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O x y g e n
E z r a D a v e I g n a c i o
The theory of how oxygen gas (O2) came to the earth and started the
beginning of life.
Oxygenrevolution
EarlyEarth
The atmosphere on early
Earth was very different than
what we have today. It is
thought that the first
atmosphere of the Earth was
made up of hydrogen and
helium, much like the gaseous
planets and the Sun.
After millions of years of volcanic
eruptions and other internal Earth
processes, the second atmosphere
emerged. This atmosphere was full of
greenhouse gases like carbon dioxide,
sulfur dioxide, and also contained other
types of vapors and gases like water vapor
and, to a lesser extent, ammonia and
methane.
Green House gases
>> While there are
many theories of how
life began on Earth, it is
certain that the first
organisms to inhabit
the Earth had to not
need oxygen, as there
was no free oxygen in
the atmosphere.
> This combination of
gases was very
inhospitable to most
forms of life.
Oxygen
-free!
>>> Most scientists agree that the building blocks of life would not have
been able to form if there had been oxygen in the atmosphere at that time.
CarbonDioxide
However, plants and other autotrophic
organisms would thrive in an atmosphere
filled with carbon dioxide and one of the
main reactants necessary for
photosynthesis to occur. With carbon
dioxide and water, an autotroph can
produce a carbohydrate for energy and
oxygen as waste. After many plants
evolved on Earth, there was an
abundance of oxygen in the atmosphere.
It is hypothesized
that no living thing
on Earth at that
time had a use for
oxygen. In fact, the
abundance oxygen
was toxic to some
autotrophs and
they became
extinct.
Toxic!
Beneficial oxygen
Even though oxygen gas couldn't be used directly by living things, oxygen wasn't
all bad for these organisms living during that time.
Oxygen gas floated to the top of the atmosphere where it was exposed to
ultraviolet rays of the sun. Those UV rays split the diatomic oxygen molecules and
helped to create ozone, which is made up of three oxygen atoms covalently
bonded to one another.
The ozone layer helped
block some of the UV rays
from reaching Earth. This
made it safer for life to
colonize on land without
being susceptible to those
damaging rays.
Before the ozone layer formed, life had to stay
in the oceans where it was protected from the
harsh heat and radiation.
The
Ozone
Since oxygen was so
plentiful in these early
stages of colonization of
land, many of the
ancestors of the species
we know today grew to
enormous sizes. There is
evidence that some types
of insects grew to be the
size of some of the larger
types of birds.
With a protective layer of
ozone to cover them and
plenty of oxygen gas to
breathe, heterotrophs were
able to evolve. The first
consumers to appear were
simple herbivores that
could eat the plants that
survived the oxygen laden
atmosphere.
LandLife!
Giveandtake
More heterotrophs could then evolve as
there were more food sources. These
heterotrophs happened to release carbon
dioxide as a waste product of their cellular
respiration.
The give and take of the autotrophs and
heterotrophs were able to keep levels of
oxygen and carbon dioxide in the
atmosphere steady. This give and take
continues today.
T h a n k y o u

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How oxygen gas allowed life to thrive on Earth

  • 1. O x y g e n E z r a D a v e I g n a c i o
  • 2. The theory of how oxygen gas (O2) came to the earth and started the beginning of life. Oxygenrevolution
  • 3. EarlyEarth The atmosphere on early Earth was very different than what we have today. It is thought that the first atmosphere of the Earth was made up of hydrogen and helium, much like the gaseous planets and the Sun.
  • 4. After millions of years of volcanic eruptions and other internal Earth processes, the second atmosphere emerged. This atmosphere was full of greenhouse gases like carbon dioxide, sulfur dioxide, and also contained other types of vapors and gases like water vapor and, to a lesser extent, ammonia and methane. Green House gases
  • 5. >> While there are many theories of how life began on Earth, it is certain that the first organisms to inhabit the Earth had to not need oxygen, as there was no free oxygen in the atmosphere. > This combination of gases was very inhospitable to most forms of life. Oxygen -free! >>> Most scientists agree that the building blocks of life would not have been able to form if there had been oxygen in the atmosphere at that time.
  • 6. CarbonDioxide However, plants and other autotrophic organisms would thrive in an atmosphere filled with carbon dioxide and one of the main reactants necessary for photosynthesis to occur. With carbon dioxide and water, an autotroph can produce a carbohydrate for energy and oxygen as waste. After many plants evolved on Earth, there was an abundance of oxygen in the atmosphere.
  • 7. It is hypothesized that no living thing on Earth at that time had a use for oxygen. In fact, the abundance oxygen was toxic to some autotrophs and they became extinct. Toxic!
  • 8. Beneficial oxygen Even though oxygen gas couldn't be used directly by living things, oxygen wasn't all bad for these organisms living during that time. Oxygen gas floated to the top of the atmosphere where it was exposed to ultraviolet rays of the sun. Those UV rays split the diatomic oxygen molecules and helped to create ozone, which is made up of three oxygen atoms covalently bonded to one another.
  • 9. The ozone layer helped block some of the UV rays from reaching Earth. This made it safer for life to colonize on land without being susceptible to those damaging rays. Before the ozone layer formed, life had to stay in the oceans where it was protected from the harsh heat and radiation. The Ozone
  • 10. Since oxygen was so plentiful in these early stages of colonization of land, many of the ancestors of the species we know today grew to enormous sizes. There is evidence that some types of insects grew to be the size of some of the larger types of birds. With a protective layer of ozone to cover them and plenty of oxygen gas to breathe, heterotrophs were able to evolve. The first consumers to appear were simple herbivores that could eat the plants that survived the oxygen laden atmosphere. LandLife!
  • 11. Giveandtake More heterotrophs could then evolve as there were more food sources. These heterotrophs happened to release carbon dioxide as a waste product of their cellular respiration. The give and take of the autotrophs and heterotrophs were able to keep levels of oxygen and carbon dioxide in the atmosphere steady. This give and take continues today.
  • 12. T h a n k y o u

Editor's Notes

  1. It is hypothesized that no living thing on Earth at that time had a use for oxygen. In fact, the abundance oxygen was toxic to some autotrophs and they became extinct.