As with his Outline of History, Wells intended The Science of Life to be read by “ordinary busy people” from all walks of life. Wells felt it was imperative that laypersons be educated about important basic biology and new developments, but he realized that the volume of scientific information was too great for most people to sift through. The amount of biological information has increased significantly since Wells wrote The Science of Life, making it even more difficult for the layperson to gain knowledge.

Examining the origins of living things helps define life and is, therefore, the area that is studied by biology.

Definitions of life are elusive because many properties of living things (for example, movement, orderliness, or energy use) also occur occasionally in “non-living” things. Wind moves, crystals grow, and fire uses energy, but we do not consider these to be alive.

Though life developed relatively late in Earth’s history, the origins of Earth and the universe are important to fully understanding it.

The universe is between 10 and 20 billion years old and began at a moment called the Big Bang. Our Sun is about 5 billion years old. The Earth, which was formed from an accumulation of cosmic dust, is about 4.6 billion years old. The early Earth, shortly after its formation about 4.6 billion years ago, was an inhospitable place that could not have supported “life” by any definition we might use today. However, 3.5 billion years ago (approximately 1 billion years after its formation), the Earth was teeming with life in the form of organisms that resemble modern-day bacteria. This development is extremely fast, especially considering that the molten Earth needed half a billion years to cool enough to form a solid rock surface.

Some biologists now think that there is evidence for life even earlier, at about 4 billion years ago.

In any case, life appeared on Earth as soon as it was possible. Most scientists now think that life arose spontaneously from non-living matter. Many religions believe that life was bestowed on non-living Earth by a deity. Some scientists suggest the panspermia hypothesis, which says that the original life on Earth arrived here from another planet. Both of these alternatives, however, ignore the question of how living matter could emerge from non-living matter.

The most fundamental, most essential property of life is a dependence on organic chemistry, a chemistry based on organic compounds (chemical compounds built around carbon).

There are four general classes of organic compounds:

1. Amino acids are the building blocks of proteins.
2. Nucleic acids include DNA and RNA.
3. Carbohydrates include sugar, starch, and cellulose (wood fiber).
4. Lipids include fats and hormones.

Organic compounds have complex properties as compared to inorganic compounds. The first step toward the origin of life must involve the formation of organic compounds from inorganic ones. However, organic compounds are generally produced only by living things. As far as we know, the early Earth was entirely inorganic.

A now-classic experiment by Stanley Miller in 1953 demonstrated that it is possible to synthesize many organic compounds under conditions simulating those thought to have prevailed on the early Earth.

For many years, scientists speculated about the possibility of spontaneously generating organic compounds. Earth’s current atmosphere is largely made up of nitrogen and oxygen. Because oxygen tends to break down organic molecules, spontaneous generation of organic compounds is impossible today. In the 1920s, Alexander Oparin and J. B. S. Haldane suggested that Earth’s early atmosphere had little oxygen, that it was composed primarily of hydrogen, methane, and ammonia. This composition would be conducive to spontaneous production of organic molecules.

Stanley Miller tried to reproduce early Earth conditions with an apparatus that used heated water in one flask (the “ocean”) and another flask (the “atmosphere”) that contained hydrogen, methane, ammonia, and water vapor. Miller also exposed the gases in the “atmosphere” to electrical energy to mimic lightning, volcanism, and ultraviolet radiation. Within a few days, Miller’s apparatus had synthesized a wide range of organic compounds, including such complex ones as amino and nucleic acids. Research following Miller’s original experiment has shown that all major classes of organic compounds can be synthesized under early Earth conditions. Miller continued his research until his death in 2007.

However, molecules synthesized this way are still rather simple compared to the compounds that make up living things.

In addition to the ability to synthesize more complex compounds, three additional things are required to create life:

1. We need to be able to make more of any compound at any time, without relying on random chemistry, which may not produce the same compound every time.
2. We need a method of combining and organizing compounds into larger functional units.
3. We need to find a way to accumulate and store energy, because living things do not rely on lightning or volcanism to power themselves.

Another characteristic of living systems is that they are organized in a hierarchical fashion, from molecules to cells to organisms to communities of species to ecosystems.

At the same time, three unifying principles that cut across all levels of organization form a useful way to look at systems as a whole. The first principle is Information and Evolution, which explores how the structure and organization of living things is encoded in the DNA molecule, how this information is transmitted and modified, and the implications of these processes for understanding life at all scales of organization.

The second principle is Development and Homeostasis which considers two related issues for understanding the workings of complex organisms: how single cells (i.e., fertilized eggs) proliferate and transform into complex, multicellular organisms and how the various parts of complex organisms remain coordinated and maintain their integrity in the face of various challenges.

The third principle is Energy and Resources, which explains how living systems obtain the energy and other materials needed to maintain their highly ordered state and the implications of these processes for understanding the organization of biology at all levels of scale. This principle is especially interesting because it dictates the structure of all levels of organization.

END PART 2

BIOLOGY THE STUDY OF LIFE:

PART 1 INTRODUCTION
PART 2 WHAT IS LIFE
PART 3 ORIGIN OF LIFE

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