key beds, absolute dating and fossils- 21the fossil record and life the fossil record provides...
TRANSCRIPT
Key Beds, Absolute Dating and FOSSILS-
21.4
Index Fossils
Key Beds
Definition: Rock or sediment layers that can
be traced back to a very specific event in
history, and cover a wide geographic area.
http://science.discovery.com/tv-
shows/greatest-discoveries/videos/100-
greatest-discoveries-kt-boundary-
discovery.htm
Absolute Age Dating
Four ways:
Radiometric Dating
Dendochronology
Ice cores
Varves
Radiometric Dating (review)
Certain elements have radioactive properties.
That is, they lose atomic parts from their nucleus
We call this losing of parts radioactive decay
When they lose protons, the element changes to a
whole new element
When they lose neutrons, they become a different
isotope of the same element, with a new atomic mass.
The radioactive decay happens at a steady rate
So we can use these elements to determine how
long ago a rock layer was formed.
Radiometric Dating
(more review) We use half-life calculations, given the amount
of parent material and daughter material in a
sample.
A half-life is the amount of time it takes for half
the element to decay.
Absolute Dating
Dendochronology = the science of studying
tree rings to determine the age of the tree and
seasonal events
Absolute Dating – Ice Cores
Ice Cores – created by drilling hollow tube
through ice up to several kilometers thick
Drilling down through ice gives a record of
seasonal events and atmospheric events.
Ice shows seasonal changes, like tree rings do.
Summer ice has more bubbles and larger crystals
than winter ice does.
Absolute Dating – Ice Cores
Absolute Dating – Varves
Varves: bands of alternating light and dark-
colored sediments of sand, clay and silt
Rates of sedimentary deposits vary by season
(as with ice cores and tree rings)
Help study glacier melting patterns
The Fossil Record and life
The fossil record provides evidence about the history of life on Earth. The fossil record also shows that different groups of organisms have changed over time.
Evolution is the gradual change in species over long periods of time.
When geologists find fossils in rocks, they know that the rocks are about the same age as the fossils. Thus, they can infer that the same fossils found elsewhere are also of the same age.
Radiolarians
Microfossils
Unicellular organisms with hard shells that have populated the oceans since the Cambrian Period
Used by petroleum geologists to determine the age of rocks that might produce oil
Original Preservation
Original Preservation
The picture on the preceding slide is from the La Brea
Tar Pit in California. The soft parts of a mammoth
were preserved in the aforementioned Pit.
Original Preservation: PLANT AND ANIMAL
REMAINS THAT HAVE BEEN ALTERED VERY
LITTLE SINCE THE ORGANISM’S DEATH
(USUALLY SOFT TISSUE DECAYS BUT IN
ORIGINAL PRESERVATION IT DOES NOT)
Original Preservation Example
The insect is completely preserved (hard and soft parts) in
amber.
Altered Hard Parts
The soft portion decays away quickly and the hard portion (bones, shells, cell walls) can become fossils in one of two ways:
1) Mineral replacement:
a) pores in hard parts are filled in with minerals from groundwater
b) groundwater comes into contact with original hard parts mineral and replaces the material with a different mineral
2) Recrystallization:
Original mineral retains the same chemical formula although takes on a crystalline structure for greater long term stability
Molds/Casts
Mold: impression left behind in the sediment
where a shell once was
Cast: filled in mold
Trace Fossils Provide evidence of how an organism lived,
moved and obtained food
Examples: worm trails, footprints, tunneling burrows, gastroliths (rocks in dinosaur stomachs- left) and coprolites (fossilized feces- right)