The fourth of five main geological eras, falling
between the Paleozoic and Cenozoic, and the erathem of
rocks deposited in this era. It includes the Triassic, Jurassic,
and Cretaceous Periods. The era begins at 248 million years
ago at the end of the Permian-Triassic extinction event and
continues to 66.4 million years ago at the Cretaceous-Tertiary
(K-T) extinction event. Named by Charles Lyell in 1830,
the term means middle life, recognizing the major differences
in the fossil record between the preceding Paleozoic era, and
the succeeding Cenozoic era. Mesozoic life saw the development
of reptiles and dinosaurs, mammals, birds, many invertebrate
species that are still flourishing, and saw flowering
plants and conifers inhabit the land. The era is commonly
referred to as the age of reptiles, since they dominated the terrestrial,
marine, and aerial environments.
Pangea continued to grow in the Early Mesozoic, with
numerous collisions in eastern Asia, but as the supercontinent
grew in some areas, it was breaking apart in others. As the
fragments drifted apart especially in the later part of the Mesozoic,
continental fragments became isolated and life-forms
began to evolve separately in different places, allowing independent
forms to develop, such as the marsupials of Australia.
The Atlantic Ocean began opening as arcs and oceanic terranes
collided with western North America. In the later part of
the Mesozoic in the Cretaceous, sea levels were high and shallow
seas covered much of western North America and central
Eurasia, depositing extensive shallow marine carbonates.
Many marine organisms such as plankton rapidly diversified
and bloomed, and thick organic rich deposits formed source
rocks for numerous coal and oil fields. With the high Cretaceous
sea levels, Cretaceous rocks are abundant on many continents
and are the most represented of the Mesozoic strata.
These strata are rich in fossils that show both ancient and
modern features, including dinosaurs, ammonoids, plus newly
developed bony fishes, and flowering plants. The dinosaurs
and reptiles continued to rule the land, sea, and air until the
devastating series of events, culminating with the collision of
an asteroid or comet with Earth at the end of the Cretaceous,
eliminating the dinosaurs, and causing the extinction of 45
percent of marine genera including the ammonites, belemnites,
inoceramid clams, and large marine reptiles.
See also CRETACEOUS; JURASSIC; MASS EXTINCTIONS;
TRIASSIC.














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