Title: DO NOW
1DO NOW
- What is stratigraphy? Write a statement about the
age of the various layers (and fossils that may
be found in those layers) you observe in the
strata model below.
2Paleontology
3What similarities are exhibited by these horses?
What differences?
4Fossils, defined
- The remains or impression of a prehistoric
organism preserved in petrified form or as a mold
or cast in rock.
5Paleontology Essays Debrief
- Fossils can be formed in many ways
- Mineral replacement
- Cooled ash/lava encasing an organism
- Arctic Ice (mammoth)
- Tree Sap (insects)
- Footprints (trace fossils)
- Bones are a typically fossilized tissue.
6- The theory of Pangea/plate tectonics suggests
that changes in land connections allowed some
living organisms to move to new areas. - This changed the environment in which certain
things lived.
How do you think the movement of plates affected
GROUPS of organisms living in Earths past?
7Dating Fossils
- There are a few ways to determine age of fossils
- Indirectly, based on where it was found
(relative dating) younger vs. older - Directly, based on the fossil itself (absolute
dating) using elements that make up the fossil - Go chemistry!
- Radiometric Dating types
- Radiocarbon Dating (fairly young organic
material uses Carbon-14) - Potassium-Argon Dating (rocks)
- Uranium-Lead Dating (realllly old rocks)
8- Radioactive Isotope Elements that undergo steady
decay and can be useful for determining the age
of objects. - Examples C-14
- Half-Life is a measurement of time involving
radioactive isotope decay - One half-life is the amount of time it takes for
half of the atoms in an object to change into
something else (which varies for each
element/substance). This change is considered to
be the decay. - Scientists can apply the concept of half life and
calculate approximate age by looking at how much
stuff is left in the object (usually a fossil,
rock, or something they are interested in dating
haha. Get it?).
9Lets model decay!
10What do you understand from this diagram? How
does half life apply?
11So, if you have a fossil (or rock surrounding
it), how can you know how old it is?
- Title a new page Carbon 14 Dating
12No problemo!
- The half life of iron-59 is 45.1 days. If you
start with a 36g sample, how long will it take
until you only have 1.13g left? How many
half-lives did that process take?
No. of Half Lives Time Amount of Sample Left
13Try this
- The half life of Iodine-131 is 8.1 days. How much
of a 20g sample will be left after 32.4 days?
What does 131 refer to?
14Isotopes Commonly Usedfor Radiometric Dating
Isotopes Isotopes Half-life(years) Effective Dating Range(years)
Dating Sample Key Fission Product Half-life(years) Effective Dating Range(years)
Lutetium-176 Hafnium-176 37.8 billion early Earth
Uranium-238 Lead-206 4.468 billion 10 million to origin of Earth
Uranium-235 Lead-207 704 million 10 million to origin of Earth
Rubidium-87 Strontium-87 48.8 billion 10 million to origin of Earth
Potassium-40 Argon-40 1.277 billion 100,000 to origin of Earth
Carbon-14 Nitrogen-14 5730 40 0-100,000
Note the half-life durations listed in the text sections of this tutorial are rounded off foruranium-238 and potassium-40.
15Your Tasks
- Continue The Half Life of MMs Lab
- Begin practice set Radioactive Isotopes, Atoms,
Radioactive Dating and Half Life - Complete at least 5 of the practice problems
- Due Monday (yes, both!)