Meant as an introductory text on the concept of fossils and their importance in the formulation of evolutionary theories, this article will discuss the two main types of fossils found in the world today. It will also shed some light on some of the most common questions regarding fossils.
This article serves as the fourth installment of my series on the Theory of Evolution, of which the three first articles were:
The word Fossil comes from the Latin fossus, literally "having been dug up", and was first used by a German physician, Georgius Agricola, in 1546, to describe a wide variety of minerals, stones, and archaeological as well as paleontological objects. Before Nichola Steno's 1666 revolutionary suggestion that fossils origin were from living organisms, people did not put much importance into fossils, except, maybe, for the fact that they were pretty and neat looking things. Nowadays, the science that studies fossils is called Paleontology, and is closely related to the science of evolutionary biology in the formulation, and validation, of evolutionary theories. As a future references, I will give the Oxford dictionary definition of fossils:
- Fossils:
- the remains or impression of a prehistoric plant or animal, usually petrified while embedded in rock, amber, etc. -- Oxford Dictionary
Today, when the word fossil is thrown in the air, we often think of the tiny imprint of a 300 000 years old plant, or of a mosquito stuck in tree resin, or even of the bones of a T-rex undug from the our very own grounds in Canada. But how are those fossils really formed ? And how old can this fossil be ? Or, of course, the creationist's favorite, why do we constantly find relatively young fossils and why are there missing links ? These are the type of questions we will look at and hopefully suggest reasonable answers to.
1. How are fossils preserved
In order for a fossil to form, the dead organism must quickly be preserved, which means that it must not be in contact with any agents of decay, such as oxygen, bacteria, radiation, and erosion. This alone explains why most fossils are found in rock or amber, and why they are relatively young (We will come to that in a little while). Thus, in order to be preserved, the dead organism must find itself in mud, which will later dries and becomes rock, or in tree resin, which eventually becomes amber.
The soil in which fossils can be found are therefore very special and are not very common. The main areas where fossils are found today form a pretty short (although increasing) list: Burgess Shale (Canada), Chengjiang (China), Liaoning Province (China), Bundenbach (Germany), Solnhofen Limestone (Germany), and a couple more sites.
You said Amber ?
As I mentioned earlier, tree resin, with time, becomes hard and is transformed in what we call Amber, which is simply a popular name for fossilized resin of botanical origin. It's molecular constituency is mainly carbon and hydrogen atoms that forms rings, which, over time, becomes hard and form this sort of hard gel (See picture). The bubbles formed in the amber fossils are due to other life captured such as bacteria and fungi (See picture).
The most common inclusions in Amber are usually invertebrates, although in rare some cases, tiny vertebrates such as lizards are seen. Fossil resin inclusions are predominately insects, which should be no surprise since botanical resin is an evolutionary adaptation of plants that is, in part, for protection against insects.
What about mud ?
As we mentioned earlier, for an organism to be well preserved, an oxygen-free environment is needed, which unfortunately are pretty much only present underwater. Therefore, the vast majority of the well preserved, and therefore interesting, fossils are found in rock that was once underwater. This means that most of the fossils are underwater animals, or seabirds. This explains the wealth of information on underwater animals that were alive millions of year ago, but does not account for the lack of very old fossils.
The small amount of very old fossils is explained by one of the agents of decay, the so-called erosion. This is probably one of the Paleontologists worst enemy (Seeing as oxygen is very much needed in order to survive...). The main problem is in the fact that erosion, over a long period of time, will destroy rocks, taking the fossils that are in it along with it. Thus, leaving the Earth with a relatively young crust on top. Of course, digging deeper could potentially solve this problem, but is much more expensive.
2. Dating fossils
We have so far explained why fossils are relatively young, and introduced the two main types of fossils found. But how do they date those fossils ? How can they predict that such a fossils was an animal around 4.3 million years ago, or in the case of the mosquito in the picture, about 2 million years ago ?
Relative Dating
Charles Lyell (1797 – 1875), close friend of Charles Darwin, was the scientist who first introduce the idea that recent strata could be categorised according to the number and proportion of marine shells encased within. Based on this he proposed dividing the Tertiary period into three parts, which he named the Pliocene, Miocene, and Eocene. Nowadays, this concept is used to date fossils, in a technique that is called relative dating.
Relative dating consist of dating the fossil based on the strata it was found in. Obviously, this methods has its drawbacks, since it is based on the age of the different strata and the age of what are called index fossils. They are fossils that are commonly found and have a known age (or at least range of age), for example trilobites (See picture). Thus, the dating performed using this methods are usually very quick (for a paleontologist), but fairly inaccurate and vague.
Radiometric Dating
The "more scientific" (at least commonly known) technique for dating fossils is called Radiometric Dating, which consists of calculating the ratio of naturally occurring radioactive isotopes found in igneous rocks (Note its biggest drawback - only specific type of rock can be aged this way). One of the specific methods, called Carbon Dating, is based on the half-life of Carbon-14, which is known to be 5,730 years. Obviously, because of the relatively short half-life, using this method will only enable scientist to date fossils (or objects in some cases) that are less than 60 000 years old (at which point there is a little less than 1/1024 left of the carbon isotopes). To date older fossils, the common method used is called Potassium-Argon Dating, since the half-life of Potassium 40 is 1.25 billion years.
These techniques are much more common and will enable scientist to date bones and rocks in which fossils are found. Note that the fossils themselves are never dated, it is the rock in which the fossil is found that is dated (the fossils are rocks anyways). This gives the paleontologist an idea of the age of the fossil, but not necessarily the exact age. This is why we are often presented a range of age as opposed to an exact date.
3. Conclusions
Although the fossil record plays a very important part in the formulation and the validation of the theory of evolution, it does not completely explains it. In fact, the lack of fossil evidence has often been one of the major arguments against evolution by creationists. Even in the time of Darwin, the fossil record was often used as a proof against evolution, and in a now very popular quote by Darwin's friend, Lyell argues that "the fossil record is like a book of which very few pages are preserved, and of the pages that are preserved, very few lines, of the lines that are preserved, few words, and of the words, few letters". Lyell was also openly in agreement with Darwin's theory, but did not believe in the process of natural selection. The fossil record simply did not support the theory.
To this day, even with a surprising wealth of fossil found (The first dinosaur fossils were only found 20 years ago), some scientist believe in a very different story than natural selection: Punctuated Equilibrium. One of its founders, Stephen Jay Gould (1941 – 2002), explains why:
"The absence of fossil evidence for intermediary stages between major transitions in organic design, indeed our inability, even in our imagination, to construct functional intermediates in many cases, has been a persistent and nagging problem for gradualistic accounts of evolution."
One thing on which today's scientists agree was very well explained by the second author of the theory, Niles Eldredge (1943 - ), is that:
"The record jumps, and all the evidence shows that the record is real: the gaps we see reflect real events in life's history -- not the artifact of a poor fossil record."
Suggested Readings:
- Eldredge, N. and Tattersall, I. (1982), "The Myths of Human Evolution".
- Eldredge, N (1991). "Fossils. The Evolution and Extinction of Species," Photographs by Murray Alcosser. Abrams, New York; Australian edition: Houghton Mifflin; English edition: Aurum Press; German edition: Belser Verlag
- Ernst Mayr (1992), "Speciational Evolution or Punctuated Equilibria," from Albert Somit and Steven Peterson's The Dynamics of Evolution, New York: Cornell University Press, 1992, pp. 21-48.
- Ernst Mayr (2001), What is Evolution
Suggested Websites: