By definition,
dynamical systems are those that change or evolve with time. Biological
evolution is only a subset of dynamical evolution. If a dynamical system does
not receive an input of energy, it decays towards a state of equilibrium, and
then stops evolving. Energy is the engine that drives all evolution.
The planet we
live on is a spaceship, which has been receiving an input of negative-entropy
solar energy throughout its existence. Influx of this energy is mainly
responsible for keeping our planet in a state away from equilibrium, which is
the reason for the ever-rising levels of its complexity. All life-forms on
Earth owe their existence and sustenance to this input of energy from the Sun. And
the entire ecosphere can be regarded as one single, highly complex, system: SYSTEM
EARTH.
In a notable
book (Energy: Engine of Evolution), Niele
(2005) presented the Earth's historical energy-staircase of increasing
complexity. As becomes clear on a perusal of Niele's book, an energy-based
evolutionary approach to the history of the Earth provides major insights into
our current affairs.
Our
energy-emitting Sun came into being ~4.6 billion years ago. The energy it emits
in all directions comes from the thermonuclear fusion reactions taking place in
it. Some of the energy emitted by the Sun is intercepted by our Earth, and most
of it is then emitted back into outer space in due course in a highly degraded
form.
Energy has the
capacity and tendency to cause change. For the change to occur, the energy has
to transform to another quality. According to the second law of thermodynamics,
such change entails an overall state of higher disorder or entropy. This
dissipation can occur only if there are dissipative paths available. As
we shall see presently, such paths are indeed there for the energy available on
Earth.
Most of the
solar energy received by the atmosphere surrounding the Earth escapes from it
ultimately. If this were not so, the average temperature of the Earth would go
on rising. What we have instead is a fairly constant average temperature.
The tiny
fraction of low-entropy (or high-quality) solar energy retained by the Earth
drives processes such as photosynthesis. Some other sources of energy on the Earth
are: geothermal energy; cosmic microwave radiation; and the energy released by
natural and artificial radioactivity. The energy flow in and around the Earth
is influenced by the energy flows in the universe. A delicate balance exists
among gravitation, nuclear reactions, and radiation, which moderates this flow
of energy.
As analyzed by
Niele (2005), there have
been FIVE ENERGY REVOLUTIONS since the origin of life on Earth:
1. The
photo-energy revolution (emergence of photosynthesis). This occurred
~3.8 billion years ago.
2. The
oxo-energy revolution (aerobic respiration). This occurred ~2.1 billion
years ago.
3. The
pyro-energy revolution (domestication of fire by humankind). This
occurred ~0.5 million years ago.
4. The
agro-energy revolution. This occurred ~12,000 years ago.
5. The
carbo-energy revolution. This occurred ~400 years ago.
Each energy
revolution heralded a new dominant ENERGY REGIME: Exposure to a new energy
source can herald a new dominant-energy regime, provided a new path for energy
dissipation is available.
Shown above is Niele's 'historical energy staircase' for the system Earth,
with near-constant influx of low-entropy energy (mainly solar energy). Plotted
on the x-axis is time (not to scale). The y-axis depicts schematically the
generally increasing degree of (terrestrial) complexity. Niele has identified the
various energy revolutions (at times marked t1, t2,
etc.), each such revolution heralding the onset of a specific energy regime. For
example, the Photoenergy Revolution, which occurred at time t1, marked
the emergence of the Phototrophic Energy Regime.
t1 = ~3.8 billion years ago;
t2 = ~2.1 billion years ago;
t3 = ~0.5 million years ago;
t4 = ~12000 years ago; and
t5 = ~400 years ago.
The time t6 is when the next energy revolution will occur, and is
a question mark at present. We can only speculate about it. One possible
scenario is that t6 will mark the emergence of a Nucleocultural
Energy Regime, heralded by a Nuclear-Energy Revolution, but, as I shall discuss
in future posts, there are other possibilities also.
Six
ecologically dominant energy regimes have been identified by Niele in the history
of the Earth. These are:
(i)
Thermophilic regime. The corresponding energy period is called the thermion
period.
(ii)
Phototrophic regime (photian period).
(iii)
Aerobic regime (oxian period).
(iv)
Pyrocultural regime (pyrian period).
(v)
Agrocultural regime (agrian period).
(vi)
Carbocultural regime (carbian period).
After human
beings appeared on the evolutionary scene, each energy revolution was
influenced by a 'cultural trigger' or signal:
For
the pyro-energy revolution the trigger was the origin of the human species.
The
agro-energy revolution was triggered by the ‘Symbolisational Signal’.
The
current carbo-energy revolution was triggered by the ‘Quantificational
Signal’.
The
next energy revolution of the future may be triggered by the ‘Macroscopical
Signal’.
These terms
will be explained in future posts, as we take a brief look at each of the
energy regimes. Let us begin with the thermophilic energy regime here.
As mentioned
in Part 53, life appeared
on Earth during the thermophilic regime. It originated through the emergence of
heat-loving or thermophile organisms. They were the ecologically dominant
organisms in that period; hence the term ‘thermophilic energy regime’ for the
energy regime engendered by them. They have been called ‘hyperthermophiles’ because
they were ‘hard-nosed heat lovers’.
This energy
regime also saw the emergence and establishment of a metabolism mechanism for
the supply of energy, with ATP as the principal cellular energy currency (Smil1999). The
hyperthermophiles used nucleotides for synthesizing DNA, and amino acids for
synthesizing proteins. During this energy regime there was practically no
oxygen in the atmosphere of the Earth, although there was plenty of carbon
dioxide.
For higher and
higher complexity to emerge, there must be an energy gradient from a local
energy source to an energy sink, and there must be a energy-dissipating
pathway. For the thermophilic energy regime:
Energy
source:
Primordial heat from the accretion events during the formation of the planet
Earth.
Energy
sink:
The cold atmosphere above the seas.
Energy-dissipating
pathways:
Chemical evolution, autocatalytic processes/metabolism.
Chief
drivers:
The hyperthermophiles.
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