HOW DO WE KNOW THE AGE OF FOSSIL?
Scientist use two methods
to determine the age of
fossils
1.Relative Dating
2. Absolute Dating
RELATIVE DATING TECHNIQUES
PRINCIPLE OF SUPERPOSITION
“In a vertical sequence, the youngest rocks are on
the top and the oldest are on the bottom.”
RELATIVE DATING TECHNIQUES
PRINCIPLE OF CROSS-CUTTING RELATIONSHIP
“A rock layer is always older than a feature that cuts
through it.”
RELATIVE DATING TECHNIQUES
PRINCIPLE OF INCLUSION
“Inclusions found in other rocks (or formations) must
be older than the rock that contain them.”
RELATIVE DATING TECHNIQUES
PRINCIPLE OF ORIGINAL HORIZONTALITY
“Sediments are deposited in nearly horizontal
layers.”
RELATIVE DATING TECHNIQUES
PRINCIPLE OF LATERAL CONTINUITY
“layers of sediment initially extend laterally in all
directions.”
CONNECTING WIDELY SEPARATED EVENTS
RELATIVE DATING TECHNIQUES
PRINCIPLE OF FAUNAL SUCCESSION
“states that groups of fossil plants and animals occur in the
geologic record in a definite and determinable order. A
period of geologic time can be recognized by its respective
fossils.”
• Determines the specific age of a fossil
• Looks at chemical Properties
• Potassium-Argon
2 TYPES
• Carbon-14 (Radiocarbon)
RADIOMETRIC TECHNIQUES
• It is based on the known and constant
rate of decay of radioactive isotopes into
their radiogenic daughter isotopes.
• Particular isotopes are suitable for
different application due to the type of
atoms present in the mineral or other
material and its approximate age
ABSOLUTE DATING TECHNIQUES
CARBON-14 DATING
• Also known as Radiocarbon dating
• Used to date organic remains
• Scientist measure the radiocarbon in the
fossil to determine its age
5,730
years
½ of
C-14
Nitrogen
5,730
years
¼ of
C-14
remain
5,730
years
1/8 of
C-14
left
Half life
of C-14
• Determine the date of death of the
organic matter in an artifact or ecofact.
ABSOLUTE DATING TECHNIQUES
POTASSIUM-ARGON DATING
• Potassium-40 is a radioactive isotope of
potassium that decayed into Argon-40.
• Scientists measure the amount of argon
in the rock to determine its age
• Argon: is not commonly incorporated into such
samples except when produced “in situ” through
radioactive decay.
• Used only for inorganic substances
(rocks and minerals)
• Used to calibrate the geometric polaity
time scale.
REFFERENCES:
 http://maps.unomaha.edu/maher/geo117/part2/117historical.html
 http://www.oldearth.org/curriculum/geology/images/Xenolith.jpg
 http://geologylearn.blogspot.com/2015/05/geologic-principles-for-dening-
relative.html
 http://www.nature.com/scitable/knowledge/library/dating-rocks-and-fossils-
using-geologic-methods-107924044
 https://www.fossilera.com/pages/dating-fossils

Fossil Dating - Relative Dating Techniques

  • 4.
    HOW DO WEKNOW THE AGE OF FOSSIL? Scientist use two methods to determine the age of fossils 1.Relative Dating 2. Absolute Dating
  • 6.
    RELATIVE DATING TECHNIQUES PRINCIPLEOF SUPERPOSITION “In a vertical sequence, the youngest rocks are on the top and the oldest are on the bottom.”
  • 7.
    RELATIVE DATING TECHNIQUES PRINCIPLEOF CROSS-CUTTING RELATIONSHIP “A rock layer is always older than a feature that cuts through it.”
  • 8.
    RELATIVE DATING TECHNIQUES PRINCIPLEOF INCLUSION “Inclusions found in other rocks (or formations) must be older than the rock that contain them.”
  • 9.
    RELATIVE DATING TECHNIQUES PRINCIPLEOF ORIGINAL HORIZONTALITY “Sediments are deposited in nearly horizontal layers.”
  • 10.
    RELATIVE DATING TECHNIQUES PRINCIPLEOF LATERAL CONTINUITY “layers of sediment initially extend laterally in all directions.” CONNECTING WIDELY SEPARATED EVENTS
  • 11.
    RELATIVE DATING TECHNIQUES PRINCIPLEOF FAUNAL SUCCESSION “states that groups of fossil plants and animals occur in the geologic record in a definite and determinable order. A period of geologic time can be recognized by its respective fossils.”
  • 13.
    • Determines thespecific age of a fossil • Looks at chemical Properties • Potassium-Argon 2 TYPES • Carbon-14 (Radiocarbon)
  • 14.
    RADIOMETRIC TECHNIQUES • Itis based on the known and constant rate of decay of radioactive isotopes into their radiogenic daughter isotopes. • Particular isotopes are suitable for different application due to the type of atoms present in the mineral or other material and its approximate age
  • 15.
    ABSOLUTE DATING TECHNIQUES CARBON-14DATING • Also known as Radiocarbon dating • Used to date organic remains • Scientist measure the radiocarbon in the fossil to determine its age 5,730 years ½ of C-14 Nitrogen 5,730 years ¼ of C-14 remain 5,730 years 1/8 of C-14 left Half life of C-14 • Determine the date of death of the organic matter in an artifact or ecofact.
  • 17.
    ABSOLUTE DATING TECHNIQUES POTASSIUM-ARGONDATING • Potassium-40 is a radioactive isotope of potassium that decayed into Argon-40. • Scientists measure the amount of argon in the rock to determine its age • Argon: is not commonly incorporated into such samples except when produced “in situ” through radioactive decay. • Used only for inorganic substances (rocks and minerals) • Used to calibrate the geometric polaity time scale.
  • 18.
    REFFERENCES:  http://maps.unomaha.edu/maher/geo117/part2/117historical.html  http://www.oldearth.org/curriculum/geology/images/Xenolith.jpg http://geologylearn.blogspot.com/2015/05/geologic-principles-for-dening- relative.html  http://www.nature.com/scitable/knowledge/library/dating-rocks-and-fossils- using-geologic-methods-107924044  https://www.fossilera.com/pages/dating-fossils