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DO NOW

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DO 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. – PowerPoint PPT presentation

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Title: DO NOW


1
DO 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.

2
Paleontology
3
What similarities are exhibited by these horses?
What differences?
4
Fossils, defined
  • The remains or impression of a prehistoric
    organism preserved in petrified form or as a mold
    or cast in rock.

5
Paleontology 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?
7
Dating 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?).

9
Lets model decay!
  • Fossil a rock of MMs

10
What do you understand from this diagram? How
does half life apply?
11
So, if you have a fossil (or rock surrounding
it), how can you know how old it is?
  • Title a new page Carbon 14 Dating

12
No 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

13
Try 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?

14
Isotopes 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.
15
Your 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!)
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