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Dinosaur fossils
     1.1.1
     1.1.1
 2.2.32.3.1




       What is geological time and the history of life on Earth?


         Our planet is approximately                                                                 Earth forms
       4,600,000,000 years old. For humans, with   fig.199 Life and geological  me.   Cambrian        Moon forms
       a lifespan of less than 100 years, these                                      Explosion
       numbers are almost impossible to                                                              Oceans form
       comprehend. Yet to fully understand why
       our planet is like it is today we do need to      Evolu on of grass                   541 million years  PHANEROZOIC  HADEAN
       understand its full history. What were the   Ex nc on of dinosuars              PROTEROZOIC  600 million years First
       key  me periods and events through which                                       1,958 million years  life
       our world evolved?                         Breakup of Pangea       Today  Green
                                                                            algae
         This history is recorded in the Earth's   Life moves onto          evolves
       rocks, which act as the planet's history   the land                                       1,500 million years
       book. Geological  me is the way that
                                                                                                   ARCHEAN
       scien sts have divided Earth’s history into                          Red-brown
                                            541 million b.p.                algae
       chapters, separated by significant events.                            appears                   Beginning of
       These events are preserved as changes in                                                     photosynthesis
       rocks. However, instead of using years,   Mass ex nc on  Evolu on    Increasing   ‘Snowball     by bacteria
       days, hours and minutes, which are too   event         of the        atmospheric  Earth’
       brief to encompass the  mescale of stone,              dinosuars     oxygen            Evidence of
       geological  me uses eons, eras, periods                                                atmospheric oxygen
       and epochs.                           Stromatolites, ‘living rocks’, formed   flowering plants. This, in turn, saw the
         Figure 199 shows the four eons of   from a build-up of microbial mats, appear   diversifica on of pollina ng insects into
       geological  me. They are unimaginably   in the fossil record 3.7 billion years ago,   bu erflies, moths, midges, bees.
       long periods of  me. One way to give a   just before 05:00 hours. They became the   Dinosaurs were wiped out in another
       sense of the enormity of this geological   dominant life of the shallow seas for over   mass ex nc on just before 23:40, crea ng
        me is to imagine the history of the Earth   twelve hours in our imaginary day.   an evolu onary niche for early mammals
       compressed into a single 24 hour day.   It is not un l 13:00 hours that more   to exploit. In the post-dinosaur Cenozoic
       The Hadean Eon                     complex, single-celled organisms, with a   era it took another 30 million years for
                                          cell nucleus emerge. Mul -cellular   grass to evolve at 23:49. Grasses then
          In this model the Earth was created   organisms appear at around 16:10 and   spurred the evolu on of many species of
       from space debris orbi ng the Sun at 00:00
                                          heralded the beginning of the decline of   grazing animals.
       hours. The first big event happened at   the stromatolites.
       about 00:30 hours when the Earth was                                      Our earliest hominid ancestors may
       involved in a cosmic collision with another   The Phanerozic Eon       have walked the Earth by 23:58 but our
       new planet. This collision knocked the   Just a er 21:10 there was a sudden   own species, Homo sapiens, did not
       Earth off its ver cal axis. The debris from   diversifica on of life in the seas. Known as   emerge un l 200,000 years ago, at just
       that collision was thrown back into space   the ‘Cambrian explosion', this period of   four seconds to midnight. Our human
       to form the Moon. It took 600 million years    me saw a vast expansion of aqua c life   ancestors invented agriculture and began
       for the surface of the Earth to cool down   forms. By 21:41 sharks had evolved,   to live in ci es just one fi h of a second
       sufficiently for the rock to become solid.  hun ng the seas for other early fish.  before midnight. Neil Armstrong set foot
                                                                              on the Moon (4.5 billion years a er its own
       The Archean Eon                       At 21:14 plants began to colonise the   forma on) at just 0.000925 seconds before
                                          land, followed soon by the first land
         Life may have evolved in its most   animals.  However, they would not become   the end of our imaginary day.
       primi ve form between 02:30 to 04:30   fully-established un l 21:44. Land plants at
       hours. Photosynthesising bacteria evolved   this  me resembled simple mosses which   KEY TERMS
       around 06:15. The first evidence of
                                          evolved into large tree ferns and primi ve
       atmospheric oxygen, a waste product of   trees by 22:00. These trees covered the   Eon: the longest division of geological
       photosynthesis, is found the end of the   Earth in dense forests by 22:10 hours.   time dividing the history of Earth into four
       Archean at 11:30 hours.                                                  sections: Hadean, Archean, Proterozoic
                                             A mass ex nc on, probably caused by   and Phanerozoic.
       The Proterozoic Eon                a meteorite strike, wiped out 90% of life   Era: subdivision of an eon, usually marked
         The Proterozoic witnessed the first   forms at the end of the Permian period at   by a significant change in the
       mass ex nc on on Earth as the planet’s   22:26. This event marked the start of the   development of life on the planet.
       first atmospheric pollutant, oxygen gas,   Triassic period and saw the evolu on of   Period: subdivision of era, often marked
       wiped out most early life forms. The   the dinosaurs. Dinosaurs were highly   by a change in the fossil record, eg.
       oxygen reduced methane levels in the   successful, domina ng the world for 183   Carboniferous period.
       atmosphere, plunging the world into a 300   million years throughout the Triassic,   Epoch: subdivision of a period, marked by
       million year-long glacia on, known as   Jurassic and Cretaceous periods.   change in the conditions for, and of, life
       ‘Snowball Earth’.                     At 23:15 the Earth saw the evolu on of   on the planet, eg. Holocene epoch.
                                                                                Age: subdivision of an epoch.
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       The climate has changed from the start of the Quaternary period.
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