Gaia Hypothesis and Daisy World
The development of the Gaia Hypothesis is described with some emphasis on how the concept has evolved in response to other scientist's skepticism. The Gaia concept itself is described and discussed. A possible means for reconciliation of the holistic Gaia hypothesis with reductionist thinking is discussed. I conclude by summarizing what the paper has accomplished.
The Gaia Hypothesis was first published by James E. Lovelock in 1972 (Lovelock, par. 23). It was, at the time, the end product of a series of observations Lovelock had made about Earth, Mars and Venus (Margulis and Lovelock, p. 11(2)).
The premise underlying the Gaia hypothesis is that the entire planet evolves over time because of the interaction of living things with their surrounding environment. Because of the interdependence of the evolution of environment and biome, Lovelock likened the entire planet Earth to a living thing with complex interlocking planet-wide systems that maintain a condition of homeostasis conducive to Earth's long-term habitability.
While the existence of symbiotic relationships between some species has been long observed and accepted, the ultimately symbiotic relationship of every living thing on Earth proved too broad a claim for many scientists to accept. Consequently, the Gaia hypothesis has been generally lambasted by most mainstream scientists.
In the next section, I describe the hypothesis in some detail and provide background information. This will be followed by a discussion contrasting Lovelock's claims with those of his critics and proffers an approach toward reconciliation and my concluding comments.
Background.
In 1957 James E. Lovelock invented a device called the electron capture detector that can accurately measure minute traces of specific elements and chemical compounds. He used this in Antarctica to detect the presence of CFCs in the atmosphere as well as the presence of DDT in many samples from around the world, including human breast milk (Holden, p. 1977). In other words, James Lovelock is the person more responsible than any other for getting DDT and CFCs removed from the market, for it was his invention that first allowed accurate measurements of these pollutants.
In 1961 he was invited to join NASA and contribute toward America's exploration of Earth's moon (Lovelock, par. 16). Later, he found himself advising NASA on its Viking Project planned to land stationary probes on the Martian surface. Part of the mission goal was to establish whether life was present on the Red Planet.
Before the mission was launched, Lovelock advised NASA to cancel the biological research portion of the mission because, he surmised, there was not currently any significant life on Mars. His reasons had to do with his examination of the Martian atmosphere.
Mars' atmosphere consists primarily of carbon dioxide at very low atmospheric pressure. It is essentially chemically inert and thus in a state of chemical equilibrium. Lovelock reasoned that were there living things on Mars capable of photosynthesis, we would expect to find free oxygen in the Martian atmosphere. He drew a similar conclusion based on the absence of methane from Mars' atmosphere. Methane is a common byproduct of the decomposition of dead plants and animals. With neither methane nor oxygen in detectable quantities in Mars' atmosphere, there seemed ample reason to conclude that nothing lives there that could be detected by the Viking landers' (there were two of them) instruments.
He drew the same conclusion about the likelihood of finding life on Venus, based on similar evidence.
Earth's atmosphere is not in a state of chemical equilibrium. It is full of gases that have an affinity for each other. Oxygen, nitrogen, and methane exist in sizable quantities, and left to their own devices, would quickly interact to form a new atmosphere of inert gases, very much like Mars' atmosphere (Margulis and Lovelock, p. 13(2)). So the persistent presence of uncombined methane, nitrogen, and oxygen in the atmosphere is strong evidence that something is replenishing these gases as fast as they naturally interact.
The answer is life (Margulis and Lovelock, p. 88 (1)). Organisms that can perform photosynthesis continuously pump oxygen into the atmosphere faster than it can react with methane or nitrogen. Microbes break down nitrates in the soil and pump out nitrogen faster than it can react with atmospheric oxygen. Decaying flora and fauna release methane into the environment in the same way. Essentially, the current state of Earth's atmosphere is the inevitable result of the kind of things that live here.
This realization was the seed for Lovelock's Gaia hypothesis. Among other things, the Gaia hypothesis proposes that the complexity of Earth's ecosystem is analogical to the complexity of an organism. Thus, Earth, while not being actually alive, is like a living thing in many respects.
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