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The Origin and
Evolution of Life on
Earth
When did life begin?
 What is it that we have to obtain to produce
a living cell?
 A living cell is capable of acquiring all the resources
it needs from its surroundings and reproducing
itself.
 The first cell had to be free-living; that is, it could
not depend on other cells for its survival because
other cells did not exist
When did life begin?
 Stromatolites (3.5 bill. Yr)
 Rocks with distinctive layer
structure
 Layers of microbes and
sediment
 Top layer uses
photosynthesis
 Lower layers use top layer’s
by products
 Microfossils dating to
3.5 billion years ago
 Difficult to distinguish
from mineral
structures
 Analysis shows that
some structures
contain organic
carbon
-found in at least 3 sites
 Evidence in metamorphic
rocks that life existed 3.85
billions years ago
 Low C12/C13 fraction in
rock layers suggests life
 Biological processes prefer
C12 to C13
When did life begin?
 Rocks before ~4 billion years old are rare and hard
to find
 Time of heavy bombardment ended about 3.8-4.0
billion years ago
 Last devastating impact between 4.2-3.9 bill. yrs. ago
 Evidence suggests life as long as 3.85 billion years
ago and definitely at 3.5 billion years ago
 Life rose and dominated the planet between 100-
500 million years
Living Fossils
 DNA used as living fossil
 The more alike the DNA sequence between species,
the more recent their divergence and extinction of
their common ancestor
 Bacteria and Archaea : genetic material NOT separated
from rest of cell
 Eukarya: DNA separated from rest of cell by membrane
 Extremophiles (live near deep-sea vents or in hot springs)
closest to root of tree of life
Where did life begin?
 Land is unlikely
 No O2, no ozone: UV destroys molecular bonds
 Shallow ponds
 Once favored, full of organic material
 When evaporated, organic chemical concentration
increases making it easier to combine complex
molecules leading to life
 Current experiments indicate lack of chemical energy
sufficient to support life
 Deep-sea vents/hot springs
 DNA evidence suggests that early organisms survived
in conditions similar to deep-sea vents
 Plenty of chemical energy available
How did life begin?
 Simplest organisms today and those dated 3.5 billion
years ago are remarkable advanced
 What are the natural chemical processes that could
have led to life?
 Assumptions
 Life began under chemical conditions of early Earth
 Life did not migrate to Earth
Organic Chemistry on Early Earth
 In 1920’s, scientists hypothesized that the chemicals
in the early atmosphere, fueled by sunlight, would
spontaneously create organic molecules
 Tested by Miller-Urey experiment 1950’s
Miller-Urey Experiment
 First flask partially filled with water and heated to
produce water vapor (sea)
 Water vapor was moved to a second flask where
methane and ammonia vapor was added
(atmosphere)
 Electric sparks (lightening) in second flask was
energy source for chemical reactions
 Below second flask, water vapor cooled (rain) and
recycled to first flask (sea)
 Result: turned brown with amino acids and other
complex organic molecules
Sources of Organic Molecules
 Chemical reactions in atmosphere
 Lab experiments show this is likely
 Organic material brought by impacts
 Chemical analysis of comets and carbonaceous chondrites
show that they have organic molecules
 Chemical reactions near deep-sea vents
 Heat from undersea volcano can fuel chemical reactions
between water and minerals
Transition from chemistry to biology
 Organic molecules are building blocks of life
 Low probability of forming life even if repeated
several times
 Intermediate steps of high probability are
necessary
Search for Self-Replicating Molecule
 Work backward from organisms that live today
 DNA is double-stranded = complicated
 RNA obvious candidate, more simple than DNA
 Hereditary information
 Can serve as template for replication
 Can act as an enzymes
RNA World Hypothesis
 Problem: RNA and DNA require enzymes to
replicate
 In 1980’s determined that RNA might catalyze their
own replication instead of other enzymes
 Early Earth was an RNA-world
RNA World Hypothesis
 On Early Earth, short strands of RNA-like
molecules were produced spontaneously partially
or completely
 RNA-like molecules that could replicate faster
with less errors soon dominated population
 Copying errors introduced mutations, ensuring
the production of many variations of successful
molecules
 Allowed molecular evolution to continue
 RNA-world gave way to DNA-world
 DNA less prone to copying errors
 DNA more flexible hereditary material
 RNA kept some of its original functions
Assembling Complex Organic Molecules
 Organic soup was too dilute to favor the creation of
complex organic molecules
 Lab experiment with possible solution: When hot
sand, clay or rock is placed in dilute organic
solution, complex molecules self-assemble
 Organic molecules stick to surface of clay
 Increases density and likelihood of reactions
 Strands of RNA up to 100 bases have been produced this
way
Early Cell-like Structures
 Advantages to
enclosing enzymes
with RNA molecules
 Close proximity
increases rate of
reactions between
them
 Isolate contents from
outside world
Panspermia?
 Panspermia = life originated elsewhere and migrated
to Earth
 Life began in rock, then kicked off the planet by an
impact
 Support: organic material is everywhere, and some
bacteria can withstand large amounts of radiation
and go dormant under low atmospheric conditions
Panspermia
 Martian meteorites
 Both have possible
fossil evidence of life on
Mars
 Evidence of microfossil
nanobacteria
 ALH1008
Living cyanobacteria
Microfossils in carbonaceous chondrites
Early Evolution and Rise of O2
 First organisms had simple metabolism
 Atmosphere was O2 free, must have been anaerobic
 Probably chemoheterotrophs
 Obtained nutrients from organic material
 Obtained nutrients from inorganic material
 Modern archaea appear to be close to the root of the tree of life
 Obtaining energy from chemical reactions involving hydrogen,
sulfur and iron compounds (all abundant on early Earth)
Early Evolution
 Natural selection probably resulted in rapid
diversification
 Modern DNA has enzymes that reduce the rate of
mutations
 RNA is not so lucky, more likely to have copying
errors
 Higher mutation rate in early evolution than now
Photosynthesis
 Around 3.5 billion years ago
 Most important new metabolic process evolved
gradually
 Organisms that lived close to ocean surface
probably developed means of absorbing sunlight
(UV in particular)
 Once absorbed, developed method of turning it
into energy
 Modern organisms of purple sulfur bacteria and green
sulfur bacteria much like early photosynthetic microbes,
use H2S instead of H2O for photosynthesis
Photosynthesis
 Using water for photosynthesis developed later, perhaps
3.5 billion years ago
 First appearing in cyanobacteria (blue-green algae)
 By product of O2, released into atmosphere
 Changed the world!
Rise of O2
 Highly reactive
 Rocks 2-3 bill. Yr old called banded iron
formations, show atmosphere had <1% of current
amount of O2
 Rock evidence suggests that O2 amounts in
atmosphere began to rise about 2.0 bill. Yr ago
 Clear evidence of O2 near current levels appears
only 200 million yr ago
 Find charcoal (fossil fuel)
 Indicates enough O2 in atmosphere for fires to burn
 Rise of O2 would have created a crisis for life
WHERE DID EARTH GET ITS WATER?
 Where did Earth’s Water come from?
 The origin of our planet’s water is an intricate story
stretching back some 13.8 billion years to the Big Bang
 After the Big Bang, the energy that sparked the outward
swelling of space transmuted into a hot, uniform bath of
particles
 During the next three minutes, these primordial constituents
bumped and jostled, combined and recombined, yielding the
first atomic nuclei
 Which gives accurate predictions for the cosmic abundances
of the simplest nuclei—a lot of hydrogen, less helium and
trace amounts of lithium.
 what about the other essential ingredient, oxygen?
 When STARS go supernova the explosions spew these
elements into space. Oxygen and hydrogen commingle to
make H2O.
The abundance of water on Earth is an enigma.
 As the planet formed it became so hot all its
surface water would have evaporated – prompting
theories our oceans were slowly filled by collisions
with icy comets and asteroids after it cooled. Now,
a new study by planetary scientist Lydia Hallis of
the University of Glasgow and colleagues,
published in Science in November, suggests that
some of the early Earth’s water was locked away in
molten rock and later resurfaced.

MCQ’s
More and more research suggests that asteroids delivered at least some of Earth's
water.
 Who Brought Water To Earth?
 Comets, trans-Neptunian objects
or water-rich meteoroids (protoplanets)
from the outer reaches of the asteroid belt
colliding with Earth may have brought
water to the world's oceans
MCQ’s
Meteorite EET 83309 contains tiny fragments of opal, a material that requires water to
form.
Early Eukaryotes
 Fossil evidence dates to 2.1 bill. Yr ago
 Dates to when O2 rising in atmosphere
 DNA evidence suggests that prokaryotes and
eukaryotes separated from common ancestor
much earlier
 O2 played a key role in eukaryote evolution
 Cells can produce energy more efficiently using aerobic
metabolism than anaerobic metabolism
 Adaptations of aerobic organisms could develop
adaptations that required more energy that would be
available for anaerobic organisms
The Cambrian Explosion
 Animal branch of the tree of life
 Different classifications based on body plan
 All known body plans made appearance in fossil
record in a time span of 40 million years
 <1% of Earth’s age
 Animal diversity began 545 mill. Yr ago
Colonization of Land
 Life flourished where liquid water exist
 Life on land was more complicated
 Had to develop means of collecting solar energy above ground
and nutrients below
 Life in shallow ponds or edges of lakes
 Water evaporates
 Natural selection favored that which could withstand periods
of drought
Colonization of Land
 DNA evidence suggests that plants evolved from
an algae
 It took only 75 mill. Yrs for animals to follow
plants out of water
Mass Extinctions
Mass Extinctions
 Possible Causes
 Impacts
 Impact sites found for K-T boundary
 Suspected for Permian extinction 245 mill yr ago
 Active volcanism
 Climate change
 External influence for copying errors
 Increase in solar particles or radiation hitting surface
 Local supernova
MCQ’s
 Which of the following hypothesis is best
supported by the Miller-Urea experiment?
 Choose any one
i. All Living things have extraterrestrial origins
ii. Early Earth’s atmosphere was able to spontaneously
synthesize DNA
iii. The molecules necessary for life could have formed in early
earth conditions
iv. Life was generated through the use of self replicating proteins
 Which of the following do scientists believe was
the first genetic material to develop on Earth ?
 Choose any one
i. Polypeptide chains
ii. Mitochondrial DNA
iii. Single stranded DNA
iv. Autocatalytic RNA
MCQ’s
 Which of the following do scientists believe was
NOT part of early Earth’s atmosphere ?
 Choose any one
i. Nitrogen
ii. Oxygen
iii. Methane
iv. Carbon dioxide
MCQ’s
 Among the scientists, who came first ?
 Choose any one
i. DNA
ii. Proteins
iii. RNA
iv. Amino acids
MCQ’s
 RNA likely played an important role in life’s
origins because it:
 Choose any one
i. Carries amino acids
ii. Is the best defensive molecules
iii. Increases temperature of vents
iv. Can replicate itself
MCQ’s
 What is the main functional difference between
RNA and DNA :
 Choose any one
i. RNA acts on molecules: DNA stores information
ii. RNA carries information: DNA acts on other molecules
iii. RNA carries information and acts on molecules: DNA stores
information
iv. There is no difference
MCQ’s

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Origin of Life

  • 1. The Origin and Evolution of Life on Earth
  • 2.
  • 3. When did life begin?  What is it that we have to obtain to produce a living cell?  A living cell is capable of acquiring all the resources it needs from its surroundings and reproducing itself.  The first cell had to be free-living; that is, it could not depend on other cells for its survival because other cells did not exist
  • 4. When did life begin?  Stromatolites (3.5 bill. Yr)  Rocks with distinctive layer structure  Layers of microbes and sediment  Top layer uses photosynthesis  Lower layers use top layer’s by products
  • 5.  Microfossils dating to 3.5 billion years ago  Difficult to distinguish from mineral structures  Analysis shows that some structures contain organic carbon -found in at least 3 sites
  • 6.  Evidence in metamorphic rocks that life existed 3.85 billions years ago  Low C12/C13 fraction in rock layers suggests life  Biological processes prefer C12 to C13
  • 7. When did life begin?  Rocks before ~4 billion years old are rare and hard to find  Time of heavy bombardment ended about 3.8-4.0 billion years ago  Last devastating impact between 4.2-3.9 bill. yrs. ago  Evidence suggests life as long as 3.85 billion years ago and definitely at 3.5 billion years ago  Life rose and dominated the planet between 100- 500 million years
  • 8. Living Fossils  DNA used as living fossil  The more alike the DNA sequence between species, the more recent their divergence and extinction of their common ancestor
  • 9.  Bacteria and Archaea : genetic material NOT separated from rest of cell  Eukarya: DNA separated from rest of cell by membrane  Extremophiles (live near deep-sea vents or in hot springs) closest to root of tree of life
  • 10. Where did life begin?  Land is unlikely  No O2, no ozone: UV destroys molecular bonds  Shallow ponds  Once favored, full of organic material  When evaporated, organic chemical concentration increases making it easier to combine complex molecules leading to life  Current experiments indicate lack of chemical energy sufficient to support life  Deep-sea vents/hot springs  DNA evidence suggests that early organisms survived in conditions similar to deep-sea vents  Plenty of chemical energy available
  • 11. How did life begin?  Simplest organisms today and those dated 3.5 billion years ago are remarkable advanced  What are the natural chemical processes that could have led to life?  Assumptions  Life began under chemical conditions of early Earth  Life did not migrate to Earth
  • 12. Organic Chemistry on Early Earth  In 1920’s, scientists hypothesized that the chemicals in the early atmosphere, fueled by sunlight, would spontaneously create organic molecules  Tested by Miller-Urey experiment 1950’s
  • 13. Miller-Urey Experiment  First flask partially filled with water and heated to produce water vapor (sea)  Water vapor was moved to a second flask where methane and ammonia vapor was added (atmosphere)  Electric sparks (lightening) in second flask was energy source for chemical reactions  Below second flask, water vapor cooled (rain) and recycled to first flask (sea)  Result: turned brown with amino acids and other complex organic molecules
  • 14.
  • 15. Sources of Organic Molecules  Chemical reactions in atmosphere  Lab experiments show this is likely  Organic material brought by impacts  Chemical analysis of comets and carbonaceous chondrites show that they have organic molecules  Chemical reactions near deep-sea vents  Heat from undersea volcano can fuel chemical reactions between water and minerals
  • 16. Transition from chemistry to biology  Organic molecules are building blocks of life  Low probability of forming life even if repeated several times  Intermediate steps of high probability are necessary
  • 17. Search for Self-Replicating Molecule  Work backward from organisms that live today  DNA is double-stranded = complicated  RNA obvious candidate, more simple than DNA  Hereditary information  Can serve as template for replication  Can act as an enzymes
  • 18. RNA World Hypothesis  Problem: RNA and DNA require enzymes to replicate  In 1980’s determined that RNA might catalyze their own replication instead of other enzymes  Early Earth was an RNA-world
  • 19. RNA World Hypothesis  On Early Earth, short strands of RNA-like molecules were produced spontaneously partially or completely  RNA-like molecules that could replicate faster with less errors soon dominated population  Copying errors introduced mutations, ensuring the production of many variations of successful molecules  Allowed molecular evolution to continue  RNA-world gave way to DNA-world  DNA less prone to copying errors  DNA more flexible hereditary material  RNA kept some of its original functions
  • 20. Assembling Complex Organic Molecules  Organic soup was too dilute to favor the creation of complex organic molecules  Lab experiment with possible solution: When hot sand, clay or rock is placed in dilute organic solution, complex molecules self-assemble  Organic molecules stick to surface of clay  Increases density and likelihood of reactions  Strands of RNA up to 100 bases have been produced this way
  • 21. Early Cell-like Structures  Advantages to enclosing enzymes with RNA molecules  Close proximity increases rate of reactions between them  Isolate contents from outside world
  • 22. Panspermia?  Panspermia = life originated elsewhere and migrated to Earth  Life began in rock, then kicked off the planet by an impact  Support: organic material is everywhere, and some bacteria can withstand large amounts of radiation and go dormant under low atmospheric conditions
  • 23. Panspermia  Martian meteorites  Both have possible fossil evidence of life on Mars  Evidence of microfossil nanobacteria  ALH1008
  • 24. Living cyanobacteria Microfossils in carbonaceous chondrites
  • 25. Early Evolution and Rise of O2  First organisms had simple metabolism  Atmosphere was O2 free, must have been anaerobic  Probably chemoheterotrophs  Obtained nutrients from organic material  Obtained nutrients from inorganic material  Modern archaea appear to be close to the root of the tree of life  Obtaining energy from chemical reactions involving hydrogen, sulfur and iron compounds (all abundant on early Earth)
  • 26. Early Evolution  Natural selection probably resulted in rapid diversification  Modern DNA has enzymes that reduce the rate of mutations  RNA is not so lucky, more likely to have copying errors  Higher mutation rate in early evolution than now
  • 27. Photosynthesis  Around 3.5 billion years ago  Most important new metabolic process evolved gradually  Organisms that lived close to ocean surface probably developed means of absorbing sunlight (UV in particular)  Once absorbed, developed method of turning it into energy  Modern organisms of purple sulfur bacteria and green sulfur bacteria much like early photosynthetic microbes, use H2S instead of H2O for photosynthesis
  • 28. Photosynthesis  Using water for photosynthesis developed later, perhaps 3.5 billion years ago  First appearing in cyanobacteria (blue-green algae)  By product of O2, released into atmosphere  Changed the world!
  • 29. Rise of O2  Highly reactive  Rocks 2-3 bill. Yr old called banded iron formations, show atmosphere had <1% of current amount of O2  Rock evidence suggests that O2 amounts in atmosphere began to rise about 2.0 bill. Yr ago  Clear evidence of O2 near current levels appears only 200 million yr ago  Find charcoal (fossil fuel)  Indicates enough O2 in atmosphere for fires to burn  Rise of O2 would have created a crisis for life
  • 30. WHERE DID EARTH GET ITS WATER?
  • 31.  Where did Earth’s Water come from?  The origin of our planet’s water is an intricate story stretching back some 13.8 billion years to the Big Bang  After the Big Bang, the energy that sparked the outward swelling of space transmuted into a hot, uniform bath of particles  During the next three minutes, these primordial constituents bumped and jostled, combined and recombined, yielding the first atomic nuclei  Which gives accurate predictions for the cosmic abundances of the simplest nuclei—a lot of hydrogen, less helium and trace amounts of lithium.  what about the other essential ingredient, oxygen?  When STARS go supernova the explosions spew these elements into space. Oxygen and hydrogen commingle to make H2O.
  • 32. The abundance of water on Earth is an enigma.  As the planet formed it became so hot all its surface water would have evaporated – prompting theories our oceans were slowly filled by collisions with icy comets and asteroids after it cooled. Now, a new study by planetary scientist Lydia Hallis of the University of Glasgow and colleagues, published in Science in November, suggests that some of the early Earth’s water was locked away in molten rock and later resurfaced.  MCQ’s
  • 33. More and more research suggests that asteroids delivered at least some of Earth's water.
  • 34.  Who Brought Water To Earth?  Comets, trans-Neptunian objects or water-rich meteoroids (protoplanets) from the outer reaches of the asteroid belt colliding with Earth may have brought water to the world's oceans MCQ’s
  • 35. Meteorite EET 83309 contains tiny fragments of opal, a material that requires water to form.
  • 36. Early Eukaryotes  Fossil evidence dates to 2.1 bill. Yr ago  Dates to when O2 rising in atmosphere  DNA evidence suggests that prokaryotes and eukaryotes separated from common ancestor much earlier  O2 played a key role in eukaryote evolution  Cells can produce energy more efficiently using aerobic metabolism than anaerobic metabolism  Adaptations of aerobic organisms could develop adaptations that required more energy that would be available for anaerobic organisms
  • 37. The Cambrian Explosion  Animal branch of the tree of life  Different classifications based on body plan  All known body plans made appearance in fossil record in a time span of 40 million years  <1% of Earth’s age  Animal diversity began 545 mill. Yr ago
  • 38. Colonization of Land  Life flourished where liquid water exist  Life on land was more complicated  Had to develop means of collecting solar energy above ground and nutrients below  Life in shallow ponds or edges of lakes  Water evaporates  Natural selection favored that which could withstand periods of drought
  • 39. Colonization of Land  DNA evidence suggests that plants evolved from an algae  It took only 75 mill. Yrs for animals to follow plants out of water
  • 41. Mass Extinctions  Possible Causes  Impacts  Impact sites found for K-T boundary  Suspected for Permian extinction 245 mill yr ago  Active volcanism  Climate change  External influence for copying errors  Increase in solar particles or radiation hitting surface  Local supernova
  • 42. MCQ’s  Which of the following hypothesis is best supported by the Miller-Urea experiment?  Choose any one i. All Living things have extraterrestrial origins ii. Early Earth’s atmosphere was able to spontaneously synthesize DNA iii. The molecules necessary for life could have formed in early earth conditions iv. Life was generated through the use of self replicating proteins
  • 43.  Which of the following do scientists believe was the first genetic material to develop on Earth ?  Choose any one i. Polypeptide chains ii. Mitochondrial DNA iii. Single stranded DNA iv. Autocatalytic RNA MCQ’s
  • 44.  Which of the following do scientists believe was NOT part of early Earth’s atmosphere ?  Choose any one i. Nitrogen ii. Oxygen iii. Methane iv. Carbon dioxide MCQ’s
  • 45.  Among the scientists, who came first ?  Choose any one i. DNA ii. Proteins iii. RNA iv. Amino acids MCQ’s
  • 46.  RNA likely played an important role in life’s origins because it:  Choose any one i. Carries amino acids ii. Is the best defensive molecules iii. Increases temperature of vents iv. Can replicate itself MCQ’s
  • 47.  What is the main functional difference between RNA and DNA :  Choose any one i. RNA acts on molecules: DNA stores information ii. RNA carries information: DNA acts on other molecules iii. RNA carries information and acts on molecules: DNA stores information iv. There is no difference MCQ’s