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[[File:The Earth seen from Apollo 17.jpg|thumbnail]]
[[File:The Earth seen from Apollo 17.jpg|thumbnail]]


The Earth is a self-regulating system according to Gaia theory and its more mainstream offshoot, Earth system science. Through various cycles and processes, living beings around the planet cooperate to stabilize the Earth's temperature, acidity, salinity, atmosphere, and more. Thus, the Earth does not function as a hierarchy or as a competitive struggle between all beings. Rather, members of a highly decentralized global network cooperate to ensure mutual survival over millions and millions of years.
The Earth is a self-regulating system according to Earth system science and its more radical predecessor known as the Gaia hypothesis. The planet's biological, physical, and chemical components cooperate to stabilize the Earth's temperature, acidity, salinity, and atmosphere. Thus, the Earth does not function as a hierarchy or as merely a competitive struggle between all beings. Rather, members of a highly decentralized global network often cooperate to ensure mutual survival over billions of years.


James Lovelock and Lynn Margulis first advanced the Gaia hypothesis, jointly publishing in Carl Sagan's journal ''Icarus''. At first, they characterized the Earth as a living superorganism, drawing harsh criticism from reductionist scientists such as Richard Dawkins, who denounced the notion as "teleological." The critics asserted that the Earth cannot self-regulate since the it does not have the consciousness necessary to plan and have foresight. Lovelock responded by programming a computer simulation called Daisyworld. In Daisyworld, sunlight-reflecting white daisies and sunlight-absorbing black daisies cooperated to stabilize the planet's temperature, allowing life to thrive for an extended period of time. The model demonstrated that planetary self-regulation does not require the foresight or conscious planning.<ref>James Lovelock, ''The Ages of Gaia: A Biography of Our Living Earth, Updated and Revised'' (New York and London: W.W. Norton & Company, 1988), 8, 34-37.</ref>
=History of Gaia hypothesis and Earth system science=


Today, the mainstream body of research called Earth system science draws heavily on Gaian ideas but, in an effort to fit into dominant scientific culture, removes the reference to the Greek goddess Gaia. In Amsterdam in 2001, over a thousand delegates signed a statement, “The Earth System behaves as a single, self-regulating system comprised of physical, chemical, biological and human components.”<ref>http://www.colorado.edu/AmStudies/lewis/ecology/gaiadeclar.pdf. James Lovelock, ''The Revenge of Gaia: Earth's Climate Crisis & the Fate of Humanity'' (New York: Basic Books, 2006), 25.</ref>
James Lovelock and Lynn Margulis first advanced the Gaia hypothesis, jointly publishing in Carl Sagan's journal ''Icarus''. At first, they characterized the Earth as a living superorganism, drawing harsh criticism from reductionist scientists such as Richard Dawkins, who denounced the notion as "teleological." Critics like Dawkins asserted that the Earth cannot self-regulate since it does not have the consciousness necessary to plan and have foresight. In 1983, Lovelock responded by programming a computer simulation called Daisyworld. In Daisyworld, sunlight-reflecting white daisies and sunlight-absorbing black daisies cooperated to stabilize the planet's temperature, allowing life to thrive for an extended period of time. The model demonstrated that planetary self-regulation does not require foresight or conscious planning.<ref>James Lovelock, ''The Ages of Gaia: A Biography of Our Living Earth, Updated and Revised'' (New York and London: W.W. Norton & Company, 1988), 8, 34-37.</ref>
 
The biochemist Stephen Harding claims that such models have advanced the Gaia hypothesis into a Gaia theory. Harding has programmed more complex and realistic computer models of Daisyworld involving many types of plants, herbivores, and carnivores. This work further demonstrated the ability of the Earth to self-regulate. <ref>Stephen Harding, ''Animate Earth: Science, Intuition and Gaia, Second Edition'' (Totnes: Green Books Ltd, 2010), ch. 3.</ref>
 
Meanwhile, in the 1980s scientists at NASA and the International Geosphere-Biosphere Program (IGBP) were studying the Earth as a system composed of interlocking chemical, biological, and climactic processes.<ref>Sébastian Dutreuil, "Exploring the Origins of Earth System Science," Max Planc Institute for the History of Science, 2017, https://www.mpiwg-berlin.mpg.de/research/projects/exploring-origins-earth-system-science.</ref>
 
Today, Earth system science is a mainstream body of science. It draws heavily on Gaian ideas but, in an effort to fit into dominant scientific culture, removes the reference to the Greek earth goddess Gaia. In Amsterdam in 2001, over a thousand delegates signed a statement, “The Earth System behaves as a single, self-regulating system comprised of physical, chemical, biological and human components.”<ref>http://www.colorado.edu/AmStudies/lewis/ecology/gaiadeclar.pdf. James Lovelock, ''The Revenge of Gaia: Earth's Climate Crisis & the Fate of Humanity'' (New York: Basic Books, 2006), 25.</ref> Science writer Ferris Jabr observes that the "essence" of the Gaia hypothesis has entered "mainstream science." In particular, it is now widely understood that "life transforms and in many cases regulates the planet."<ref>Ferris Jabr, "The Earth is Just as Alive as You Are," ''New York Times'', 20 April 2019, https://www.nytimes.com/2019/04/20/opinion/sunday/amazon-earth-rain-forest-environment.html.</ref>
 
=Examples of Self-Regulation=
 
[[File:Gaia evidence.png|framed|center]]
 
Harding's book ''Animate Earth'' presents the charts above as evidence of the Earth's ability to self-regulate. The figure on the left shows that the the Earth has kept its conditions habitable for life for its 4.6 billion years of existence, despite the sun sending progressively more heat to the Earth. The middle chart shows that, until very recently impacted by extreme human impacts, the Earth kept its atmospheric levels of carbon dioxide within the stable range of 180 and 300 parts per million. The chart on the right shows that the Earth has consistently recovered even from mass extinction events, taking 5 to 10 million years each time. To Harding, this resilience "is strong evidence for Gaia."<ref>Harding, ''Animate Earth'', ch. 2.</ref>
 
Harding warns, however, that humans have largely impaired Gaia by taking over half of the planet's surface and by causing unprecedented rates of destruction. Thus, there is no guarantee that Gaia will survive this time around: “the fact that biodiversity has recovered after previous mass extinctions is no guarantee that the same thing will happen again. After all, Gaia is now older and more stressed by the sun, and the current mass extinction is happening much more quickly than any other.”<ref>Harding, ''Animate Earth'', ch. 11.</ref>
 
The nitrogen cycle is another example of self-regulation. Nitrogen is a key nutrient for life, but it isn't accessible until certain bacteria "fix" the air's nitrogen by bringing it into the soils and bodies of water. In a nitrogen-deficient ecosystem, bacteria that fixes its own nitrogen has a clear advantage over nonfixers, and the number of fixers will increase and enhances the ecosystem. Once there is abundant available nitrogen (it is toxic to an ecosystem in excess), the fixers lose their advantage over nonfixers. Thus, as Timonthy Lenton writes, "Reduced nitrogen input will lead to more nitrogen fixation; increased nirogen input, to less nitrogen fixation." This process has been observed in pastures and lakes and is theorized to be key to how the world's oceans maintain nutrient balance.<ref>Timothy Lenton, "Clarifying Gaia: Regulation with or without Natural Selection" in ''Scientists Debate Gaia: The Next Century'' ed. Stephen Schneider, James Miller, Eileen Crist and Penelope Boston (Cambridge: MIT Press, 2004), 20.</ref>
 
[[File:Nitrogen Cycle.svg|thumbnail]]
 
 
Another example involves the Amazon rainforest's summoning of rain. Jabr explains:
<blockquote>
Life in the Amazon does not simply receive rain — it summons it. All of that lush vegetation releases 20 billion tons of water vapor into the sky every day. Trees saturate the air with gaseous compounds and salts. Fungi exhale plumes of spores. The wind sweeps bacteria, pollen, leaf fragments and bits of insect shells into the atmosphere. The wet breath of the forest, peppered with microbes and organic residues, creates ideal conditions for rain. With so much water in the air and so many minute particles on which the water can condense, rain clouds quickly form.<ref>Jabr, "The Earth is Just as Alive as You Are."</ref>
</blockquote>


=Archean=
=Archean=


With each eon lasting a thousand million years, the Archean is the era from Earth's assembly 4.5 eons ago to the oxygen revolution 2.5 eons ago. During the Archean, Gaia theory suggests that life adapted the Earth to make it a home. There emerged a self-regulating interaction between early photosynthesizers (cyanoacteria) who cooled the Earth by removing heat-trapping carbon-dioxide from the atmosphere and methanogen decomposers ([[bacteria]]) who warmed the Earth by converting bacteria into the greenhouse gases carbon dioxide and methane.<ref>Lovelock, ''Ages of Gaia'', 73.</ref> So, the photosynthesizers were like the light daisies, and the decomposers were like the dark daisies.<ref>Lovelock, ''Ages of Gaia'', 76.</ref>
With each eon lasting a thousand million years, the Archean is the era from Earth's assembly 4.5 eons ago to the oxygen revolution 2.5 eons ago. Gaia theory suggests that life during the Archean adapted the Earth to make it a home. There emerged a self-regulating interaction between early photosynthesizers (cyanoacteria) who ''cooled'' the Earth by removing heat-trapping carbon-dioxide from the atmosphere and methanogen decomposers who ''warmed'' the Earth by converting [[bacteria]] into the greenhouse gases carbon dioxide and methane.<ref>Lovelock, ''Ages of Gaia'', 73.</ref> So, the photosynthesizers were like the light daisies of the Daisyworld model, and the decomposers were like the dark daisies. Together, they kept the planet at livable temperatures.<ref>Lovelock, ''Ages of Gaia'', 76.</ref>


=Proterozoic=
=Proterozoic=


Around 2.5 eons ago, photosynthesizers transformed the atmosphere from being methane-dominated to being oxygen-dominated. This transformation heralded a new geological era, the Proterozoic, and it allowed the evolution of new kinds of life, including the evolution of eukaryotes.
Around 2.5 eons ago, photosynthesizers transformed the atmosphere from being methane-dominated to being oxygen-dominated. This transformation heralded a new geological era, the Proterozoic. This period saw the [[Evolution of eukaryotes|evolution of eukaryotes]], when two cells symbiotically combined to form a more complex cell with a nucleus surrounded by a membrane. The new type of cell, the eukaryote, went on to become the building block of plants, animals, and fungi.


A key self-regulatory mechanism of the Proterozoic involved the deposit of calcium carbonate on the oceanic floor. Through such deposits, bacteria converted toxic soluble calcium into insoluble calcium. Although calcium is essential for many life forms, too much of it is deadly, and this self-regulatory mechanism would have been crucial for many beings' survival.<ref>Lovelock, ''The Ages of Gaia'', 98.</ref>
A key self-regulatory mechanism of the Proterozoic involved the deposit of calcium carbonate on the oceanic floor. Through such deposits, bacteria converted toxic soluble calcium into insoluble calcium. Although calcium is essential for many life forms, too much of it is deadly, and this self-regulatory mechanism would have been crucial for many beings' survival.<ref>Lovelock, ''The Ages of Gaia'', 98.</ref>


Another example of self-regulation involved salt-regulation. Few organisms can survive with an abundance of salt, and somehow oceans stayed within a safe salinity level. Various chemical reactions helped remove salt from the sea floor, and microorganisms deposited salt as sediments and as limestone.<ref>Lovelock, ''Ages of Gaia'', 98, 103.</ref>
Another example of self-regulation involved salt-regulation. Few organisms can survive with an abundance of salt, and oceans stayed within a safe salinity level. Various chemical reactions helped remove salt from the sea floor, and microorganisms deposited salt as sediments and as limestone.<ref>Lovelock, ''Ages of Gaia'', 98, 103.</ref>


=Phanerozoic=
=Phanerozoic=
Lasting from 600 million years ago until today, the Phanerozoic marks the time when organisms evolved to be large enough that they could be seen with a human's naked eye.<ref>Lovelock, ''Ages of Gaia'', 119.</ref> During this period, the carbon cycle marked one example of planetary self-regulation, in which the vegetation sequestered carbon and produced oxygen, keeping atmospheric carbon dioxide within levels manageable for most life on Earth. This process has, of course, been disrupted by the capitalist system's unprecedented levels of deforestation and greenhouse gas emissions.
=Resistance=
Raoul Vaneigem, formerly a theorist of the [[Situationist International]], argues that the Earth engages in resistance to the grow-or-die, destructive capitalist system:
<blockquote>
[N]ature has unpredictable fits of anger, sudden jolts that threaten the
edifice of civilization. And the moment it refuses to pro­duce, nature, like workers in revolt, is deemed stupid, pit­iless and cruel.<ref>Raoul Vaneigem, ''The Movement of the Free Spirit: General Considerations and Firsthand Testimony Concerning Some Brief Flowerings of Life in the Middle Ages, the Renaissance and, Incidentally, Our Own Time'' trans. Randall Cherry and Ian Patterson (New York: Zone Books, 1998), 32.</ref>
</blockquote>
Many anti-authoritarian societies, communities, and movements have sought to live in harmony with and act in defense of the Earth. For example, see [[Earth First!]] and [[Earth Liberation Front]].




<references/>
<references/>

Latest revision as of 17:16, 27 July 2021

The Earth seen from Apollo 17.jpg

The Earth is a self-regulating system according to Earth system science and its more radical predecessor known as the Gaia hypothesis. The planet's biological, physical, and chemical components cooperate to stabilize the Earth's temperature, acidity, salinity, and atmosphere. Thus, the Earth does not function as a hierarchy or as merely a competitive struggle between all beings. Rather, members of a highly decentralized global network often cooperate to ensure mutual survival over billions of years.

History of Gaia hypothesis and Earth system science

James Lovelock and Lynn Margulis first advanced the Gaia hypothesis, jointly publishing in Carl Sagan's journal Icarus. At first, they characterized the Earth as a living superorganism, drawing harsh criticism from reductionist scientists such as Richard Dawkins, who denounced the notion as "teleological." Critics like Dawkins asserted that the Earth cannot self-regulate since it does not have the consciousness necessary to plan and have foresight. In 1983, Lovelock responded by programming a computer simulation called Daisyworld. In Daisyworld, sunlight-reflecting white daisies and sunlight-absorbing black daisies cooperated to stabilize the planet's temperature, allowing life to thrive for an extended period of time. The model demonstrated that planetary self-regulation does not require foresight or conscious planning.[1]

The biochemist Stephen Harding claims that such models have advanced the Gaia hypothesis into a Gaia theory. Harding has programmed more complex and realistic computer models of Daisyworld involving many types of plants, herbivores, and carnivores. This work further demonstrated the ability of the Earth to self-regulate. [2]

Meanwhile, in the 1980s scientists at NASA and the International Geosphere-Biosphere Program (IGBP) were studying the Earth as a system composed of interlocking chemical, biological, and climactic processes.[3]

Today, Earth system science is a mainstream body of science. It draws heavily on Gaian ideas but, in an effort to fit into dominant scientific culture, removes the reference to the Greek earth goddess Gaia. In Amsterdam in 2001, over a thousand delegates signed a statement, “The Earth System behaves as a single, self-regulating system comprised of physical, chemical, biological and human components.”[4] Science writer Ferris Jabr observes that the "essence" of the Gaia hypothesis has entered "mainstream science." In particular, it is now widely understood that "life transforms and in many cases regulates the planet."[5]

Examples of Self-Regulation

Gaia evidence.png

Harding's book Animate Earth presents the charts above as evidence of the Earth's ability to self-regulate. The figure on the left shows that the the Earth has kept its conditions habitable for life for its 4.6 billion years of existence, despite the sun sending progressively more heat to the Earth. The middle chart shows that, until very recently impacted by extreme human impacts, the Earth kept its atmospheric levels of carbon dioxide within the stable range of 180 and 300 parts per million. The chart on the right shows that the Earth has consistently recovered even from mass extinction events, taking 5 to 10 million years each time. To Harding, this resilience "is strong evidence for Gaia."[6]

Harding warns, however, that humans have largely impaired Gaia by taking over half of the planet's surface and by causing unprecedented rates of destruction. Thus, there is no guarantee that Gaia will survive this time around: “the fact that biodiversity has recovered after previous mass extinctions is no guarantee that the same thing will happen again. After all, Gaia is now older and more stressed by the sun, and the current mass extinction is happening much more quickly than any other.”[7]

The nitrogen cycle is another example of self-regulation. Nitrogen is a key nutrient for life, but it isn't accessible until certain bacteria "fix" the air's nitrogen by bringing it into the soils and bodies of water. In a nitrogen-deficient ecosystem, bacteria that fixes its own nitrogen has a clear advantage over nonfixers, and the number of fixers will increase and enhances the ecosystem. Once there is abundant available nitrogen (it is toxic to an ecosystem in excess), the fixers lose their advantage over nonfixers. Thus, as Timonthy Lenton writes, "Reduced nitrogen input will lead to more nitrogen fixation; increased nirogen input, to less nitrogen fixation." This process has been observed in pastures and lakes and is theorized to be key to how the world's oceans maintain nutrient balance.[8]

Nitrogen Cycle.svg


Another example involves the Amazon rainforest's summoning of rain. Jabr explains:

Life in the Amazon does not simply receive rain — it summons it. All of that lush vegetation releases 20 billion tons of water vapor into the sky every day. Trees saturate the air with gaseous compounds and salts. Fungi exhale plumes of spores. The wind sweeps bacteria, pollen, leaf fragments and bits of insect shells into the atmosphere. The wet breath of the forest, peppered with microbes and organic residues, creates ideal conditions for rain. With so much water in the air and so many minute particles on which the water can condense, rain clouds quickly form.[9]

Archean

With each eon lasting a thousand million years, the Archean is the era from Earth's assembly 4.5 eons ago to the oxygen revolution 2.5 eons ago. Gaia theory suggests that life during the Archean adapted the Earth to make it a home. There emerged a self-regulating interaction between early photosynthesizers (cyanoacteria) who cooled the Earth by removing heat-trapping carbon-dioxide from the atmosphere and methanogen decomposers who warmed the Earth by converting bacteria into the greenhouse gases carbon dioxide and methane.[10] So, the photosynthesizers were like the light daisies of the Daisyworld model, and the decomposers were like the dark daisies. Together, they kept the planet at livable temperatures.[11]

Proterozoic

Around 2.5 eons ago, photosynthesizers transformed the atmosphere from being methane-dominated to being oxygen-dominated. This transformation heralded a new geological era, the Proterozoic. This period saw the evolution of eukaryotes, when two cells symbiotically combined to form a more complex cell with a nucleus surrounded by a membrane. The new type of cell, the eukaryote, went on to become the building block of plants, animals, and fungi.

A key self-regulatory mechanism of the Proterozoic involved the deposit of calcium carbonate on the oceanic floor. Through such deposits, bacteria converted toxic soluble calcium into insoluble calcium. Although calcium is essential for many life forms, too much of it is deadly, and this self-regulatory mechanism would have been crucial for many beings' survival.[12]

Another example of self-regulation involved salt-regulation. Few organisms can survive with an abundance of salt, and oceans stayed within a safe salinity level. Various chemical reactions helped remove salt from the sea floor, and microorganisms deposited salt as sediments and as limestone.[13]

Phanerozoic

Lasting from 600 million years ago until today, the Phanerozoic marks the time when organisms evolved to be large enough that they could be seen with a human's naked eye.[14] During this period, the carbon cycle marked one example of planetary self-regulation, in which the vegetation sequestered carbon and produced oxygen, keeping atmospheric carbon dioxide within levels manageable for most life on Earth. This process has, of course, been disrupted by the capitalist system's unprecedented levels of deforestation and greenhouse gas emissions.

Resistance

Raoul Vaneigem, formerly a theorist of the Situationist International, argues that the Earth engages in resistance to the grow-or-die, destructive capitalist system:

[N]ature has unpredictable fits of anger, sudden jolts that threaten the edifice of civilization. And the moment it refuses to pro­duce, nature, like workers in revolt, is deemed stupid, pit­iless and cruel.[15]

Many anti-authoritarian societies, communities, and movements have sought to live in harmony with and act in defense of the Earth. For example, see Earth First! and Earth Liberation Front.


  1. James Lovelock, The Ages of Gaia: A Biography of Our Living Earth, Updated and Revised (New York and London: W.W. Norton & Company, 1988), 8, 34-37.
  2. Stephen Harding, Animate Earth: Science, Intuition and Gaia, Second Edition (Totnes: Green Books Ltd, 2010), ch. 3.
  3. Sébastian Dutreuil, "Exploring the Origins of Earth System Science," Max Planc Institute for the History of Science, 2017, https://www.mpiwg-berlin.mpg.de/research/projects/exploring-origins-earth-system-science.
  4. http://www.colorado.edu/AmStudies/lewis/ecology/gaiadeclar.pdf. James Lovelock, The Revenge of Gaia: Earth's Climate Crisis & the Fate of Humanity (New York: Basic Books, 2006), 25.
  5. Ferris Jabr, "The Earth is Just as Alive as You Are," New York Times, 20 April 2019, https://www.nytimes.com/2019/04/20/opinion/sunday/amazon-earth-rain-forest-environment.html.
  6. Harding, Animate Earth, ch. 2.
  7. Harding, Animate Earth, ch. 11.
  8. Timothy Lenton, "Clarifying Gaia: Regulation with or without Natural Selection" in Scientists Debate Gaia: The Next Century ed. Stephen Schneider, James Miller, Eileen Crist and Penelope Boston (Cambridge: MIT Press, 2004), 20.
  9. Jabr, "The Earth is Just as Alive as You Are."
  10. Lovelock, Ages of Gaia, 73.
  11. Lovelock, Ages of Gaia, 76.
  12. Lovelock, The Ages of Gaia, 98.
  13. Lovelock, Ages of Gaia, 98, 103.
  14. Lovelock, Ages of Gaia, 119.
  15. Raoul Vaneigem, The Movement of the Free Spirit: General Considerations and Firsthand Testimony Concerning Some Brief Flowerings of Life in the Middle Ages, the Renaissance and, Incidentally, Our Own Time trans. Randall Cherry and Ian Patterson (New York: Zone Books, 1998), 32.