Ecology is the study of the relationships between living organisms and the interactions between them and their environment.
Scientists have organized living organisms into several levels: individual, species, population, community, ecosystem, biome and biosphere. Understanding the interactions that living organisms of the same or different species have with one another and with their habitat makes it easier to grasp the impacts that human activity can have on the biosphere as a whole.
Emergence of Life on Earth
Aristotle (384 – 322 BCE) believed that animals came from other identical animals, but that they could also come from inert (non-living) matter. This theory was taught until the 17th century.
In 1862, Louis Pasteur made a surprising discovery that refuted the spontaneous generation theory. He proved that life could only come from another life form. At that time, no scientist could explain how life began. They had no understanding of evolution or even time, so they believed in spontaneous generation.
Like Pasteur, Charles Darwin claimed that life did not emerge spontaneously. Living things descended from each other through the generations. It became clear that changes could occur over long periods of time. The concept of evolution was developed.
See the concept sheet on Darwin and Natural Selection for more details.
Many hypotheses have been proposed to explain the origin of life. Panspermia is one of them. This hypothesis suggests that bacteria was brought to Earth by meteorites or cosmic dust, eventually giving rise, through evolution, to all the currently known living species.
This hypothesis is very common in some communities. It proposes that a random chemical combination of atoms present in sufficient proportions may have generated new substances from which life originated. This event never happened again, which explains why there is only one origin of life.
From the Big Bang to the Primordial Soup
Formation of the Universe
The Big Bang theory maintains that, 13.7 billion years ago, a very hot and dense environment grew from a single point to form the Universe.
The expansion and cooling of the generated mass created quarks, which then assembled into protons and neutrons. The first atoms appeared (hydrogen and helium).
Formation of the Solar System
The clouds of gas and cosmic dust created from the Big Bang eventually agglomerated into a mass, which contracted as it rotated around its own axis. As a result, our solar system appeared as a mass (called a protostar) and developed within one of the many galaxies being formed.
A wide variety of chemical compounds then appeared after the solar system had formed.
Formation of the Sun-Earth System
During the formation of the solar system, a proto-Sun emerged. Its core contained large amounts of hydrogen (H), oxygen (O), nitrogen (N) and carbon (C), and was surrounded by an atmosphere composed of hydrogen.
Elements from the centre of the proto-Sun combine with atmospheric hydrogen to form more complex chemical compounds: CH4 (methane), NH3 (ammonia) and H2O (water vapour).
Rotating matter came together to form the Earth, which would have been in a degassing period, emitting gases such as H2O, CO2 and H2S, as a result of certain phenomena such as volcanism.
Development of the Primitive Atmosphere
Soviet biochemist Alexander Oparin believed the primitive atmosphere of our planet was composed of an “inhospitable” mixture of methane (CH4), ammonia (NH3), water vapour (H2O), carbon dioxide (CO2) and hydrogen sulphide (H2S).
Exposed to powerful solar radiation (especially UV rays), this mixture of gases created several simple organic molecules, such as amino acids which would later form proteins. These organic molecules evolved to generate the first living molecules. We call this mixture the primordial soup.
Note: Organic molecules are formed from the following atoms: C-H-O-N.
In 1953, an American scientist named Stanley Miller performed an experiment proving the Oparin hypothesis.
Evolution of the Primordial Soup
The organic molecules accumulated in lagoons and primitive seas continued to react over hundreds of millions of years.
As they were exposed to solar energy over time, these organic molecules combined into large complex organic molecules, such as nucleic acids, proteins, sugars and fats (lipids). These were the first biomolecules (polymers, chains of monomers) to develop. DNA, the basic molecule of life, is one of these biomolecules.
In order to evolve, these molecules needed to:
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Create a protective envelope, so they could control exchanges with their environment (by osmosis and diffusion);
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Use the environment’s resources (chemical products of fermentation) to meet their nutritional and energy needs. These are referred to as heterotrophic organisms;
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Reproduce by making copies of themselves. This is the origin of the genetic code.
This started a “passive competition,” where the living organisms with the most advantages lived longer.
These organisms evolved into “proto-organisms” (more perfected), which were the ancestors of algae and bacteria.
It is important to know that the activation energy required for the first vital reactions came from molecules, such as glucose and ATP. This is known as the fermentation process.
Heterotrophs are organisms that obtain nourishment from the environment rather than creating it themselves, like autotrophs. Heterotrophs generate more and more waste in the form of carbon dioxide (CO2).
As some organisms became “hungrier” and competed for food, they started feeding on carbon dioxide. This was the beginning of photosynthesis during which oxygen is released.
Diversity among living organisms refers to the variety of strategies adopted by individuals (animals or plants, for example) in order to survive. Whether it’s a cat, a plant, an elephant or a bacterium, all life forms have one thing in common: the cell is the basic unit of all living organisms.
However, the type of movement, lifestyle and changes that individuals experience during their lives can vary from one species to another. This section introduces several strategies present in living organisms, including the evolution and classification of species.