Period Epoch Age MYA Cretaceous 2 Senonian Maastrichtian 65 Campanian 73 Santonian 83 Coniacian 87 Unnamed Turonian 88 Cenomanian 91 Cretaceous 1 Albian 97 Aptian 113 Barremian 119 Neocomian Hauterivian 125 Valanginian 131 Berriasian 138 Malm Tithonian 144 Kimmeridgian 150 Oxfordian 156 Dogger Callovian 163 Bathonian 169 Bajocian 175 Aalenian 181 Lias Toarcian 188 Pliensbachian 194 Sinemurian 200 Hettangian 206 Triassic 3 Rhaetian 213 Norian 219 Carnian 225 Triassic 2 Ladinian 231 Anisian 238 Scythian (Triassic 1) Spathian 243 Smithian Dienarian Griesbachian
Geology: At the beginning of the Triassic
Period, all of the continents were lumped together into
a large continent called Pangaea. There was no Atlantic
ocean at this time. Approximately 135 million years ago,
this continent broke up into two major landmasses: Laurasia
and Gondwana. 35 million years later, Gondwana broke up into
present-day South America and Africa. The Indian
subcontinent began its 8000-km journey pursuing Asia. 45
million years ago, Australia, like South America, became
independent of Antarctica. This brought about some curious
results (explained in the Cenozoic).
Climate in the Mesozoic was
generally warm and wet. Animal Life: Almost anyone who thinks about the Mesozoic
will think "dinosaur" at the
same time. After all, the Mesozoic
has been dubbed "The Age of the Reptiles." You can read more
about these in this era's Creature
Feature. Different types of reptiles existed: Dinosaurs were not the only
ones, though. Insects had large developments, the first
inconspicuous mammals appeared,
and swimming and flying
reptiles conquered the sea and sky. Plant Life: Taking advantage of the warm and wet climate, the major
plants were cycads, ferns,
and ginkgoes. Later, in the
Cretaceous, flowering
plants would start to evolve with insect
pollinators.

