Title: Notes
1 SPI 0807.5.5 Fossils
Notes
DEC 2012
- What Are Fossils?
- The preserved physical remains of deceased
organisms that are at least 10,000 years old - NOTE Most organisms do not become fossils when
they die - NOTE The formation of fossils is a rare event
- How Are Fossils Formed?
- Watch this amusing video Link Video How
Fossils Are Made
PRESS THE RIGHT-ARROW BUTTON ON YOUR KEYBOARD TO
GET STARTED! ?
8 Types of Fossils 8 Types of Fossils
A) Fossils In Rocks E) Frozen Fossils
B) Fossils In Amber F) Trace Fossils
C) Petrified Fossils G) Mold/Cast Fossils
D) Fossils In Asphalt H) Index Fossils
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2 SPI 0807.5.5 Fossils
Notes
Science
- A) Fossils In Rocks
- Found in sedimentary rock
- An organism died was covered with mud, dirt,
sand, ash, etc. - Later the mud, dirt, sand, or ash became
sedimentary rock
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3 SPI 0807.5.5 Fossils
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Science
- B) Fossils In Amber
- Tree sap fell on a small organism, enclosed it,
killed it - Over time the sap hardened into amber
- The amber became covered with mud, dirt, sand,
ash, etc.
Example Insects In Amber
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4 SPI 0807.5.5 Fossils
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Science
(Also known as petrifaction)
- C) Petrified Fossils
- Organism died- then was covered with mud, dirt,
sand, ash, etc. - The structure of the organism was replaced with
minerals
Sometimes when wood is buried, groundwater will
flow through the sediment and deposit minerals in
the cells of the wood.
The wood rots away the minerals remain in the
shape of the tree.
Example Petrified Wood
Example Petrified Wood
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5 SPI 0807.5.5 Fossils
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Science
- D) Fossils In Asphalt
- Animals fell into tar pits, were trapped, and
died - The asphalt hardened preserving skeletons,
shells, teeth, etc.
Saber Tooth Tiger Fossil (From La Brea Tar
Pits, California)
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6 SPI 0807.5.5 Fossils
Notes
Science
- E) Frozen Fossils
- Animals died in a cold climate region and were
frozen - The cold temperatures preserved both soft and
hard parts - Many mammoths became frozen during the last ice
age
Frozen Baby Mammoth (From Siberia,
Russia) Approx. 42,000 yrs old
Frozen Baby Mammoth (From Siberia,
Russia) Approx 40, 000 yrs old
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7 SPI 0807.5.5 Fossils
Notes
Science
- F) Trace Fossils
- Are impressions or traces left by plants and
animals - Can be simple tunnels or burrows in the mud
- Can be footprints or imprints in the mud etc.
(Also called ichnofossils)
Trace Fossil Imprint Of A Fish
Trace Fossil Dinosaur footprints
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8 SPI 0807.5.5 Fossils
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Science
- G) Mold/Cast Fossils
- In sediment, ground water may dissolve shells,
leaving a shape called a mold - Sometimes the shell dissolves and is replaced by
minerals, leaving behind a mineral cast of the
fossil
Mold Fossil
Cast Fossil
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9 SPI 0807.5.5 Fossils
Notes
Science
- H) Index Fossils
- A way to relatively date rocks
- Some fossils are commonly found at certain strata
levels across large geographic areas
(A.K.A. relative dating)
we call these index fossils
Example Trilobite fossils
Example Ammonite fossils
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10 SPI 0807.5.5 Fossils
Notes
Science
- Sedimentary rock and fossils
- deeper layers are older than layers above it.
- Example See three layers belowLayer A, Layer B,
and Layer C - Layer C is older than layer B.
- So fossils in deeper layers are older than
fossils above it.
called the law of superposition
B is older than A
So fossil one is older than fossil two
Layer A
3
Layer B
2
Layer C
1
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