11: Methods
- Page ID
- 299432
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Human Skeletal Characteristics
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How are human physical characteristics distinguished from other organisms:
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Centered foramen magnum
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V-shaped (parabolic) dental arcade; in non-human primates, it is U-shaped
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Shorter, bowl-shaped pelvis
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S-shaped vertebral column
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Longer femur with bicondylar angle, larger and lighter femoral head
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Arms shorter than legs
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Non-grasping hallux (big toe)
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Increased manual dexterity (thumb is longer)
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Reduced prognathism (flatter face)
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Reduction in size of dentition
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Fossilization
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Fossilization is a process that preserves remains or traces of a once-living organism
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Ways fossilization can occur:
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Organic material (remains) become mineralized
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Organisms become trapped in tree resin that hardens after the tree is buried (amber-preserved fossils)
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Freezing preserves remains
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Tar pits or volcanic ash preserve remains
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Imprints of animal tracks, shells, leaves, stems, or flowers become preserved
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Human Origins
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The first hominins (group consisting of modern humans, extinct human species, and all our immediate ancestors) originate in the African continent
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Several fossils have been found in the Rift Valley region, and some have been found in Sterkfontein Valley (southern Africa)
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The East African Rift Valley is a divergent plate boundary
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The African and Nubian plates are drifting apart, and ocean is forming between the plates
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Divergent plate boundaries have volcanic activity, so fossils are often better preserved in this region
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The presence of volcanic activity means that certain types of radioactive dating methods can be used on specimens here
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Sterkfontein Valley
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There is no volcanic activity here, so radioactive dating methods cannot be used
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Must use relative dating methods
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Isotopes
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Elements
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Atomic # = # protons (same # of electrons)
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Atomic weight = protons + neutrons
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Nuclei with the same atomic number but different mass numbers are isotopes
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Most elements have more than one stable isotope
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Isotopes:
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Stable isotopes - do not decay into another isotope
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Ex: Both Carbon-12 and Carbon-13 are stable isotopes
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Radioactive isotopes - decay into another isotope
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Ex: Carbon-14 is a radioactive isotope
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Radioactive decay
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Unstable atomic nucleus loses energy by emitting ionizing particles and radiation -> transforms parent isotope into daughter isotope
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Radioactive Decay
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Radiometric dating
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Measures the abundance of a naturally occurring radioactive isotope within the
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material to the abundance of its decay products (constant rate of decay)
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Isotopes – differ in the number of neutrons (some are unstable and decay over time: radioactive)
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Parent isotope -> decays into daughter isotope
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Carbon-14
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Can date fossils up to 50,000 ya (years ago)
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Potassium-argon
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Can date fossils older than 50,000 ya
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Use of volcanic rock (Rift Valley)
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Argon-argon
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useful for dating smaller samples and volcanic rock
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greater accuracy than K/Ar for small samples
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More info: https://humanorigins.si.edu/evidence/dating
Other Dating Methods
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Relative dating
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Law of superposition; stratigraphy
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Comparing unknown fossils with known species (method for chronologically ordering specimens)
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Paleomagnetism
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Positions of magnetic north and south poles are interchanged
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There have been 183 reversals over the last 83 million years
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Latest occurred 780,000 years ago.
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By analyzing magnetic properties, we can determine possible age of the specimen
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Photos:
- See Google slides below:

