Okay, we're going to take a quick overview look at the Mesozoic Era, also known as the Age of Reptiles. It lasted from 252 to 66 million years ago. It has 3 Periods nestled within it; the Triassic, Jurassic and Cretaceous periods. It was characterized by dinosaurs, conifers and ferns, a hot greenhouse climate, and the tectonic break-up of Pangaea.
The Mesozoic began just after the
largest well-documented mass extinction in Earth's history, and it ended with
another extinction event.
During this era, the supercontinent
Pangaea broke into separate landmasses that would eventually move into their
current positions during the following era. There was not much mountain
building during this era, but what little did occur took place around what is
now known as the Arctic Ocean. In contrast, the supercontinent Pangaea
gradually split into a northern continent, Laurasia, and a southern continent,
Gondwana. (Seems like this name has been used before.) By the end of the era,
the continents had split up and some had rejoined into their present forms,
though not their present positions. Laurasia became North America and Eurasia,
while Gondwana split into South America, Africa, Australia, Antarctica and the
Indian subcontinent, which would eventually slam into Asia, giving rise to the Himalayas, but not during this Era.
The climate varied, alternating
between warm and cool periods. Overall, the Earth was hotter than it is today.
The Triassic (first) Period was generally dry and highly seasonal, especially in
Pangaea's interior. Low sea levels would have exacerbated temperature extremes.
Pangaea's interior probably included expansive deserts.
Sea levels began to rise during the
Jurassic (second) Period, most likely caused by seafloor spreading. The sea
levels could have risen as much as 656 ft (200 m) above today's sea level. This
would have flooded coastal area. In addition, the breaking up of Gondwana into
smaller continents created new shorelines. Temperatures continued to increase
for a time, then began to stabilize. With the proximity of water, humidity also
increased, and the deserts retreated.
The climate of the Cretaceous (third)
Period is more widely disputed. Probably, higher levels of carbon dioxide in
the atmosphere could have almost eliminated the north-south temperature
gradient, meaning that temperatures were about the same across the planet,
about 10 degrees Centigrade higher than today.
Dinosaurs first appeared mid-way
through the first period, and became the dominant terrestrial vertebrates by early
in the second period, then died out at the end of the third period. Archaic
birds appeared during the 2nd period (Jurassic), evolving from a branch of
dinosaurs. True birds appeared in the third period. Mammals also appeared
during this era, but they remained small (less than 33 lb) until the third
period. Flowering plants appeared early in the third period and rapidly
diversified, replacing conifers and other gymnosperms as the dominant group of
plants. But we'll take a closer look at flora and fauna as we get to those
periods.
https://en.wikipedia.org/wiki/Mesozoic
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