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Into the Cool, Part III, Chapter 13
Blue Planet Blues

   

Ecosystems are nonequilibrium dissipative processes. The kind of energy required for organisms to maintain their bodies, their metabolism, is strictly limited. The list includes light (photoautotrophy), organic chemical energy (heterotrophy), and a very limited number of inorganic energy-yielding chemical reactions (sulfide to sulfur or sulfate, methane to carbon dioxide, ammonia to oxidized nitrogen compounds, hydrogen to water). Heat, a thermodynamic waste product roughly equivalent to entropy, is not on the list. Organisms also need food, which forms the stuff of their bodies. Energy gets used up; food is transformed into matter and materials of the body.

Ecology has been called an orphan science. In contrast with theoretical physics, space sciences, and the human genome project, ecology attracts little money. The federal budget for theoretical ecology is in the tens of millions of dollars annually whereas tens of billions of dollars support these other fields. Why does ecology, the study of the home that supports us, receive such scant attention? Perhaps it is because ecosystems are so ordinary. Familiarity can engender contempt: human-supporting ecosystems are neither wondrously huge nor enchantingly tiny. They hark to no ancient time nor storybook place. They are right here now, at our scale, in our face…..

Odum's 1969 paper was given as the presidential address to the Ecological Society of America annual meeting at the University of Maryland. During this period of great political unrest in the United States because of the war in Vietnam, there was also an industry- and labor-supported backlash on recent national environmental victories. The college campuses were in an uproar over both issues. Even though this paper is the most important synthesis of phenomenological observations of ecosystems ever completed, more than a third of it is dedicated to environmental issues. Here was the president of the Ecological Society of America speaking out on crucial political-environmental issues of his time: "Thus the preservation of natural areas [is not a] peripheral luxury for society, but a capital investment from which we expect to draw interest. Also, it may well be that the restrictions in the use of land and water are our only means of avoiding overpopulation or too great an exploitation of resources, or both.” It was a brave lecture for its time.

Odum's classic text Fundamentals of Ecology, first published in 1971, linked energy flow to succession. In both his 1969 paper and his text Odum made some basic observations. With regard to ecological succession, he made three points: (1) "It is an orderly process of community development that is reasonably directional and therefore, predictable." (2) "It results from modification of the physical environment by the community." (3) "It culminates in a stabilized ecosystem in which maximum biomass (or high information content) and symbiotic function between organisms are maintained per unit of energy flow.”

Odum's ecology fits comfortably into our thermodynamic paradigm. We have attempted to synthesize Odum's basic ideas in the Figure. This diagram maps changes in ecosystem characteristics discussed in this and the next chapter. We have made additions and attempted to distill Odum's ideas. Across the top of the figure is the flora associated with the archetypal New England succession, from fallow field to oak-hickory forest. In the western United States the sequence would look similar, with sagebrush instead of blackberries and bunch grasses playing the role of crabgrass. The final stages of the western forest would be fir, spruce, or white pine instead of oak. The same successional processes are seen in grasslands, where there are no forests of oaks and fir. Grasslands go through their own succession, with annual grasses replaced by perennials. The ecosystem is doing its "best" under its constraints to prosper. Many of the steppes and grasslands of the world are water-limited, and the grasslands have evolved to develop a stable community that degrades incoming energy as completely as possible.

A climax ecosystem should be looked at as a mosaic of different stages of ecosystem succession. Each time one of these major setbacks happens, for example a big forest fire, the ecological structure and process are set back to the beginning like a player sent to Go on a Monopoly board, the initiation point for the game. The penalty is not being thrown out of the game, but being set back to zero and starting the progression again.

Because of the patchiness in ecosystem disturbance, ecosystems tend not to die. But then, they are not organisms (no organism recycles all its materials), although, like organisms, they are complex thermodynamic systems. Ecosystems represent biologically stable patterns across many scales of a space-time hierarchy. Climax systems are vulnerable to rapid change. The systems are often at an unstable point, like dry wood load and biomass in a dry forest. A very small perturbation, a spark from metal to rock of a passing horseshoe, can reset the successional clock within seconds. Nonlinear dynamics and catastrophic events are common throughout these biological systems.

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Part III: The living

11. Thermodynamics and Life

12. Brimstone Beginnings

13. Blue Planet Blues

14. Regress under Stress

15. The Secret of Trees

16. Into the Cool

17. Trends in Evolution



The energy flow through an ecosystem. Ecological processes are driven by the flow of energy from the sun to thermal and chemical sinks. Primary producers (autotrophs) fix about 1% of the energy impinging upon them. Herbivores, from insects to elk, consume autotrophs that in turn are eaten by carnivores, which are often eaten by other carnivores. Each time food (chemical energy) passes up the food chain, 80–90% of the energy is lost to heat (entropy). By the time energy passes up four or five trophic levels, very little energy makes it to the top. Ecologists call this structure a trophic pyramid, because many organisms are required at the base of the system to sustain the few on top. (Adapted from Morowitz [1968] 1979.)



Changes in ecosystem characteristics over time and during successional development. The succession from grassland to climax forest is typical of the eastern forests of the United States. Similar succession takes place in aquatic and other terrestrial ecosystems, with different species playing different roles in the process. The biomass of the ecosystem and total system throughput (TST) increase during succession. Production-biomass ratios (P/B) decrease during succession, meaning that late successional systems require less food or energy to maintain a unit of weight. These later mature ecosystems are more efficient than their predecessors. (Adapted from Schneider 1988.)

© 2005 Hawkwood Institute • Eric D. SchneiderInto the Cool