Mesozoic,  and  Cenozoic  Eras.
                         Fossils show that 90% of Paleozoic species disappeared 251 mil-
                         lion years ago between the Permian and Triassic Periods and 65%
                         died 65 million years ago between the Cretaceous and Tertiary
                         Periods.  (Remember  all  that  Cold  oysters  Congeal  Quickly
                         stuff at the end of Chapter 3? The Tertiary is the first period at
                         the beginning of the Cenozoic Era.) Paleontologists study these
                         mass extinction events carefully, hoping to understand them
                         so that Homo sapiens can avoid turning up on a list of extinction
                         fatalities.


                         precaMBrian eternities

                         So what was going on during that long stretch from when the
                         Earth  was  congealing  from  hot  star  stuff  just  beyond  your  left
                         fingertip  to  your  right  wrist?  Life  existed  during  much  of  that
                         Precambrian  time,  but  it  was  microscopic.  Sometimes,  it  left
                         little  more  than  chemical  traces  in  ancient  rocks  until  about
                         3,500  million  years  ago.  Then,  some  chains  of  simple  plant
                         cells—informally referred to as pond scum—coiled together into
                         some  amazing  pillars  of  cells  and  sand  called  stromatolites.
                         Fossil stromatolites look a bit like giant concrete stalks of cauli-
                         flower, but they changed the course of history forever by evolving
                         the process of photosynthesis—a technique for using light energy
                         to turn water and carbon dioxide into sugars with the aid of a
                         “helper” molecule called chlorophyll. Stromatolites, as a result,
                         had to “pass a little gas.” Unlike the methane that escapes from
                         animals from time to time, plants release oxygen—the waste prod-
                         uct of photosynthesis.
                             The earliest living cells made energy by breaking the chemi-
                         cal  bonds  in  methane  and  various  sulfur  compounds.  Oxygen,
                         because it reacts with vital chemicals very quickly, was a deadly
                         poison. Stromatolites were so successful that they drove the first
                         living cells to “hellish” places like hot sulfur springs (like those
                         in Yellowstone National Park) and deep-sea hydrothermal vents










        RE_Fossils2print.indd   52                                                             3/17/09   8:59:43 AM
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