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The Origin and History of Life on Earth

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Title: The Origin and History of Life on Earth


1
The Origin and History of Life on Earth
  • What is Life?
  • Life is, to the best of our knowledge to date,
    unique to our planet Earth.
  • There is no simple definition of Life, except
    that life forms are able to act on their own
    behalf to support their own existence, and to
    reproduce themselves.
  • The field of science known as Biology is
    dedicated to the study of life, its component
    species, and the variations within species of
    life forms.

2
The Origin and History of Life on Earth
  • What Is a Species?
  • Species Are Groups of Interbreeding Populations
  • Appearance Can Be Misleading
  • Allopatric and sympatric speciation
  • Geographic Separation of a Population Can Lead to
    Allopatric Speciation
  • Ecological Isolation of a Population Can Lead to
    Sympatric Speciation

3
Earths Biosphere and Life Science
  • Our Earth is, to the best of our current
    knowledge, the only planet in our Solar System
    (or beyond) which supports life of any kind.
  • The time table and processes of the origin of
    life is poorly known at present, but there is
    evidence that the simplest forms of life came
    into being more than 3 billion years ago (out of
    the total of 4.6 billion years our Earth has been
    in existence).
  • Earths original atmosphere contained little or
    no molecular oxygen, which is required by current
    animal and advanced plant life forms.

4
Earths Biosphere and Life Science
  • The oxygen currently in our atmosphere is
    produced by green plant photosynthesis, which
    began with reduction of carbon dioxide by
    anaerobic bacteria, also known as cyanobacteria
    or blue-green algae, inhabiting the oceans in
    Earths early history.
  • Animal life, as we know it (which requires
    atmospheric oxygen), did not come into existence
    until about 600 million years ago.
  • An important topic of the present day is that
    humans are returning CO2 to the atmosphere at a
    faster rate than plants can reduce it to form O2,
    which can cause global warming.

5
Evolution of Oxygen Content of Earths Atmosphere
6
How Do New Species Form?
  • Changes in Chromosome Number Can Lead to
    Sympatric Speciation
  • Speciation by polyploidy
  • Change Over Time Within a Species Can Cause
    Apparent Speciation in the Fossil Record
  • Under Some Conditions, Many New Species May Arise

7
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8
How Is Reproductive Isolation Between Species
Maintained?
  • Premating Isolating Mechanisms Prevent Mating
    Between Species
  • Members of Different Species May Be Prevented
    from Meeting
  • Different Species May Occupy Different Habitats
    (Ecological isolation)
  • Different Species May Breed at Different Times
    (Temporal Isolation)
  • Different Species May Have Different Courtship
    Rituals
  • Species Differing Sexual Organs May Foil Mating
    Attempts
  • Postmating Isolating Mechanisms Limit Hybrid
    Offspring
  • One Species Sperm May Fail To Fertilize Another
    Species Eggs
  • Hybrid Offspring May Survive Poorly
  • Hybrid Offspring May Be Infertile

9
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10
What Causes Extinction?
  • Localized Distribution and Overspecialization
    make Species Vulnerable in Changing Environments
  • Very localized distribution can endanger a
    species
  • Extreme specialization places species at risk
  • Interactions with Other Organisms May Drive a
    Species to Extinction
  • Habitat Change and Destruction Are the Leading
    Causes of Extinction
  • Natural events, of geological or extraterrestrial
    origin, can cause sudden, and extremely
    catastrophic, extinctions on a large, or even
    global, basis.

11
How Did Life Begin?
  • Experiments Refuted Spontaneous Generation
  • Chemical Evolution Preceded and Gave Rise to
    Life
  • Organic Molecules Can Form Spontaneously Under
    Prebiotic Conditions
  • Organic Molecules Probably Accumulated Under
    Prebiotic Conditions
  • Organic Molecules May Have Become Concentrated
    in Tidal Pools
  • RNA May Have Been the First Self-Reproducing
    Molecule
  • Membrane-Like Microspheres May Have Enclosed
    Ribozymes

12
No growth (Broth cooled without exposure to room
air)
Growth (Broth cooled and exposed to room air)
Broth Heated to Boiling to Sterilize
  • Louis Pasteur's experiment disproving the
    spontaneous generation of microorganisms in
    broth.

13
Experimental Research on the Origin of Life
  • One of the greatest unsolved mysteries of science
    is, how did life evolve on Earth?
  • We have evidence that the oldest and simplest
    forms of life, anaerobic bacteria, may have
    formed more than 3.6 billion years ago (only 1
    billion years after Earth was created).
  • These life forms, also called cyanobacteria or
    blue-green algae, did not require oxygen to
    breathe (as do nearly all organisms inhabiting
    Earth at the present time).

14
Experimental Research on the Origin of Life
  • However, the capability of these anaerobic
    bacteria to convert atmospheric carbon dioxide
    (CO2) into oxygen (O2) and carbohydrates made
    possible the evolution of more complex life
    forms, including all animal life, that breathe
    oxygen and feed upon plant carbohydrates.
  • Since we have very few geologic records of the
    earliest periods of life on Earth, scientists
    have performed laboratory experiments with
    electric discharges (simulating lightning) in
    various mixtures of gases (simulating Earths
    earliest atmosphere) to see if the chemical
    substances required for life forms could have
    been produced by lightning early in Earths
    history.

15
  • The Experimental Apparatus of Stanley Miller
    and
  • Harold Urey
  • Life's earliest stages left no fossils, so
    evolutionary historians have pursued a strategy
    of re-creating in the laboratory the conditions
    that may have prevailed on early Earth.
  • The mixture of gases in the spark chamber
    simulates lightning in Earth's early atmosphere.

16
  • Did Microspheres Enclose the Earliest Cells?
  • Cell-like microspheres can be formed by agitating
    proteins and lipids in a liquid medium. Each
    microsphere in this photo is about 5 micrometers
    (µm) in diameter.

17
What Were the Earliest Organisms Like?
  • The First Organisms Were Anaerobic Prokaryotes
  • Some Organisms Evolved the Ability to Capture the
    Suns Energy
  • Photosynthesis Increased the Amount of Oxygen in
    the Atmosphere
  • Aerobic Metabolism Arose in Response to the
    Oxygen Crisis
  • Some Organisms Acquired Membrane-Enclosed
    Organelles
  • Mitochondria and Chloroplasts May Have Arisen
    from Engulfed Bacteria
  • Evidence for the Endosymbiont Hypothesis Is
    Strong

18
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19
  • The Relationship between Time and the Decay of
    Radioactive 40K (yellow) to 40Ar (blue)

20
  • The Probable Origin of Mitochondria and
  • Chloroplasts in Eukaryotic Cells

21
  • Symbiosis Within a Modern Cell
  • The ancestors of the chloroplasts in today's
    plant cells may have resembled Chlorella, the
    green, photosynthetic, single-celled algae living
    symbiotically within the cytoplasm of the
    Paramecium pictured here.

22
What Were the Earliest Multicellular Organisms
Like?
  • Some Algae Became Multicellular
  • Higher organisms with differentiated cells
    evolved more than 1 billion years ago
  • Animal Diversity Arose in the Precambrian Era
  • Original animal forms were primarily aquatic
    shelled invertebrates (ocean dwellers), dating
    back to the Proterozoic (pre-Cambrian) era, more
    than 600 million years ago.
  • Life Invaded the Land beginning in the Cambrian
    Era
  • Land plants began in the Cambrian era, about 500
    million years ago
  • Oxygen content of the atmosphere reached
    near-current levels in the Devonian era,
    beginning nearly 400 million years ago
  • Land animals date back to the Devonian era, about
    350 million years ago.

23
  • Diversity of Ocean Life during the Silurian
    Period
  • (a) Life characteristic of the oceans during the
    Silurian period, 440 million to 410 million years
    ago. Among the most common fossils from that time
    are (b) trilobites and their predators, such as
    nautiloids and (c) ammonites. This (d) living
    Nautilus is very similar in structure to the
    Silurian nautiloids, showing that a successful
    body plan may exist virtually unchanged for
    hundreds of millions of years.

24
How Did Life Invade the Land?
  • Some Plants Became Adapted to Life on Dry Land
  • Primitive Land Plants Retained Swimming Sperm and
    Required Water to Reproduce
  • Seed Plants Encased Sperm in Pollen Grains
  • Flowering Plants Enticed Animals to Carry Pollen
  • Some Animals Became Adapted to Life on Dry Land
  • Amphibians Evolved from Lobefin Fishes
  • Reptiles Evolved from Amphibians
  • Reptiles Gave Rise to Both Birds and Mammals

25
  • A Fish that Walks on Land
  • Some modern fishes, such as this mudskipper, walk
    on land. Like the ancient lobefin fishes that
    gave rise to amphibians, mudskippers use their
    strong pectoral fins to move across dry areas in
    their swampy habitats.

26
What Role Has Extinction Played in the History of
Life?
  • Evolutionary History Has Been Marked by Periodic
    Mass Extinctions
  • Climate Change Contributed to Mass Extinctions
  • Catastrophic Events May Have Caused the Worst
    Mass Extinctions
  • The extinction of the Dinosaurs has recently been
    determined to have been caused by an asteroid
    impact with the Earth about 65 million years ago
  • There is evidence of an even more catastrophic
    extinction event further back in Earths history
    (about 300 million years ago)

27
  • Continental Drift from Plate Tectonics
  • The continents are passengers on plates moving on
    Earth's surface as a result of plate tectonics.
  • (a) About 340 million years ago, much of what is
    now North America was positioned at the equator.
  • (b) All the plates eventually fused together into
    one gigantic landmass, which geologists call
    Pangaea.
  • (c) Gradually Pangaea broke up into Laurasia and
    Gondwanaland, which itself eventually broke up
    into West and East Gondwana.
  • (d) Further plate motion eventually resulted in
    the modern positions of the continents.

28
Evolution of the Earth with Time Continental
Drift
200 Million Years Ago
50 Million Years Ago
150 Million Years Ago
100 Million Years Ago
Present
29
How Did Humans Evolve?
  • Some Early Primate Adaptations for Life in Trees
    Were Inherited by Humans
  • Binocular Vision Provided Early Primates with
    Accurate Depth Perception
  • Early Primates Had Grasping Hands
  • A Large Brain Facilitated HandEye Coordination
    and Complex Social Interactions
  • The Oldest Hominid Fossils Are from Africa

30
How Did Humans Evolve?
  • The Earliest Australopithecines Could Stand and
    Walk Upright
  • Several Species of Australopithecus Emerged in
    Africa
  • The Genus Homo Diverged from the
    Australopithecines 2.5 Million Years Ago
  • The Evolution of Homo Was Accompanied by Advances
    in Tool Technology
  • Neanderthals Had Large Brains and Excellent Tools

31
How Did Humans Evolve?
  • Modern Humans Emerged Only 150,000 Years Ago
  • Cro-Magnons and Neanderthals Lived Side by Side
  • Several Waves of Hominids Emigrated from
    AfricaThe Evolutionary Origin of Large Brains May
    Be Related to Meat Consumption
  • The Evolutionary Origin of Human Behavior Is
    Highly Speculative
  • The Cultural Evolution of Humans Now Far Outpaces
    Biological Evolution

32
  • Representative Primates
  • The (a) tarsier, (b) lemur, and (c) lion-tail
    macaque monkey all have relatively flat faces,
    with forward-looking eyes providing binocular
    vision. All also have color vision and grasping
    hands. These features, retained from the earliest
    primates, are shared by humans.

33
  • The earliest hominid
  • This nearly complete skull of Sahelanthropus
    tchadensis, which is more than 6 million years
    old, is the oldest hominid fossil yet found.

34
  • Representative hominid tools
  • (a) Homo habilis produced only fairly crude
    chopping tools called hand axes, usually
    unchipped on one end to hold in the hand. (b)
    Homo ergaster manufactured tools that were
    typically sharp all the way around the stone at
    least some of these blades were probably tied to
    spears rather than held in the hand. (c)
    Neanderthal tools were works of art, with
    extremely sharp edges made by flaking off tiny
    bits of stone. In comparing these weapons, note
    the progressive increase in the number of flakes
    taken off the blades and the corresponding
    decrease in flake size. Smaller, more numerous
    flakes produce a sharper blade and suggest either
    more insight into tool making, more patience,
    finer control of hand movements, or perhaps all
    three.

35
Paleolithic Burial
  • This 24,000-year-old grave shows evidence that
    CroMagnon people ritualistically buried their
    dead.
  • The body was covered with a dye known as red
    ocher, then buried wearing a headdress made of
    snail shells and with a flint tool in its hand.

36
  • Competing Hypotheses for the Evolution of Homo
    Sapiens
  • The "multiregional" hypothesis suggests that
    populations of H. sapiens evolved in many regions
    simultaneously from the already widespread
    populations of H. erectus.
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