To begin this lesson plan:
Start with a Story: (NOTE:Words in italics are those you might say to the child as you present the demo.)
Close your eyes! Imagine a world where the air is hot and humid…your skin feels sticky almost all the time. When you wake in the morning, the heavy dew wets your body as if you’ve been in the shower and as the sun heats the air, the steam rises from the earth. It’s not a very comfortable place for your human body. In fact, no humans lived at that time.
But there were many, many species of animals and plants that did live at this time and place. Dense forests grew in the tropical climate. The oxygen-rich air caused the growth of plants much larger than those on earth today. That was a good thing, too, because the giant dinosaurs, many of them herbivores, needed a lot of plants to fill their huge bellies!
There must have been some catastrophic deaths among the dinosaurs from time to time. Modern paleontologists often find the fossilized remains of dozens of different species’ bodies all in the same place. I wonder how this happened? What would have caused so many dinosaurs to die at once in the same place? We know that many mammals died in huge tar pits in an area that is modern-day Los Angeles, CA. This was long after the dinosaurs were extinct, but I wonder if something like the tar pits happened to the dinosaurs?
Finding dinosaur fossils is one way we know about these huge ancient creatures, but there are lots of other ways we learn about them; they left us clues! There are so many different clues, that paleontologists have grouped them into two different types. Today, we’re going to make some models to help us look at how fossils form and how paleontologists classify the different types of fossils.
Demonstration: Cast fossils (Type I fossils)
Imagine the animals of the Paleozoic seas. A lot of the fossils you find in our sandbox are from that time. Today, we’re going to use your fossil to discover two ways fossils form and tell us about the living animal whose body made it.
In the ocean, the sand on the bottom is constantly being churned up due to waves and currents. The Plaster of Paris is like the sand. Over time, the sand and water mix together and harden into rock. That’s what will happen in our model, too, but for a slightly different reason.
If you’re interested in learning about that, we can talk about the difference on another day. (This is a chemical study of how crystals form…so this is a chance for yet another discipline to be investigated!)
Look at photographs of fossils that are formed in this way.
Discuss the body parts that are visible (in a cast you only see the form of the outer part of the body, often a shed exoskeleton like a snake skin, as in the flexicalymene or a dissolved shell as in the clam or gastropod.)
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Geologic Time Geologic Time LineProterozoic Era