
Evolution:
Biology as a science made its move from an Arisotitlean stage to a Newtonian one with the development of the theory of evolution. Evolution is a change in the gene pool of a population over time. A gene is a hereditary unit (the microscopic `atom') that can be passed on unaltered for many generations. The gene pool is the set of all genes in a species or population (the macroscopic `object').

The English moth, Biston betularia, is a frequently cited example of observed evolution. In this moth there are two color morphs, light and dark (typica and carbonaria). H. Kettlewell found that dark moths constituted less than 2% of the population prior to 1848. Then, the frequency of the dark morph began to increase. By 1898, the 95% of the moths in Manchester and other highly industrialized areas were of the dark type, their frequency was less in rural areas. The moth population changed from mostly light colored moths to mostly dark colored moths. The moths' color was primarily determined by a single gene. So, the change in frequency of dark colored moths represented a change in the gene pool. This change was, by definition, evolution.
The increase in relative abundance of the dark type was due to natural selection. The late eighteen hundreds was the time of England's industrial revolution. Soot from factories darkened the birch trees the moths landed on. Against a sooty background, birds could see the lighter colored moths better and ate more of them. As a result, more dark moths survived until reproductive age and left offspring. The greater number of offspring left by dark moths is what caused their increase in frequency. This is an example of natural selection.
Populations evolve, not individuals. In order to understand evolution, it is necessary to view populations as a collection of individuals, each harboring a different set of traits. A single organism is never typical of an entire population unless there is no variation within that population. Individual organisms do not evolve, they retain the same genes throughout their life. When a population is evolving, the ratio of different genetic types is changing -- each individual organism within a population does not change. For example, in the previous example, the frequency of black moths increased; the moths did not turn from light to gray to dark in concert.
The process of evolution can be summarized in three sentences: Genes mutate. Individuals are selected. Populations evolve.
Thomas Malthus (1766-1834) was an English clergyman, whose writings on population growth had a strong influence on the theory of evolution by natural selection developed by Charles Darwin and Alfred Russel Wallace.

In An Essay on the Principle of Population (1797), Malthus observed that most organisms produce far more offspring than can possibly survive.

Evolution came of age as a science when Charles Darwin published "On the Origin of Species." Darwin's contributions include hypothesizing the pattern of common descent and proposing a mechanism for evolution -- natural selection.

In Darwin's theory of natural selection, new variants arise continually within populations. A small percentage of these variants cause their bearers to produce more offspring than others. These variants thrive and supplant their less productive competitors. The effect of numerous instances of selection would lead to a species being modified over time.
Selection:
Some types of organisms within a population leave more offspring than others. Over time, the frequency of the more prolific type will increase. The difference in reproductive capability is called natural selection. Natural selection is the only mechanism of adaptive evolution; it is defined as reproductive success of classes of genetic variants in the gene pool.
Natural selection can be broken down into many components, of which survival is only one. Sexual attractiveness is a very important component of selection, so much so that biologists use the term sexual selection when they talk about this subset of natural selection. Sexual selection is natural selection operating on factors that contribute to an organism's mating success.


Human Evolution:
Most of human evolution involves physical evolution, cultural evolution plays a fairly minor role until the Upper Paleolithic, 40,000 years ago. Proto-humans, hominids, were constrained and directed by the same evolutionary pressures as the other organisms they shared the ecosystem with.
Around 13 million years ago, a tree-dwelling primate developed:


The idea that man evolved a large brain first was propagated for most of the 20th century by the famous Piltdown Hoax. When, in fact, most of the physical attributes of human form (upright walking, jaw and teeth structure, pelvic and leg formation) came before brain size evolved.
Our current idea of the human family tree is shown below, whose origins lie on the continent of Africa, then spread around the globe. We also know that every living human is the direct descendent of a single Homo Sapian woman who lived in Africa 150,000 years ago (i.e. Eve) based on the matching of DNA from cellular mitochondria in people around the world. Notice that our last common ancestor with apes is Australopithecus ramidus, about 5 million years ago. Also note that many species of Australopithecus and Homo are now extinct.


At the point where early Homo Sapian developed language a new form of evolution began. Normal evolution has inherited traits being transmitted by genes. So a bird knows how to build a nest due to inherited learning. However, language now allows the passing on of information by behavioral means, the process of learning and teaching. Although we humans are genetically equipped with basic biological imperatives, our sophisticated cultural behavior must be learned and language is the symbolic mode of communication that is associated with this learning.
The basic premise here is that culture has some advantage for the survival of our ancestors, therefore natural selection favors genes responsible for such behavior. DNA information only passes from individual to individual, but cultural evolution is active, incorporates a lifetime of teaching and can be passed from one individual to many. Cultural evolution, with its global nature, becomes the distinguishing characteristic of humans.
Is there Life Out There?
Perhaps the most important discovery humankind could ever make would be the discovery of life outside the Earth.
The search for life outside the Earth actually starts on the Earth with the investigation of meteors. Carbonaceous chondrites have been found to contain organic molecules, proteins and amino acids. Interestingly, there are equal numbers of left-handed and right-handed amino acids in meteors, whereas on the Earth all amino acids are left-handed. On the Earth this is due to the fact that chemical evolution eliminated all right-handed macromolecules. Thus, amino acids in meteors must represent samples from the early stages of the Solar System before chemical evolution.
Over 800 pounds of lunar soil was returned by the Apollo missions. All of it was tested for organic materials. The only carbon found was in carbide, CH4 or CO, no amino acids or proteins. The bombardment of the lunar surface by high energy particles probably prevents the formation of macromolecules, and breaks down the ones from earlier times.
The Viking mission placed two landers on Mars, each containing three experiments to search for life:

Life in Other Solar Systems:
There is strong evidence for planets around other stars. But, for life to develop several requirements must be met:
All lifeforms on this planet are based on hydrocarbons, i.e. the carbon atom is the atomic ``glue'' in our bodies. Thus, all assumptions we make about life on other planets is based on the properties of carbon. Is it possible all our theories are wrong and that non-carbon based life is possible?
The next element of the periodic table with the same atomic properties as carbon is silicon (Si). Can hydro-silicon compounds be formed as a starting point for silicon based life forms? The answer is that hydro-silicon molecules are possible, but since the silicon atom is much heavier than the carbon atom, the atomic bonds for silicon are only stable at much lower temperatures than for carbon (on the order of -150 F). So hydro-silicon compounds might form, for example, on the moons of the Jovian worlds where the temperatures are low.
Unfortunately, low temperature also mean low chemical reaction rates. One of the requirements for complex lifeforms is a high rate of chemical reactions to supply the energy for mechanical action. It is possible to imagine primitive silicon based lifeforms, but they would not be able to compete with higher speed carbon-based lifeforms.