Begin Earth’s Past Begin Earth’s Past 3/28/12 3/28/12 What do you know about What do you know about Fossils? Fossils?
Jan 19, 2016
Begin Earth’s PastBegin Earth’s Past3/28/12 3/28/12
What do you know about Fossils?What do you know about Fossils?
FossilsFossils are traces or remnants of past are traces or remnants of past life. Many fossils are found in rock. life. Many fossils are found in rock.
Rocks, fossils, and other natural Rocks, fossils, and other natural evidence provide information about evidence provide information about how Earth and life on Earth have how Earth and life on Earth have
changed over timechanged over time. .
original remainsoriginal remains
A fossil that is the actual body or body parts of an organism. The are 3 different substances original remains are found are the following:
1. 1. Ice- Ice preserves remains (Mammoth)
2. 2. Amber- Resin from tree hardened and preserves remains (insects)
3. 3.Tar- Pools of tar preserve remains (Saber-toothed cats)
Fossils in RocksFossils in Rocks
• These fossils are impressions or traces made of rock and provide indirect evidence that the organisms were there.
There are 4 types of fossils in rocks:
1. Mold and Cast
2. Petrified wood
3. Carbon Films
4. Trace fossils
Process and Example of Mold and Process and Example of Mold and CastCast
1. Organism dies and falls into soft sediment.
2. Over time, the sediment becomes rock and the organism decays, leaving a mold.
3. Minerals fill the mold and make a cast of the organism.
Example- Clams, snails
A mold and cast fossil is formed when minerals A mold and cast fossil is formed when minerals take the shape of a decayed organism.take the shape of a decayed organism.
Petrified WoodPetrified Wood
• The stone fossil of a tree is called petrified wood.
Process - A fallen tree an be covered with sediment. Over time, water passes through the sediments and into the trees cells. Minerals that are carried in the water take the place of the cells, producing a stone likeness of the tree.
Example- petrified forest
Petrified WoodPetrified Wood
Carbon FilmsCarbon Films
• Carbon is an element that is found in everything living.
• Process- Sometimes when dead plant or animal decays, its carbon is left behind on a visible layer.
• Example- moth 10 million years old
Carbon FilmsCarbon Films
Trace FossilsTrace Fossils
• Example of Trace fossils include preserved footprints, trails, animal holes, and even feces.
• Process of how the trace fossils are preserved is when weather changes drastically and causes weathering and erosion to occur which preserves events that occurred prior to the change.
Trace FossilsTrace Fossils
Relative AgeRelative Age
Scientists combine information about the relative and absolute ages of rocks and fossils to construct a timeline of Earth.
Scientists combine information about the relative and absolute ages of rocks and fossils to construct a timeline of Earth.
relative agerelative age
The age of an event or object in relation to other events or objects.
index fossilindex fossil
A fossil of an organism that was common, lived in many areas, and existed only during a certain span of time. Index fossils are used to help determine the age of rock layers.
absolute ageabsolute age
The actual age in years of an event or object.
half-lifehalf-life
• The length of time it takes for half of the atoms in a sample of a radioactive element to decay into atoms of another element
Sedimentary rock layers show the order in which rocks formed. The order of the layers is used to determine the relative ages of fossils found in the rock.
Radioactive dating can be used to determine the absolute age of igneous rock.