evolution = descent with modification - msu billings 2008/toenjes/biol...evidence for evolution ......
TRANSCRIPT
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Chapter 21:
Evidence for Evolution
I. Evolution & Darwin
II. Artificial Selection
III. Fossil Record
IV. Comparative Anatomy
V. Embryology
VI. Genetic Analysis
VII. Biogeographical Evidence
VIII. Conclusions
“Nothing in biology makes sense except in the light of evolution”
--Theodosius Dobzhansky
Evolution = descent with modification
! Macroevolution = large changes
! Microevolution = small changes
I. Evolution & Darwin
Charles Darwin:
On the Origin of Species
(mid-1800’s)
• Traveled extensively
• Galapagos Islands
– off the coast of Ecuador
• One area of focus: finches
Both rely on same mechanisms!
Primarily natural selection
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• Finches of the Galapagos
• 14 species
• Difference between them:
– Beak shape
• Seed crackers
• Cactus eaters
• “Tool users”
• Vampire
I. Evolution & Darwin
• Darwin’s idea:
– One original species has adapted to different food
sources
II. Artificial Selection
CAN selection produce major evolutionary change?
! Darwin found convincing evidence for his ideas in the results of
artificial selection
Artificial selection:
• organisms may be modified by controlled breeding
• and change drastically in short time periods!
• 3 examples…
A) Plants
!Broccoli, brussel sprouts, kale,
cabbage, & cauliflower
! All artificially selected
from Brassica oleracea
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B) Insects: Pesticide resistance
(Florida)
Agent of Natural Selection:
Pesticide called "Combat®"
– Cockroaches who like
bait: continuously killed
– Those who didn’t like
bait: survived
• Had rare, glucose
disliking mutation
– Bait now is ineffective>>
populations are resistant
II. Artificial Selection (cont.)
C) Mammals: Dogs
II. Artificial Selection (cont.)
Change can happened
over a very short
geological period if the
selection pressure is
strong!
READ 420-421
SILVER FOX
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Fossils: Preserved remains of ancient organisms
III. The Fossil Record
How to make a fossil:
! Burial in sediment
! Mineralization of organic
material
! Hardening of sediment
III. The Fossil Record
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Darwin and his contemporaries saw and knew of fossils:
! Local fossils looked like local organisms
! Progressive changes in layers
• Fossil Record
– Remains or evidence of past life
– Dating fossils
• Relative dating – old layers under new
• Absolute dating – radioactive decay
– Fossilization chancy
• Right kind of organism, in right place
• Gaps unavoidable
– Many excellent series though
• Horses, titanotheres, whales, humans
III. The Fossil Record
Organization of fossils:
a) Fossils are found in distinct layers
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b) Resemblance to modern forms oflife gradually increases withyounger fossils
c) Many fossils are of species nowextinct
Conclusions:
! Many different types of organismsin the past (some extinct)
! Change in lineages over time
Organization of fossils:
a) Fossils are found in distinct layers
Facts – Geology and Fossils
• Fossils are found in sedimentary rocks
• Many fossils represent extinct organisms
• Oldest sedimentary rocks contain no fossils, or fossils of
extremely simple organisms
– Prokaryotes (stromatolites)
• Fossil prokaryotes appear prior to fossil eukaryotes
• Colonial eukaryotes appear prior to multicellular
eukaryotes (invertebrates and plants)
• Invertebrates appear prior to vertebrates–Fish, amphibians, reptiles, mammals, and birds appear in order
• Seedless vascular plants, seeds, gymnosperms, and
angiosperms appear in order
III. The Fossil Record
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Unstable isotopes decay at a constant and predictable rate
Allows setting of absolute age on rock strata.
One conclusion: the Earth is very old ! ~4.5 billion years
READ 422
Fossil recordevidence ofevolutionarychange over time
Ancient primitiveorganisms !
Several intermediarystages
!Modern forms
How Do We Know That Evolution Has Occurred?
READ 423-425
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Copyright © 2005 Pearson Education, Inc. Publishing as Benjamin Cummings
Modern toothed whales
Ambulocetus natans
walked on land …like sea lions
swam by flexing & paddling … like otters
Pakicetus attocki
lived on land;skull had whale characteristics
Rodhocetus kasrani
reduced hind limbscould not walk;swam with up-down motionlike modern whales
Whale Evolution:
Fossil Record of Evolution
READ 422-423
Cambrian
(545-490)
Ordovician
(490-438)
Silurian
(438-408)
Devonian
(408-360)
Carboniferous
(360-280)
Permian
(280-248)
Triassic
(248-213)
Jurassic
(213-144)
Cretaceous
(144-65)
Tertiary
(65-2)
Millions of years ago
800
600
400
200
0600 500 400 300 200 100 0
Nu
mb
er
of
fam
ilie
s
Diversity over the Last 600 Million Years
III. The Fossil Record: Evidence for Mass Extinctions
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IV. Comparative Anatomy
• Organisms can be grouped (classified) by
unique anatomical characteristics
• Similar anatomy is found in organisms with
greatly divergent functions
Homologous structures
! structures that may have different appearances andfunctions, yet all derived from a common ancestor
Similar anatomy is found in organisms with
greatly divergent functions
Evolution helps us understand patterns in the diversity of life
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Vestigial structures
! No apparent purpose
! Resemble similarfunctional structures inother, closely relatedspecies
! also human appendix
Vestigial structures are Evolutionary relicts. They
present a strong argument for common ancestry.
V. Embryology and Comparative Development
Embryological stages
!All vertebrate embryos look
similar early in their
development
!evidence of common ancestry
! similar developmental
“instructions” in DNA
pig cow rabbit human
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Comparative Development Reveals
Descent from a Common Ancestor
V. Embryology and Comparative Development
VI. Genetic Analysis
• Essentially all organisms have DNA as genetic material
• With very few exceptions, all organisms use the same
genetic code
• Similarities in genes and proteins exist in predictable ways
(based on morphological similarities)
Modern technology reveals relatedness among diverseorganisms
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Molecular Record – Independent test
! Distantly related organisms are expected to accumulate a greater
number of evolutionary differences than closely related species.
VII. Biogeographical Evidence
• Islands often have unique (endemic) species
• Species on islands are most similar to those onnearest continent (or nearest island)
Species of Gallotia lizards on
the Canary Islands
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• Different continents have different species
• Modern species on any continent are most similar to
fossils on that continent
VII. Biogeographical Evidence
Evolution in Action• Darwin’s Finches – beak size
– Grant and Grant – 1970s
• Showed beak size heritable and responsive to
environmental change
• Guppies – with and without predators
• Pesticide and Antibiotic resistance
• Peppered Moths/Industrialized Melanism!
VIII. Conclusions
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VIII. Conclusions READ 416-417
Evolution – Supported by Many
Independent Lines of Evidence
!Evolution requires that all of these facts are trueand congruent with each other.
– Fossils, Order of Appearance, Relative andAbsolute Dates
– Anatomical Classification, Vestigial Structures,Homologies
– Embryology
– Biogeography
– Genetic Analysis
VIII. Conclusions
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Evolution – Both a Fact and a Theory
• That evolution has occurred (and is currently
occurring) is NOT in scientific debate now; it has been
settled.
• FACT – The biodiversity on Earth is a result of
evolution from a common ancestor.
• FACT – Evolution continues today.
• THEORY – The intricacies of evolutionary change and
mechanisms driving evolution.
VIII. Conclusions
Myths
! Evolution is “only a theory”.
– Misuse of word “theory”
– Theory of Gravity, Relativity, Cell theory,
Germ theory of disease etc.
– “Theory” in science means most certain
VIII. Conclusions
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End Evolution