Fossils - Moldy Oldies
The great
fossil mystery
Some plants and animals which lived on the Earth long
ago left clues of past life that science detectives have discovered. These
clues are called fossils. So grab your notepad and magnifying glass and
get started on the most exciting case ever. It is time to investigate
the "Great Fossil Mystery."
If rocks could talk
Fossils are the evidence of plants or animals which lived
on Earth long ago. Scientists examine this evidence to make inferences
about what happened on Earth millions of years ago. Fossils are usually
found in rocks and are the preserved remains of a once living thing. To
become a fossil, most organisms must have hard parts such as bones or
shells since the soft parts decay before they are fossilized. The plant
or animal must be buried quickly to prevent decay. It must also remain
undisturbed for a long period of time. A fossil might be the thigh bone
of a triceratops or the petrified trunk of a tree.
How do you explain it?
Sometimes a fossil is just a mark left behind by an organism
when it was alive such as a trail, a burrow, or a track. These are called
trace fossils. Dinosaur footprints are often found in the roofs of coal
mines in Carbon County. Were the dinosaurs walking upside-down? Think
about it...does this make sense? Perhaps it would be more accurate to
say that the coal formed under the material of which the dinosaur stepped.
Leave no trace...
Some rare organisms are preserved unaltered (unchanged).
This might happen when an animal falls through ice or into a tar pit.
Some insects such as mosquitos have been preserved in amber (the fossilized
sap from ancient trees). Most plants and animals that lived in the past
died without leaving a trace.
What changes must happen to allow a fossil to form?
Replacement fossils are made when water dissolves part of the dead plant or animal and washes it away. This leaves an imprint of an organism - which is kind of like a sponge filled with holes. Minerals fill in the holes and then harden to form a fossil. The fossil is the same shape and size of the original organism. Sometimes the minerals fill in each cell so perfectly, that you can see very detailed parts of the once living organism like the rings in a tree trunk. Replacement fossils can be very colorful because the minerals which fill in the holes may be different colors.
Choose one of the following activities to make your own model fossil.
| Replacement
Fossil Option |
Film Trace Option |
Mold / Cast Option |
| Animal option | Plant option | |
Materials:
Procedure:
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Materials:
Procedure:
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Materials:
Procedure:
Cast Fossil:
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