Happenings During the Mesozoic Era (248-65 Million Years Ago)
Characteristics of the Mesozoic
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L.Gardiner/Windows to the Universe (fossil images courtesy of AGI Imagebank)
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Time:
248 to 65 million years ago
(See
the geologic timescale!)
Paleogeography:
At the start of the Mesozoic, the continents were all joined together forming
one large continent called Pangaea. During Mesozoic time, they pulled apart
from one another. Continents move due to plate tectonics.
Climate:
- The climate most likely remained warm throughout the Mesozoic. No evidence
of glaciations has been found in Mesozoic age rocks and abundant evidence
of tropical species has been found in Mesozoic age fossils.
- During the last part of the Mesozoic (called the Cretaceous period) the
climate warmed very much. Earth was several degrees warmer than it is today.
There was much less variation in temperature between the equator and the poles
at this time.
- There is strong evidence that global cooling occurred at the end of the
Mesozoic. The cooling may have been caused by either a huge asteroid impact
near the Yucatan Peninsula, a large amount of volcanic eruptions in the area
that is today India and Pakistan, or by a combination of both the asteroid
and volcanoes. The Sun would have been blocked for some time by the debris
spewed into the atmosphere.
Evolutionary Events:
- Dinosaurs evolved and became abundant! Some were herbivores (eating
plants) while others were carnivores (eating meat). Dinosaurs were reptiles,
however there is some evidence that they may have been warm-blooded.
- Birds: During the late Mesozoic, birds evolved from a group of
small carnivorous dinosaurs.
- Plants: Conifer trees evolved at the beginning of the Mesozoic.
The first flowering plants evolved towards the end of the Mesozoic.
- Mammals evolved during the Mesozoic but there were relatively few
species and they were small in size. During the Mesozoic, mammals were eaten
by carnivorous dinosaurs.
- At the end of the Mesozoic, the Cretaceous-Tertiary Mass Extinction occurred.
This was the extinction event that killed the dinosaurs (among others). Many
of the animals and plants that survived the extinction event (such as mammals
and birds) went on to become very abundant afterward. Likely causes of the
extinction event include a large asteroid impact, erupting volcanoes, and
climate change. There is evidence that all three of these happened.
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Travel through Time! The Paleozoic (Before the Dinosaurs)
Travel through Time! The Cenozoic (The Last 65 Million Years)
Geologists Discover New Way of Estimating Size and Frequency of Meteorite Impacts
Page created June 1, 2005 by Lisa Gardiner.
Last modified August 23, 2009 by Jennifer Bergman.
The source of this material is Windows to the Universe, at http://www.windows.ucar.edu/ at the University Corporation for Atmospheric Research (UCAR). © The Regents of the University of Michigan. Windows to the Universe® is a registered trademark of UCAR. All Rights Reserved. Site policies and disclaimer