Chapter 8
Fossil - the preserved remains or traces of a living thing. Mold - the hollow space that is left. Cast - forms when dissolved minerals fill the space and harden. Index fossil- helps scientists find the age of a rock layer that may be out of order. Theory -
One theory is that 4.5 billion years ago Earth formed from a giant cloud of gas and dust. Another theory says that 3.5 billion years ago the first organism or living thing appeared. The organisms reproduced by dividing Fossils show how organisms have changed over time. Most fossils form in sedimentary rocks.
Continental drift is the theory that the continents have been slowly drifting apart for millions of years. 225 million years ago all of Earth’s landmasses were joined. This landmass is now called Pangea. It then broke into pieces- Earth’s continents.
When organisms die, they usually are eaten or decay quickly. Some remains are buried in sediment, ice, or tree sap. These remains become fossils. Some fossils are the actual hard parts of organisms. Teeth, bones, shells Some organisms or parts become petrified.
Mold is the hollow space that is left. Cast forms when dissolved minerals fill the space and harden. Mold and casts preserve the shapes of organisms. Sometimes an entire animal is preserved Example- Insects have been trapped in tree sap or mammoths buried in ice and snow.
Trace fossils are evidence of an animal’s activities. A carbon film is an extremely thin coating of carbon. Fossils tell scientists what these past organisms were like.
Sedimentary rock forms in layers. The relative age of a rock is its age compared with the ages of other rocks. This process would work if the rock layer was never disturbed. It is disturbed from earthquakes, water, and wind.
Index fossils provide a way to match rocks of the same age found in different places. The age of a rock in years is its absolute age.
Paleontology- The study of fossils.
Some types of organisms haven’t changed much through years, but many others are extinct. Fossils show what living things were like in the past and how they have changed.
The study of fossils They compare fossils with organisms living today. They study ways living things have changed.
ELEPHANTMAMMOTH
Many plants die and decay without a trace and don’t leave a fossil. Because they have no hard parts such as bones or shells. Most plant fossils that we do have are carbon films. An object is petrified when dead cells are replaced by minerals. The first plants lived in the sea. Ferns were the main type of plants for more than 175 million years. Plant fossils provide clues about past environments. Can infer the climate that existed on Earth millions of years ago.