The Cenozoic Era http://bluepyramid.org/ia/woolmamm.jpg

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Title: The Cenozoic Era http://bluepyramid.org/ia/woolmamm.jpg


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The Cenozoic Era
http//bluepyramid.org/ia/woolmamm.jpg
Christy Stock, Madison Cooley, Katie Schmittauer
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65 Ma to Present The Cenozoic spans only about 65
million years, from the end of the Cretaceous and
the extinction of non-avian dinosaurs to the
present. The Cenozoic is sometimes called the Age
of Mammals, because mammals dominate the era.
Photo Link http//p.vtourist.com/2348861-West_tex
as_cave_drawings-Texas.jpg
The two time periods within the Cenozoic Era were
previously known as the Tertiary and the
Quaternary Periods, but are now known as the
Paleogene and Neogene Periods.
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Paleogene Period 66.5-23.03 Ma The name
Paleogene means Ancient-born. This is
because the animals on earth became more, but not
completely, modernized during the Paleogene
period.  
http//www.leloir.org.ar/espanol/paginas/Muestras/
CyT/-La_Evolucion-/Antepasados/Gondwana20y20Laur
asia.jpg
http//www.palaeos.com/Cenozoic/Paleogene.html
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The First Epoch of the Paleogene Period
  • Paleocene 66.5Ma 55.8Ma
  • The Paleogene epoch immediately followed the mass
    extinction event that killed the dinosaurs. This
    time division is known as the K-T Boundary.
  • The continents continued to drift North America
    and Greenland began to separate. The Rocky
    Mountains began to form.
  • Gondwanaland continued to split Africa, South
    America, Australia and Antarctica continued to
    pull apart.
  • Warm temperatures gave rise to forests that
    covered the globe, including the rise of the
    first recognizable rainforest.
  • Earlier mammals had been small and nocturnal. Due
    to the
  • extinction of the dinosaurs, they all grew bigger
    and more ferocious, although they still had
    extremely small brains and no specialized teeth
    or limbs. Reptiles became smaller, birds began
    to diversify into different types.

Photo Link http//www.kamcom.co.nz/kiwi/Gondwanal
and.gif
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The Second Epoch of the Paleogene Period
  • Eocene 55.8 Ma - 33.9 Ma
  • Emergence of the first modern mammals.
  • Began with extreme global warming known as the
    Paleocene-Eocene thermal maximum.
  • Australia and Antarctica began to split apart,
    and Laurasia began to become north America,
    Greenland, and Europe. The Alps reached their
    full height.
  • The entire earth was almost completely covered in
    rainforests, including Antarctica.
  • Primates began to develop teeth and limbs. The
    very first hoofed mammals emerged, as well as
    early forms of bats and marsupials. The earliest
    forms of whales appeared at this time.
  • When the Grande Coupure, some sort of meteor or
    asteroid, collided into Siberia, it formed
    Chesapeake Bay and caused a mass extinction event
    and marking the end of the Paleogene Period.

oto.blox.pl/resource/laurasia.jpg
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The Last Epoch of the Paleogene Period
  • Oligocene 34 Ma - 23 Ma
  • The warm climate gradually cooled into an ice
    age.
  • The expansion of grass begins to replace the
    forests, reptiles began to modernize and becoming
    more diverse.
  • Water animals, such as whales and sharks
    continued to develop and the oceans in some
    places began to cool, i.e. Antarctica.

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y-grass.jpg
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The Neogene Period 23 Ma - Present
  • The name neogene means new birth. This is
    because the Neogene period is the time that
    continues to today.

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0297.jpg
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The First Epoch of the Neogene Period The Miocene
Epoch - 23 Ma to 5.33 Ma
  • Lasting 18 million years, this epoch marks the
    end of old prehistoric world and the beginning of
    a more recent world. The Miocene also had a
    warmer climate than the epochs before and after.
  • Kelp forests and grasslands appeared during the
    Miocene epoch.
  • Antarctica became isolated. African-Arabian plate
    joined to Asia and a number of animal migrations
    took place.

http//www.palaeos.com/Cenozoic/Miocene/Miocene.ht
m
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The Second Epoch of the Neogene Period The
Pliocene Epoch - 5.3Ma to 1.8 Ma
  • It was a time of global cooling. This may have
    contributed to the spread of grasslands and
    savannahs.
  • Continents had taken their present day positions,
    the Mediterranean Sea dried up, and India
    collided with Asia bringing forth the Himalayan
    mountains
  • The epoch marked the beginning of large ice caps,
    especially in Antarctica. The ocean cooled and in
    the northern hemisphere there was a gradual
    southward migration of marine invertebrates.
  • The large-brained australopithecine Homo habilis
    continued on into the Early Pleistocene, giving
    rise to Homo erectus , the common ancestor of
    both Neanderthal and modern man during the late
    Pleistocene.

http//www.palaeos.com/Cenozoic/Pliocene/Pliocene.
htm
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The Third Epoch of the Neogene Period The
Pleistocene Epoch - 1.81 to 0.012 Ma
  • During the Pleistocene the first true Ice Age
    hit. The sea level rose during the melting of the
    glaciers, then dropped again during the next
    period of glacier formation. The lowered sea
    levels formed land bridges that enabled the
    migration of animals and humans across
    continents.
  • Animals were at their heights, and mammals
    dominated the globe, although they were living in
    unusual places, for instance hippos and elephants
    in modern-day London.
  • During the Pleistocene the hominid tendency to
    increase brain size and hence intelligence
    continued.

http//www.palaeos.com/Cenozoic/Pleistocene/Pleist
ocene.htm
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The Third Epoch of the Neogene Period The
Holocene Epoch - The Last 12,000 Years
http//www.math.montana.edu/nmp/materials/ess/atm
osphere/advanced/activities/andrew/hurricane.andre
w.globe.gif
  • The boundary between the Pleistocene and the
    recent is set at around 10,000 years BCE (12,000
    years ago), which represented a marked climatic
    warming phase and the beginning of the present
    warm period between glaciations.
  • This age has witnessed the rise of civilization. 
    The ten thousand years of its extent are too
    short to see much in the way of the evolution of
    species and ecosystems, but natural processes of
    erosion and sedimentation have been supplemented
    by human activities and geographical impacts the
    rise of towns, fields, roads, etc.  And there has
    been a growth in human population and
    knowledge.   

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Resources
General Information about the Cenozoic Era
http//www.ucmp.berkeley.edu/cenozoic/cenozoic.htm
l Information about the Paleocene Epoch
http//en.wikipedia.org/wiki/Paleocene Information
about the Eocene Epoch http//en.wikipedia.org/w
iki/Eocene Information about the Oligocene Epoch
http//en.wikipedia.org/wiki/Oligocene Information
about the Neocene Time Period
http//www.palaeos.com/Cenozoic/Neogene.html Infor
mation about the Miocene Epoch
http//www.palaeos.com/Cenozoic/Miocene/Miocene.ht
m Information about the Pliocene Epoch
http//www.palaeos.com/Cenozoic/Pliocene/Pliocene.
htm Information about the Pleistocene Epoch
http//www.palaeos.com/Cenozoic/Pleistocene/Pleist
ocene.htm Information about the Holocene Epoch
http//www.palaeos.com/Cenozoic/Holocene/Holocene.
htm
Picture Link http//www.dot.co.pima.az.us/gis/tr
ip/grass.jpg
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