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Ch.3, Sec.4 – Looking at Fossils

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Presentation on theme: "Ch.3, Sec.4 – Looking at Fossils"— Presentation transcript:

1 Ch.3, Sec.4 – Looking at Fossils
Fossilized Organisms - the remains of an organism preserved by geologic processes is called a fossil - fossils are usually found in sedimentary rock, but can be found in many types of materials - fossils found in rocks are usually made of bones or shells

2 Ch.3, Sec.4 – Looking at Fossils
- fossils (insects, frogs, lizards) have been found in amber, which is hardened tree sap - fossils can also be preserved through petrification, in which minerals replace an organism’s tissues

3 Ch.3, Sec.4 – Looking at Fossils
- fossils (woolly mammoths, saber-toothed cats) have been found in asphalt pits (evaporating oil), which can trap animals in them - the La Brea asphalt pits in Los Angeles have trapped animals for the last 38,000 years!

4 Ch.3, Sec.4 – Looking at Fossils
La Brea Asphalt Pits, Los Angeles, California

5 Ch.3, Sec.4 – Looking at Fossils
- fossils can also be preserved by frozen climates with tundra - scientists have discovered multiple woolly mammoths in the permafrost tundra of Siberia, in Russia

6 Ch.3, Sec.4 – Looking at Fossils
Other Types of Fossils - any naturally preserved evidence of animal activity is called a trace fossil - trace fossils can be tracks, burrows, or animal dung (coprolite)

7 Ch.3, Sec.4 – Looking at Fossils
- fossils can also be preserved in molds & casts - a cavity in rock where a plant or animal was buried is called a mold - a cast is an object created when sediment fills a mold and becomes rock

8 Ch.3, Sec.4 – Looking at Fossils
Using Fossils to Interpret the Past - unfortunately, the fossil record is incomplete because most organisms never became fossils or haven’t been discovered - using the fossils of plant and land animals allows scientists to reconstruct past climates - some of the oldest fossils in the world have been discovered at the Burgess Shale Formation in British Columbia, Canada

9 Ch.3, Sec.4 – Looking at Fossils
Using Fossils to Date Rocks - many fossils are only found in certain layers of rocks, so dating the rocks give us an idea of how old they are - index fossils are fossils of organisms that lived during a relatively short, well-defined geologic time span - two perfect examples of index fossils are ammonites & trilobites, which is Ohio’s state fossil Ammonites Trilobites

10 Ch.3, Sec.4 – Looking at Fossils


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