Gaia Theory: A Critical Analysis
In the 1960's, James Lovelock, a British atmospheric chemist, was engaged in research commissioned by the National Aeronautic and Space Administration
NASA) in the United States. Specifically, the studies were intended to develop a method for determining reliably whether or not biological life existed on Mars. Part of Lovelock's work involved analyzing certain elements of Earth's atmospheric properties and mechanisms, in order to understand how a planet teeming with biological life might be differentiated accurately from interplanetary distances from a planet completely devoid of biological life (Enteractive, 1995).
While Lovelock's NASA research project originally pertained to Mars rather than to the Earth, his findings led him to postulate a theory in which he characterized
Earth as a complex living organism, rather than merely an inanimate host for the many terrestrial life forms dependent on it for sustenance. Lovelock called his theory
Gaia" after an ancient Greek Goddess of the Earth and published his ideas outlining the principle elements of Gaia Science in 1968. In his book GAIA: The Practical
Science of Planetary Medicine, Lovelock suggests that the Earth is itself a tremendously large and complex super-organism, comprising all of the (other) life forms dependant upon it in very much the same fashion that the human body comprises the many trillions of individual living cellular organisms that, collectively, constitute a human being (Lovelock, 1991).
Initially, mainstream scientists rejected the notion of a living Earth outright, and others objected to the characterization of Gaia as a scientific theory, suggesting that it represents merely a metaphor for what Earth scientists already know about the delicate balance of terrestrial life, rather than a new scientific postulate capable of empirical proof or disproof (Gould, 1991). More recently, Lovelock has found support for his ideas from other scientists such as Peter Liss, an environmental researcher, and renowned Harvard University sociobiologist, Edmond O. Wilson, author of the 1998 best seller Consilience: The Unity of Knowledge. Together,
Lovelock, Liss and Wilson launched a new venture in 1998 dedicated to promoting
Gaia science and research on Earth as a self-regulating system (AAAS, 1998).
Essential Elements of Gaia Theory:
Initially, what struck Lovelock about the chemistry of Earth's atmosphere was the preponderance of some of its individual gaseous elements without any apparent explanation for their failure to have combined into other substances, given the timescale involved. According to Lovelock, nitrogen in particular readily combines with oxygen, and his calculations suggested that the atmosphere contains billions of times more solitary nitrogen than it should. His conclusion was that the perpetual existence of so much elemental nitrogen in the atmosphere could not be explained by natural chemical mechanisms, but only by the effects of metabolic processes of living organisms and their interaction with the atmosphere.
Similarly, Lovelock suggests that the stability and relative uniformity of the gaseous composition and temperature of Earth's atmosphere could not be explained by ordinary inorganic chemistry. Furthermore, global climate has remained essentially the same despite the fact that the amount of solar energy that reaches the Earth varied significantly during that time, increasing quite substantially since the first appearance of terrestrial life. Lovelock (1991) proposed that a feedback loop or similar mechanism is responsible, whereby the organic processes of living organisms release so-called "greenhouse" gases to warm the planet when necessary, and that a stable temperature is maintained by their many deaths when the planet becomes too warm for them to survive.
According to Gaia scientists, complex mechanisms would also have had to replenish the atmospheric ammonia, carbon dioxide and methane in order to maintain such a stable global temperature via the greenhouse effect. Conversely, any global temperature increases beyond the normal range (whether from increasing solar radiation or organic overpopulation) would quickly result in the deaths of a proportionate amount of organic life to reduce the greenhouse effect in order to maintain the Earth's stable climate over time. Gaia theorists regard this as precisely the same type of biofeedback loops that enable (other) living organisms to maintain homeostatic equilibrium (Lovelock, 1991).
Lovelock (1991) proposes a very similar feedback loop-type of relationship between nitrous oxide produced by anaerobic microbial organisms living in the soil of the seabed to account for the stability of the correct proportion of oxygen to support biological life on Earth.
As far as the oceans are concerned, Lovelock (1991) explains the delicate maintenance of the optimal salinity for biological life through a complicated interrelationship between the terrestrial sources of salt that increase ocean salinity and the relative...
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