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Continental Drift

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Continental Drift & Speciation – PowerPoint PPT presentation

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Title: Continental Drift


1
Continental Drift Speciation
2
Continental Drift
  • Alfred Wegener
  • In the 1930s suggested that continents were (and
    are currently) moving relative to each other and
    that at some time in the past they were joined
    together forming a super continent Pangea

3
Continental Geography
  • The eastern coast of South America and the
    western coast of Africa appear to fit nicely
    together like pieces of a puzzle

4
Paleontology Climate
  • The ranges of fossil plant and animal specimens
    of similar age appear to correlate well across
    current continental boundaries
  • Tropical fossils exist in Antarctic sediment
    suggesting that this continent has not always
    existed in its current location

5
Past Glacial Events
  • Mapping of the extent of glacial rock remains on
    the different continent suggests particular
    connections between the continents in the past

6
Plate Tectonics
  • Continental Drift was not taken seriously by the
    geological community until a mechanism that could
    explain the movement of the continents could be
    developed

7
Ruggedness of the Ocean Floor
  • Through development of sonar and more extensive
    use of submarines a picture of a rugged sea floor
    emerged (previously it was thought that the ocean
    floor was flat)
  • In fact, the Earths largest feature is the
    Mid-Atlantic Ridge running down the middle of the
    Atlantic Ocean

8
Oceanic Ridges
  • At ocean ridges new crust arises from magma
    within the Earth forcing the existing plate out
    while a new border for the plate is being made

9
Magnetic Striping
  • As new magma cools magnetic crystals within it
    line up with the magnetic poles of the Earth
  • The north end facing north and the south end
    facing south

10
  • As magma in the Earths core circulates magnetic
    or polar reversals occur
  • Our current north and south flip such that the
    magnetic crystal line up opposite of what they
    would be normally.

11
Oceanic Trenches
  • Where two plates come together one is subducted
    under the other forming a trench
  • Tension builds up in the plate laying on top
    while heat may generate magma below (Mts
    Volcanoes)

12
  • Mapping of the distribution of Earthquakes across
    the globe correlates well with places were plates
    are coming together

13
  • http//pubs.usgs.gov/publications/text/
  • Information on Continental Drift and Plate
    Tectonics

14
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15
Speciation
  • Process by which
  • a) subpopulations of one species diverge
    becoming adapted to different environments and
    reproductively isolated
  • b) descendants of a species become adapted to
    an environment different than the one in which
    it was originally adapted

16
Allopatric Speciation
  • Type of speciation in which the subpopulations
    diverge because they are separated by a
    geographic barrier

17
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18
Reproductive Isolation
  • Pre-Zygotic Mechanisms
  • 1) Temporal
  • 2) Behavioral
  • 3) Mechanical
  • 4) Ecological
  • 5) Gametic Mortality
  • Post-Zygotic Mechanisms
  • 1) Hybrid Inviability
  • 2) Hybrid Sterility
  • 3) Low Fitness Hybrids
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