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Clues About Evolution
Section 2
Clues From
Fossils
How do fossils form?
How do fossils form?
Fossilization - a variety of complex processes
 that preserve organic remains within the
 geological record.
How do fossils form?
Fossilization - a variety of complex processes
 that preserve organic remains within the
 geological record.
It includes the following conditions:
How do fossils form?
Fossilization - a variety of complex processes
 that preserve organic remains within the
 geological record.
It includes the following conditions:

     rapid and permanent
      burial/entombment
    protecting the specimen
     from environmental or
     biological disturbance
How do fossils form?
Fossilization - a variety of complex processes
 that preserve organic remains within the
 geological record.
It includes the following conditions:

     rapid and permanent             continued sediment
      burial/entombment          accumulation as opposed to
    protecting the specimen          an eroding surface
     from environmental or      ensuring the organism remains
     biological disturbance         buried in the long-term
How do fossils form?
Fossilization - a variety of complex processes
 that preserve organic remains within the
 geological record.
It includes the following conditions:

     rapid and permanent             continued sediment
      burial/entombment          accumulation as opposed to
    protecting the specimen          an eroding surface
     from environmental or      ensuring the organism remains
     biological disturbance         buried in the long-term

       oxygen deprivation
      limiting the extent of
    decay and also biological
        activity/scavenging
How do fossils form?
Fossilization - a variety of complex processes
 that preserve organic remains within the
 geological record.
It includes the following conditions:

     rapid and permanent             continued sediment
      burial/entombment          accumulation as opposed to
    protecting the specimen          an eroding surface
     from environmental or      ensuring the organism remains
     biological disturbance         buried in the long-term

       oxygen deprivation       absence of excessive heating
      limiting the extent of          or compression
    decay and also biological   which might otherwise destroy
        activity/scavenging             the remains
How do fossils form?
How do fossils form?
      Fossil evidence is typically
     preserved within sediments
How do fossils form?
      Fossil evidence is typically
     preserved within sediments
         beneath water
How do fossils form?
      Fossil evidence is typically
     preserved within sediments
         beneath water


                      Why?
How do fossils form?
      Fossil evidence is typically
     preserved within sediments
         beneath water


                      Why?
How do fossils form?
        Fossil evidence is typically
       preserved within sediments
           beneath water


                        Why?

The conditions
 listed on the
previous slide
  occur more
   frequently
beneath water
How do fossils form?
        Fossil evidence is typically
       preserved within sediments
           beneath water


                        Why?

The conditions
 listed on the
previous slide
  occur more
   frequently
beneath water
How do fossils form?
        Fossil evidence is typically
       preserved within sediments
           beneath water


                        Why?

The conditions     The majority of
 listed on the       the Earth's
previous slide        surface is
  occur more      covered by water
   frequently          (70%+)
beneath water
How do fossils form?
        Fossil evidence is typically
       preserved within sediments
           beneath water


                        Why?

The conditions     The majority of
 listed on the       the Earth's
previous slide        surface is
  occur more      covered by water
   frequently          (70%+)
beneath water
How do fossils form?
        Fossil evidence is typically
       preserved within sediments
           beneath water


                        Why?

The conditions     The majority of     Even fossils derived
 listed on the       the Earth's       from land, including
previous slide        surface is       dinosaur bones were
  occur more      covered by water     ultimately preserved
   frequently          (70%+)              in sediments
beneath water                           deposited beneath
                                               water
How do fossils form?
How do fossils form?
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
                   How?
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
                   How?
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
                   How?




          specimens that
              undergo
          mummification
            in a cave or
               desert
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
                   How?
                           But...


          specimens that
              undergo
          mummification
            in a cave or
               desert
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
                   How?
                           But...


          specimens that
              undergo
          mummification
            in a cave or
               desert
How do fossils form?

  Fossilization can also occur on land, but is
                      rare.
                   How?
                           But...


          specimens that     In reality these examples
              undergo            are only a delay of
          mummification         decomposition rather
            in a cave or      than a lasting mode of
               desert               fossilization
A fish returns to its birth place to
             spawn.
Having spawned the fish dies and
shortly after sinks to the seafloor.
After several weeks the soft body
  tissues have mostly decayed.
Tectonic activity induces nearby
sediment to mobilize, burying the fish
             in the event.
Several months pass and all that
 remains of the buried fish is its
            skeleton.
As times passes more sediment
 accumulates above the fish and the
skeleton is gradually compressed and
           permineralized.
Over time the rock is distorted and
uplifted by geological forces associated
 with continental movement, raising it
            above sea level.
The uplifted rock is exposed to
weathering and gradually erodes away,
eventually exposing the tip of the fish's
          skull at the surface.
A paleontologist recognizes the fish by
 the small area of skull exposed and
    begins to carefully extract the
              specimen.
A Pomognathus fish from Houghton
Quarry - the skull is clearly visible, and
 what parts of the skeleton remain are
  obscured within the chalk matrix.
Types of Fossils
Mineralized Fossils
 Minerals replace wood or bone to create
 a piece of petrified wood or mineralized
 bone fossil.
Types of Fossils
Imprint Fossil
 A leaf, feather, bone or entire
 body can leave an imprint on
 sediment that later hardens to
 become rock.
Types of Fossils
Cast Fossil
 Minerals can fill in the hollows of animal
 tracks
Types of Fossils
Frozen Fossils
 The remains of an organism can be trapped
 in ice that remains frozen for thousands of
 years.
  
Types of Fossils
Fossil in Amber
 When the sticky resin of certain cone-bearing
 plants hardens over time, amber forms.
Most fossils are found in sedimentary
 rocks.
Most fossils are found in sedimentary
 rocks.
Sedimentary rocks:
 formed when layers of sand, silt, clay, or
 mud are compacted and cemented
 together, or when minerals are deposited
How Old?
Paleontologists use two basic methods,
either together or alone, to determine the
age of a fossil:
Paleontologists use two basic methods,
either together or alone, to determine the
age of a fossil:

relative dating
Paleontologists use two basic methods,
either together or alone, to determine the
age of a fossil:

relative dating
Paleontologists use two basic methods,
either together or alone, to determine the
age of a fossil:

relative dating          radiometric dating
Paleontologists use two basic methods,
either together or alone, to determine the
age of a fossil:

relative dating          radiometric dating
relative dating
based on the idea that in
relative   dating undisturbed areas, younger
                 rock layers are deposited on
                   top of older rock layers.
based on the idea that in
relative   dating undisturbed areas, younger
                 rock layers are deposited on
                   top of older rock layers.

                   provides only an estimate of
                          a fossil’s age
based on the idea that in
relative   dating undisturbed areas, younger
                 rock layers are deposited on
                   top of older rock layers.

                   provides only an estimate of
                          a fossil’s age

                        estimate is made by
                    comparing the ages of rock
                    layers above and below the
                             fossil layer
radioactive elements give
  off a steady amount of
   radiation as it slowly
changes to a nonradioactive
          element
radioactive elements give
  off a steady amount of
   radiation as it slowly
changes to a nonradioactive
          element

the age is estimated by comparing
the amount of radioactive element
with the amount of nonradioactive
        element in the rock
radioactive elements give
  off a steady amount of
   radiation as it slowly
changes to a nonradioactive
          element

the age is estimated by comparing
the amount of radioactive element
with the amount of nonradioactive
        element in the rock


   this method does not always
produce exact results, because the
  original amounts of radioactive
 element in the rock can never be
            determined
radiometric    radioactive elements give
                off a steady amount of
  dating         radiation as it slowly
              changes to a nonradioactive
                        element

              the age is estimated by comparing
              the amount of radioactive element
              with the amount of nonradioactive
                      element in the rock


                 this method does not always
              produce exact results, because the
                original amounts of radioactive
               element in the rock can never be
                          determined
Radioactive Decay
an unstable nucleus loses energy by emitting
ionizing particles and radiation.




                  Carbon 14
Radioactive Decay
an unstable nucleus loses energy by emitting
ionizing particles and radiation.




                  Carbon 14
                         6 protons
                        8 electrons
                 trace amounts on Earth
                     – less than 1 ppt
                    (0.0000000001%)
Radioactive Decay
an unstable nucleus loses energy by emitting
ionizing particles and radiation.




                  Carbon 14
                         6 protons
                        8 electrons
                 trace amounts on Earth
                     – less than 1 ppt
                    (0.0000000001%)
Radioactive Decay
an unstable nucleus loses energy by emitting
ionizing particles and radiation.




                  Carbon 14
                         6 protons
                        8 electrons
                 trace amounts on Earth
                     – less than 1 ppt
                    (0.0000000001%)
Radioactive Decay
This decay, or loss of energy, results in an
atom of one type transforming to an atom of
a different type.




                    Carbon 14
                           6 protons
                          8 electrons
                   trace amounts on Earth
                       – less than 1 ppt
                      (0.0000000001%)
Half life of carbon-14 is 5,730 ± 40 years. It can
 only accurately measure up to 60,000 years.
Half life of carbon-14 is 5,730 ± 40 years. It can
 only accurately measure up to 60,000 years.
The method of dating does not always produce exact
 results, because the original amount of radioactive
 element in the rock can never be determined for
 certain.
Fossils and Evolution
Fossils and Evolution
Fossils provide a record of organisms that
 lived in the past.
Fossils and Evolution
Fossils provide a record of organisms that
 lived in the past.
However, the fossil record is incomplete, it
 has gaps.
Fossils and Evolution
Fossils provide a record of organisms that
 lived in the past.
However, the fossil record is incomplete, it
 has gaps.
The gaps exist because most organisms do
 not become fossils.
Green Egg and Ham
 I am Sam              Would you like them
  Sam I am               Here or there?

 That Sam-I-am          I would not like them
 That Sam-I-am!         here or there.
 I do not like          I would not like them
 that Sam-I-am          anywhere.
                        I do not like
 Do you like            green eggs and ham.
 green eggs and ham     I do not like them,
                        Sam-I-am
 I do not like them,    Would you like them
 Sam-I-am.              in a house?
 I do not like          Would you like them
 green eggs and ham.    with a mouse?


                        .
Fossils and Models
Fossils and Models
Scientists can use fossils to make models that
 show what the organisms might have looked
 like.
Fossils and Models
Scientists can use fossils to make models that
 show what the organisms might have looked
 like.
From fossils, scientists can sometimes
 determine
 whether the organisms lived in family groups
  or alone
 what types of food they ate
 what kind of environment they lived in
Direct Evidence for Evolution
Direct Evidence for Evolution
Plant breeders observe evolution when
 they use cross-breeding to produce
 genetic changes in plants.
Direct Evidence for Evolution
Plant breeders observe evolution when
 they use cross-breeding to produce
 genetic changes in plants.
The development of antibiotic resistance in
 bacteria is another direct observation of
 evolution.
Direct Evidence for Evolution
Plant breeders observe evolution when
 they use cross-breeding to produce
 genetic changes in plants.
The development of antibiotic resistance in
 bacteria is another direct observation of
 evolution.
Scientists have noted similar rapid
 evolution of pesticide-resistant insect
 species.
Indirect Evidence for Evolution
Indirect Evidence for Evolution
Similarities in embryo structures
Indirect Evidence for Evolution
Similarities in embryo structures
Chemical makeup of organisms including
  DNA
  the way organisms develop into adults
Indirect Evidence for Evolution
Similarities in embryo structures
Chemical makeup of organisms including
  DNA
  the way organisms develop into adults
Indirect evidence does not provide proof of
 evolution, but it does support the idea.
Embryology
Embryology
The study of embryos and their
 development.
Embryology
The study of embryos and their
 development.
A tail and pharyngeal pouches are found at
 some point in the embryos of fish, reptiles,
 birds, and mammals.
Embryology
The study of embryos and their
 development.
A tail and pharyngeal pouches are found at
 some point in the embryos of fish, reptiles,
 birds, and mammals.
Fish develop gills, but the other organisms
 develop other structures.
Embryology
The study of embryos and their
 development.
A tail and pharyngeal pouches are found at
 some point in the embryos of fish, reptiles,
 birds, and mammals.
Fish develop gills, but the other organisms
 develop other structures.
Fish, birds, and reptiles keep their tails,
 but many mammals lose theirs.
Embryology
The study of embryos and their
 development.
A tail and pharyngeal pouches are found at
 some point in the embryos of fish, reptiles,
 birds, and mammals.
Fish develop gills, but the other organisms
 develop other structures.
Fish, birds, and reptiles keep their tails,
 but many mammals lose theirs.
These similarities suggest an evolutionary
 relationship among all vertebrate species.
Homologous Structures
Homologous Structures
Body parts that are similar in origin and
 structure are called homologous. They can
 also be similar in function.
Homologous Structures
Body parts that are similar in origin and
 structure are called homologous. They can
 also be similar in function.

They often
 indicate that
 two or more
 species share
 common
 ancestors.
Vestigial Structures
Vestigial Structures
Vestigial structures —structures that
 don’t seem to have a function.
Vestigial Structures
Vestigial structures —structures that
 don’t seem to have a function.
Vestigial structures also provide
 evidence for evolution.
Vestigial Structures
Vestigial structures —structures that
 don’t seem to have a function.
Vestigial structures also provide
 evidence for evolution.
Scientists hypothesize that vestigial
 structures are body parts that once
 functioned in an ancestor.
Vestigial Structures
Vestigial structures —structures that
 don’t seem to have a function.
Vestigial structures also provide
 evidence for evolution.
Scientists hypothesize that vestigial
 structures are body parts that once
 functioned in an ancestor.
Appendix
Our Appendix ~ Useful after
The US scientists                        This function has been made obsolete by modern,
found that the                           industrialised society; populations are now so
appendix acted as a                      dense that people pick up essential bacteria from
"good safe house" for                    each other, allowing gut organisms to regrow
bacteria essential for                   without help from the appendix, the researchers
healthy digestion, in                    said.
effect re-booting the                    But in earlier centuries, when vast tracts of land
digestive system after                   were more sparsely populated and whole regions
the host has                             could be wiped out by an epidemic of cholera, the
contracted diseases                      appendix provided survivors with a vital individual
such as amoebic                          stockpile of suitable bacteria.
dysentery or cholera,                    "The function of the appendix seems related to the
which kill off helpful                   massive amount of bacteria that populates the
germs and purge the                      human digestive system," said Bill Parker, a
gut.                                     professor of surgery and one of the scientists
                                         responsible for establishing its status as a useful

              http://www.independent.co.uk/life-style/health-and-families/health-news/the-appendix-does-have-a-use--rebooting-the-gut-396277.
DNA
DNA
Scientists compare DNA from living
 organisms to identify similarities among
 species.
DNA
Scientists compare DNA from living
 organisms to identify similarities among
 species.
Examinations of ancient DNA often
 provide additional evidence of how some
 species evolved from their extinct
 ancestors.
DNA
Scientists compare DNA from living
 organisms to identify similarities among
 species.
Examinations of ancient DNA often
 provide additional evidence of how some
 species evolved from their extinct
 ancestors.
By looking at DNA, scientists also can
 determine how closely related organisms
 are.
DNA
Scientists compare DNA from living
 organisms to identify similarities among
 species.
Examinations of ancient DNA often
 provide additional evidence of how some
 species evolved from their extinct
 ancestors.
By looking at DNA, scientists also can
 determine how closely related organisms
 are.
For example, DNA studies indicate that
 dogs are the closest relatives of bears.

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Science 6.2

  • 4. How do fossils form? Fossilization - a variety of complex processes that preserve organic remains within the geological record.
  • 5. How do fossils form? Fossilization - a variety of complex processes that preserve organic remains within the geological record. It includes the following conditions:
  • 6. How do fossils form? Fossilization - a variety of complex processes that preserve organic remains within the geological record. It includes the following conditions: rapid and permanent burial/entombment protecting the specimen from environmental or biological disturbance
  • 7. How do fossils form? Fossilization - a variety of complex processes that preserve organic remains within the geological record. It includes the following conditions: rapid and permanent continued sediment burial/entombment accumulation as opposed to protecting the specimen an eroding surface from environmental or ensuring the organism remains biological disturbance buried in the long-term
  • 8. How do fossils form? Fossilization - a variety of complex processes that preserve organic remains within the geological record. It includes the following conditions: rapid and permanent continued sediment burial/entombment accumulation as opposed to protecting the specimen an eroding surface from environmental or ensuring the organism remains biological disturbance buried in the long-term oxygen deprivation limiting the extent of decay and also biological activity/scavenging
  • 9. How do fossils form? Fossilization - a variety of complex processes that preserve organic remains within the geological record. It includes the following conditions: rapid and permanent continued sediment burial/entombment accumulation as opposed to protecting the specimen an eroding surface from environmental or ensuring the organism remains biological disturbance buried in the long-term oxygen deprivation absence of excessive heating limiting the extent of or compression decay and also biological which might otherwise destroy activity/scavenging the remains
  • 10. How do fossils form?
  • 11. How do fossils form? Fossil evidence is typically preserved within sediments
  • 12. How do fossils form? Fossil evidence is typically preserved within sediments beneath water
  • 13. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why?
  • 14. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why?
  • 15. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why? The conditions listed on the previous slide occur more frequently beneath water
  • 16. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why? The conditions listed on the previous slide occur more frequently beneath water
  • 17. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why? The conditions The majority of listed on the the Earth's previous slide surface is occur more covered by water frequently (70%+) beneath water
  • 18. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why? The conditions The majority of listed on the the Earth's previous slide surface is occur more covered by water frequently (70%+) beneath water
  • 19. How do fossils form? Fossil evidence is typically preserved within sediments beneath water Why? The conditions The majority of Even fossils derived listed on the the Earth's from land, including previous slide surface is dinosaur bones were occur more covered by water ultimately preserved frequently (70%+) in sediments beneath water deposited beneath water
  • 20. How do fossils form?
  • 21. How do fossils form?
  • 22. How do fossils form? Fossilization can also occur on land, but is rare.
  • 23. How do fossils form? Fossilization can also occur on land, but is rare. How?
  • 24. How do fossils form? Fossilization can also occur on land, but is rare. How?
  • 25. How do fossils form? Fossilization can also occur on land, but is rare. How? specimens that undergo mummification in a cave or desert
  • 26. How do fossils form? Fossilization can also occur on land, but is rare. How? But... specimens that undergo mummification in a cave or desert
  • 27. How do fossils form? Fossilization can also occur on land, but is rare. How? But... specimens that undergo mummification in a cave or desert
  • 28. How do fossils form? Fossilization can also occur on land, but is rare. How? But... specimens that In reality these examples undergo are only a delay of mummification decomposition rather in a cave or than a lasting mode of desert fossilization
  • 29. A fish returns to its birth place to spawn.
  • 30. Having spawned the fish dies and shortly after sinks to the seafloor.
  • 31. After several weeks the soft body tissues have mostly decayed.
  • 32. Tectonic activity induces nearby sediment to mobilize, burying the fish in the event.
  • 33. Several months pass and all that remains of the buried fish is its skeleton.
  • 34. As times passes more sediment accumulates above the fish and the skeleton is gradually compressed and permineralized.
  • 35. Over time the rock is distorted and uplifted by geological forces associated with continental movement, raising it above sea level.
  • 36. The uplifted rock is exposed to weathering and gradually erodes away, eventually exposing the tip of the fish's skull at the surface.
  • 37. A paleontologist recognizes the fish by the small area of skull exposed and begins to carefully extract the specimen.
  • 38. A Pomognathus fish from Houghton Quarry - the skull is clearly visible, and what parts of the skeleton remain are obscured within the chalk matrix.
  • 39. Types of Fossils Mineralized Fossils Minerals replace wood or bone to create a piece of petrified wood or mineralized bone fossil.
  • 40. Types of Fossils Imprint Fossil A leaf, feather, bone or entire body can leave an imprint on sediment that later hardens to become rock.
  • 41. Types of Fossils Cast Fossil Minerals can fill in the hollows of animal tracks
  • 42. Types of Fossils Frozen Fossils The remains of an organism can be trapped in ice that remains frozen for thousands of years.  
  • 43. Types of Fossils Fossil in Amber When the sticky resin of certain cone-bearing plants hardens over time, amber forms.
  • 44.
  • 45. Most fossils are found in sedimentary rocks.
  • 46. Most fossils are found in sedimentary rocks. Sedimentary rocks: formed when layers of sand, silt, clay, or mud are compacted and cemented together, or when minerals are deposited
  • 48.
  • 49. Paleontologists use two basic methods, either together or alone, to determine the age of a fossil:
  • 50. Paleontologists use two basic methods, either together or alone, to determine the age of a fossil: relative dating
  • 51. Paleontologists use two basic methods, either together or alone, to determine the age of a fossil: relative dating
  • 52. Paleontologists use two basic methods, either together or alone, to determine the age of a fossil: relative dating radiometric dating
  • 53. Paleontologists use two basic methods, either together or alone, to determine the age of a fossil: relative dating radiometric dating
  • 55. based on the idea that in relative dating undisturbed areas, younger rock layers are deposited on top of older rock layers.
  • 56. based on the idea that in relative dating undisturbed areas, younger rock layers are deposited on top of older rock layers. provides only an estimate of a fossil’s age
  • 57. based on the idea that in relative dating undisturbed areas, younger rock layers are deposited on top of older rock layers. provides only an estimate of a fossil’s age estimate is made by comparing the ages of rock layers above and below the fossil layer
  • 58.
  • 59. radioactive elements give off a steady amount of radiation as it slowly changes to a nonradioactive element
  • 60. radioactive elements give off a steady amount of radiation as it slowly changes to a nonradioactive element the age is estimated by comparing the amount of radioactive element with the amount of nonradioactive element in the rock
  • 61. radioactive elements give off a steady amount of radiation as it slowly changes to a nonradioactive element the age is estimated by comparing the amount of radioactive element with the amount of nonradioactive element in the rock this method does not always produce exact results, because the original amounts of radioactive element in the rock can never be determined
  • 62. radiometric radioactive elements give off a steady amount of dating radiation as it slowly changes to a nonradioactive element the age is estimated by comparing the amount of radioactive element with the amount of nonradioactive element in the rock this method does not always produce exact results, because the original amounts of radioactive element in the rock can never be determined
  • 63. Radioactive Decay an unstable nucleus loses energy by emitting ionizing particles and radiation. Carbon 14
  • 64. Radioactive Decay an unstable nucleus loses energy by emitting ionizing particles and radiation. Carbon 14 6 protons 8 electrons trace amounts on Earth – less than 1 ppt (0.0000000001%)
  • 65. Radioactive Decay an unstable nucleus loses energy by emitting ionizing particles and radiation. Carbon 14 6 protons 8 electrons trace amounts on Earth – less than 1 ppt (0.0000000001%)
  • 66. Radioactive Decay an unstable nucleus loses energy by emitting ionizing particles and radiation. Carbon 14 6 protons 8 electrons trace amounts on Earth – less than 1 ppt (0.0000000001%)
  • 67. Radioactive Decay This decay, or loss of energy, results in an atom of one type transforming to an atom of a different type. Carbon 14 6 protons 8 electrons trace amounts on Earth – less than 1 ppt (0.0000000001%)
  • 68.
  • 69. Half life of carbon-14 is 5,730 ± 40 years. It can only accurately measure up to 60,000 years.
  • 70. Half life of carbon-14 is 5,730 ± 40 years. It can only accurately measure up to 60,000 years. The method of dating does not always produce exact results, because the original amount of radioactive element in the rock can never be determined for certain.
  • 72. Fossils and Evolution Fossils provide a record of organisms that lived in the past.
  • 73. Fossils and Evolution Fossils provide a record of organisms that lived in the past. However, the fossil record is incomplete, it has gaps.
  • 74. Fossils and Evolution Fossils provide a record of organisms that lived in the past. However, the fossil record is incomplete, it has gaps. The gaps exist because most organisms do not become fossils.
  • 75. Green Egg and Ham  I am Sam  Would you like them Sam I am Here or there? That Sam-I-am I would not like them That Sam-I-am! here or there. I do not like I would not like them that Sam-I-am anywhere. I do not like Do you like green eggs and ham. green eggs and ham I do not like them, Sam-I-am I do not like them, Would you like them Sam-I-am. in a house? I do not like Would you like them green eggs and ham. with a mouse? .
  • 77. Fossils and Models Scientists can use fossils to make models that show what the organisms might have looked like.
  • 78. Fossils and Models Scientists can use fossils to make models that show what the organisms might have looked like. From fossils, scientists can sometimes determine whether the organisms lived in family groups or alone what types of food they ate what kind of environment they lived in
  • 79. Direct Evidence for Evolution
  • 80. Direct Evidence for Evolution Plant breeders observe evolution when they use cross-breeding to produce genetic changes in plants.
  • 81. Direct Evidence for Evolution Plant breeders observe evolution when they use cross-breeding to produce genetic changes in plants. The development of antibiotic resistance in bacteria is another direct observation of evolution.
  • 82. Direct Evidence for Evolution Plant breeders observe evolution when they use cross-breeding to produce genetic changes in plants. The development of antibiotic resistance in bacteria is another direct observation of evolution. Scientists have noted similar rapid evolution of pesticide-resistant insect species.
  • 84. Indirect Evidence for Evolution Similarities in embryo structures
  • 85. Indirect Evidence for Evolution Similarities in embryo structures Chemical makeup of organisms including DNA the way organisms develop into adults
  • 86. Indirect Evidence for Evolution Similarities in embryo structures Chemical makeup of organisms including DNA the way organisms develop into adults Indirect evidence does not provide proof of evolution, but it does support the idea.
  • 88. Embryology The study of embryos and their development.
  • 89. Embryology The study of embryos and their development. A tail and pharyngeal pouches are found at some point in the embryos of fish, reptiles, birds, and mammals.
  • 90. Embryology The study of embryos and their development. A tail and pharyngeal pouches are found at some point in the embryos of fish, reptiles, birds, and mammals. Fish develop gills, but the other organisms develop other structures.
  • 91. Embryology The study of embryos and their development. A tail and pharyngeal pouches are found at some point in the embryos of fish, reptiles, birds, and mammals. Fish develop gills, but the other organisms develop other structures. Fish, birds, and reptiles keep their tails, but many mammals lose theirs.
  • 92. Embryology The study of embryos and their development. A tail and pharyngeal pouches are found at some point in the embryos of fish, reptiles, birds, and mammals. Fish develop gills, but the other organisms develop other structures. Fish, birds, and reptiles keep their tails, but many mammals lose theirs. These similarities suggest an evolutionary relationship among all vertebrate species.
  • 93.
  • 95. Homologous Structures Body parts that are similar in origin and structure are called homologous. They can also be similar in function.
  • 96. Homologous Structures Body parts that are similar in origin and structure are called homologous. They can also be similar in function. They often indicate that two or more species share common ancestors.
  • 98. Vestigial Structures Vestigial structures —structures that don’t seem to have a function.
  • 99. Vestigial Structures Vestigial structures —structures that don’t seem to have a function. Vestigial structures also provide evidence for evolution.
  • 100. Vestigial Structures Vestigial structures —structures that don’t seem to have a function. Vestigial structures also provide evidence for evolution. Scientists hypothesize that vestigial structures are body parts that once functioned in an ancestor.
  • 101. Vestigial Structures Vestigial structures —structures that don’t seem to have a function. Vestigial structures also provide evidence for evolution. Scientists hypothesize that vestigial structures are body parts that once functioned in an ancestor. Appendix
  • 102. Our Appendix ~ Useful after The US scientists This function has been made obsolete by modern, found that the industrialised society; populations are now so appendix acted as a dense that people pick up essential bacteria from "good safe house" for each other, allowing gut organisms to regrow bacteria essential for without help from the appendix, the researchers healthy digestion, in said. effect re-booting the But in earlier centuries, when vast tracts of land digestive system after were more sparsely populated and whole regions the host has could be wiped out by an epidemic of cholera, the contracted diseases appendix provided survivors with a vital individual such as amoebic stockpile of suitable bacteria. dysentery or cholera, "The function of the appendix seems related to the which kill off helpful massive amount of bacteria that populates the germs and purge the human digestive system," said Bill Parker, a gut. professor of surgery and one of the scientists responsible for establishing its status as a useful http://www.independent.co.uk/life-style/health-and-families/health-news/the-appendix-does-have-a-use--rebooting-the-gut-396277.
  • 103. DNA
  • 104. DNA Scientists compare DNA from living organisms to identify similarities among species.
  • 105. DNA Scientists compare DNA from living organisms to identify similarities among species. Examinations of ancient DNA often provide additional evidence of how some species evolved from their extinct ancestors.
  • 106. DNA Scientists compare DNA from living organisms to identify similarities among species. Examinations of ancient DNA often provide additional evidence of how some species evolved from their extinct ancestors. By looking at DNA, scientists also can determine how closely related organisms are.
  • 107. DNA Scientists compare DNA from living organisms to identify similarities among species. Examinations of ancient DNA often provide additional evidence of how some species evolved from their extinct ancestors. By looking at DNA, scientists also can determine how closely related organisms are. For example, DNA studies indicate that dogs are the closest relatives of bears.

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