Edaphosaurus
The fi rst true
mammals began to
evolve during the
Triassic period
Triassic fi sh and
ocean reptiles lived
in the warm seas
Ivantosaurus
Diplodocus
Augustasaurus
Pliosaurus
Chasmatosaurus
Lystrosaurus
Ichthyosaurs
Cynognathus
THE PREHISTORIC WORLD
Evolution of the dinosaur world
250 to 200 million years ago
It might have been quite hot and
dry, but that didn’t stop the very
fi rst mammals and fl ying reptiles
from appearing. Trees and plants
also grew in the places we know
today as the cold and icy south
and north poles
Triassic period
How did the dinosaurs’
world evolve?
Dinosaurs roamed Earth between
230 and 65 million years ago, when our
planet was very different to today
The ultra-dr y climates of the Permian
era, and the subsequent destruction of
the ancient coal swamps that were
home to a great many Carboniferous plants,
meant that the Mesozoic (or ‘middle life’) era
signalled something of a recover y period in
Earth’s histor y. Comprising the Triassic,
Jurassic and Cretaceous periods, the Mesozoic
era was less dr y but was still swathed in high
global temperatures, and the now-empt y
ecosystems on the land were soon taken over by
evolv ing mammals and dinosaurs. Meanwhile,
beneath the oceans, new corals appeared and
various sea urchins began to diversif y and
thrive, having been almost driven to the point
of extinction at the end of the Permian era.
Some estimates put some of the more tropical
temperatures during the start of the Triassic
period (at the beginning of the Mesozoic era)
as high as 38°C (100°F), and at this point
the world’s land masses were still
combined in one large supercontinent
called Pangaea. During the Triassic
period, Pangaea gave rise to climatic
zonation, with some areas becoming extremely
dr y and others experiencing monsoon-like
conditions. As a consequence of this climatic
zonation, plants began to separate into
northern and southern realms.
By the time of the Jurassic period, global
temperatures had dropped to around 30°C (86°F)
and Pangaea had separated into northern and
southern parts. The oceans as we know them
today really started to take shape during the
Cretaceous period – so-called because of the
large chalk content in the shallow seas as a
result of the build up of algae skeletons.
Following the major extinctions at the end of
the Cretaceous period, mammals – which were
prev iously small and insignifi cant compared to
the dinosaurs – were now able to exploit many
of the vacant ecosystems and gradually come to
dominate the planet.
200 to 145 million years ago
The Jurassic period is called the ‘Age
of the Reptiles’ because it was during
this time that reptiles ruled the planet
Jurassic period
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