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Earth

What is Gaia?

Gaia: Evidence for Homeostasis

From "Biological Modulation of the Earth's Atmosphere"

Margulis and Lovelock, 1973

  • compiled of cybernetic systems
  • has the ability to control atmospheric

gas concentration

Origin

The Earth is Consistent

Theory

Greek Origin

Early after life began...

1. Patterns of crustal alterations and soil formation

have stayed constant through time

aquired control over planetary environment

References...

the maintenence of homeostasis by and for

the atmosphere has persisted ever since

all systems on earth are connected:

plant, animal and human

2. Ocean basins, lake and stream morphology

  • have not changed much in 3 billion years

Lynn Margulis: Science’s Unruly Earth Mother.

Research News vol 252, 19 April 1991, pp 378-381

3. Temperature changes have occured, but not too extreme

Lovelock, J.E. and Margulis, Lynn.

Biological

6 Nov 1973

Modulation of the Earth’s Atmosphere,

Lovelock, James. "What Is Gaia?" James Lovelock. Ecolo.org. Web. 15 Nov. 2011. <http://www.ecolo.org/lovelock/what_is_Gaia.html>.

Control of Acidity and Redox

Conclusion

How Life Changes the Atmosphere..

Microbial Contribution

If the Earth had no life...

  • Earth has maintained a relatively

constant atmospheric pH

Lovelock on "What is Gaia states “we now see that the air, the ocean and the soil are much more than a mere environment for life; they are part of life itself.”

The End

1. Nitrogen Fixation

  • Oxidation/ Reduction potential controlled

mainly by biota

  • since about 3 billion

years ago

If the Gaia hypothesis is proven to be true?

2. Carbon Fixation

Adds

Algae, blue-green algae

  • methane
  • ammonia
  • diatomic nitrogen
  • diatomic oxygen, ect.

3. Oxygen Secretion

  • All components of the environment are interconnected and maintain homeostasis for life on Earth.
  • New hypothesis concerning the improvement of global sustainability can be formulated regarding our Planets limiting resources for agriculture, water and topsoil.

Controlling Temperature

Three Stages of Atmosphere

Radiation Balance

  • incoming solar
  • Emissivity
  • Albedo

1. Anaerobic conditions

2. Transition from reducing to oxidizing conditions

Ozone

3. Conditions oxidized and stable for abundant life

Gas Composition

Suspended Particulate Matter

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