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| OVERVIEW |
Jurassic 200–146 mya |
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Defining Characteristics:
- • ”The Age of Dinosaurs”: dinosaurs become very diverse, evolving into stegosaurs, theropods, and huge sauropods
- • Map of the Jurassic World
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Secondary Characteristics:
- • origin of birds
- • origin of the parasitic
feeding guilds in terrestrial ecosystems—possibly
replacing predators as top insect carnivores
- • Pangea continues breaking apart, and is
better separated toward the end of the Jurassic, with
a lush, warm tropical climate
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The name Jurassic comes from
the Jura Mountains, an extension of the Swiss Alps into eastern France,
where rocks of this age were first studied. They were first identified
as the Jura Kalkstein (“Jura Limestone”) by Alexander
von Humboldt in 1799, and later termed the Terrains Jurassiques
by Alexander Brongniart. The rocks were officially named the Jurassic
System by Leopold von Buch in 1839. Formed approximately 144–206
million years ago, Jurassic rocks have now been found on every continent.
Pangea was centered on the equator for most of the
Jurassic Period, and Earth’s climate was decidedly tropical.
During the Early Jurassic, some regions of the world were still arid,
but by the Late Jurassic much of the planet was lush. Great rivers
covered North America, and the land was green with ferns, seed
ferns, cycads, ginkgos, and conifers. It was
the ideal environment for the largest animals ever to walk on Earth—giant
sauropods such as Diplodocus,
as well as many other types of large dinosaurs. Like
today, much of the land was covered with trees, although flowering
plants had not yet evolved. And, like today, there were many understory
plants such as ferns, cycads, and
horsetails, but there was no
grass
for smaller animals to hide in. Because of the dinosaurs’ dominance,
mammals were still no larger than rats but had begun
to diversify by the Early Jurassic. The Jurassic seas were filled
with many types of sharks, bony fishes,
marine crocodiles, and other marine reptiles
of all sizes. Cephalopods such as
ammonites
propelled themselves through the oceans. Birds evolved
and began to diversify during the Late Jurassic, but the most common
flying vertebrates were the reptilian pterosaurs.
By the end of the Jurassic, major parts of Europe and North America
had become flooded as sea level rose, and Pangea continued to break
apart. As North America and Eurasia drifted away from
Africa and South America, the Atlantic Ocean was born, creating a
barrier for land travel between these regions.
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Overview |
Jurassic Life |
Diversity in the “Age of Dinosaurs”
Flight and the Origin of Birds |
Jurassic Climate and Tectonic Activity

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