bgast1 said:
I am interested in knowing from you guys how fossils are formed. I am not interested in fossil placement yet. Although that could be my next question, I don't know yet. Right now I want to know how they are formed. Again, please do not point me to some link. Explain it to me in your own words.
also, you do not want to read a book. Well, I am sorry, but there is NO WAY anyone is going to explain how fossils are formed here in a post to any satisfying degree. Taphonomy, the part of paleontology that addresses that question, is a large area, including lots of chemistry, sedimentology, biology and so on. So you
really should read a proper book.
But, you are lucky, you happen to have available here someone who gives courses in taphonomy. Someone willing to give you a quick fly-by of the most important aspects. Here is what I can do for you:
How fossils are formed
First, we need to get one thing clear: there are a huge number of different kinds of fossils. Not different plants and animals fossilized, but rather different way of how they became fossils. In this huge diversity, certin groups can be differentatied, for the ease of addressing. Note please that any classification will not be perfect - there will always be exceptions, fossils that do not quite fit the groups etc. That's the normal story when one tries to group things into easy-to-understnad groups.
The main groups we should distinguish are:
Body fossils
These are fossils where the actual material of the animal or plant is either still preserved, or has been dissolved and the space taken up by new material (usually either clastic sediments or crystals growing into the cavity, the latter then form a so-called pseudomorphosis into the form of the fossil).
Infills
In which the original material is gone and has not been replaced. Only the cavities within the e.g. shell are filled, usually with clastic sediment.
Un-filled cavities or
impressions or natural casts are somewhat of a variant of the last group - essentially they are what's in the rock around an infill. For plant leaves, impressions are rule, except for rare circumstances. Wood is often preserved as a body fossil, though.
There are other ways to group fossils, e.g. on whether orignial chemical material is still present or not, what kind of chemcial reactions have taken place (very similar to 'what sediment are they in) etc.
But I prefer to regard fossils based on the fossilization processes as a whole. Basically, each fossil tells a story - a story of how it got into that lump of rock. It starts with the death of the animal or plant and then goes all then way through deposition, sedimentation, checmical alteration, erosion, preparation.
I'll give you two examples that show how complex and gripping a tale it can be. let us regard what has happen to a ammonites of the genus
Dactylioceras in two places in southern Germany - two places that are less than 100km apart and are in the same time horizon (actually, the layer of rock is continuous between the two outcrops where they were found, and the character of the roch changes slowly when you follow it from one outcrop to the other).
Now, as you can see, the two look decidedly different.
OK, time now to finish this:
What ARE ammonites?
They are, simply speaking, squids with a shell around them. Closely related to
Nautilius, which still exists today. Here are a few pics:
The living animal:
The shell:
A medial cut through the shell:
You can see that the shell consists of a large outer chamber (the animal lives in this chamber) and a number of smaller chambers in the middle, connected by a thin tube (the siphon). As gthe animal grows, it adds material to the edge of the shell, then adds a new sectioning wall, cutting off part of the living chamber. Rinse and repeat. So you get this row of chambers in the middle (together called the phragmokon). The shell itself consists of inner layers made from calcium carbonate (as calcite or aragonite), mixed with a low amount of protein tht dictates how the crystals grow, and a thin outer membrane called the periostracum, which is organic and can be coloured (the calcit/aragonite layers are white or mother of pearl).
What is this arrangement good for? The phragmokon chambers are filled with gas and some (little) water. Depnding on how much gas / water is pumped in through the siphon, the animal can control the lift created by it. And thus steer up and down in the water.
When the animal dies, the shell will drift a while and slowly fill with water after the naimal's body has decomposed. Then, it sinks to the ground and may get covered by sediment. If it doesn't get covered quickly, chances are it will be utterly dissolved. but let us assume it gets covered in time.
Now, usually, the shell is tight - it has only one opening (the siphon) into the inner part and thus cannot get filled with sediment. But as soon as the tiniest hole in the middle part develops, water can stream through and sediment is carried in. A bit like a house in a desert: as soon as you have a keyhole in one door and one in another, wind can go through and bring in sand and dust. If you have only one tiny opening, nothing gets blown in.
The one hsown here at the top got filled well. Then the sediment got somewhat hardened by cementation with calcium carbonate, and later the shell got dissolved. now, the rock was compressed and the shape of the external surface, with the ribs and all, was stamped onto the infill.
Contrast with with the second pic. This same ammonite got preserved a totally different way: