Lecture 2_Phylogenies and the History of Life (Chap 27) Spring 2010
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Transcript of Lecture 2_Phylogenies and the History of Life (Chap 27) Spring 2010
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Chapter 27
PHYLOGENIES ANDTHE HISTORY OF
LIFE
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Tools for Studying the History of Life
- Phylogenies: evolutionary histories of
groups (taxa) of organisms usually
depicted as trees.
- note, phylogenies are hypotheses.
- Fossils collection continues to grow,
transitional forms are found and
relationships are refined.
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Phylogenies as Trees
Estimates or hypotheses of the relationships amongorganisms.
Reading the tree:
Root
Branches
Nodes (forks)
Branch Tips
Outgroup
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Phylogenies as Trees
Types of phylogenies
Monophyletic group or Clade -
Paraphyletic group
Polyphyletic group
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How are they constructed?
What would you look for or compare?
Comparisons:
Phenetic based on computing a statisticshowing overall similarity among populations
Cladistic relationships among organisms based
on shared derived characteristics orsynaptomorphies
- characteristics derived from a common ancestor
Phylogenies as Trees
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Fig 27.1
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How are they constructed?
Problems:
- Characteristics that arose independently in 2 or
more distantly related groups (analogous traits or
homoplasy)
- Loss of a derived characteristic in 1 or more
closely related groups
- Lack of transitional forms
Solution: Parsimony, the most logical, simplest
explanation, involves the least amount of change.
Phylogenies as Trees
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Fossils Traces of Organisms from
the Past How are fossils formed?
- Rapid burial
- Lack of or very slow decay
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Fig 27.5
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Types ofFossils fig 27.6
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Types ofFossils Fig 27.6
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Fossils
Limitations: the formation of fossils requires
that conditions be just right. Fossils may be
formed or found preferentially according to:
Habitat sediments form routinely Composition of organism hard substances
fossilize better.
Time line ancient fossils disappear into the
earth.
Abundance more abundant, more likely to
find fossils.
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How do we determine the age of fossils? - Radiometric dating: using radioactive isotopes
to predict the age of rocks and other formations
The ages of the Earth and its organismshave been used to create Lifes Timeline,fig 26.9. - Divided into 4 major segments or eras, with
further divisions demonstrating majoradvancements, etc.
Fossils
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Fig 27.8
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Fig 27.8
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Fig 27.8
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Fig 27.8
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Cambrian Period (Paleozoic era) Significance: rapid diversification of the species.
- Multicellular organisms
- Rapid increase in size and complexity of organisms.
Fossils from China (Doushantuo formation),
Australia, Ukraine, Siberia, etc. (Ediacaran
period), and Canada (Burgess Shale fossils)
deposits are unique soft bodied animals.
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Cambrian Period
Fossil record How did this explosion of
diversity happen?
Diversity of Habitats Genetic changes
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Evolution the Process
Natural Selection
Natural selection and evolution requires genetic
change. Genetic changes:
Gene duplication multiple copies of genes
Gene expression timing and duration of
expression during development.
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Genetic Mechanisms
Newest Approach: evo-devo, evolution
and developmental studies combined.
- Correlates evolutionary history, morphologyand genetic make-up of organisms.
- The more characteristics that suggest a
relationship among organisms, the more
plausible the phylogenetic hypothesis.
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Genetic Mechanisms
Homeotic genes: direct the pattern of
development of organisms, universal.
Hypothesis: new genes = new bodies Gene duplication studies, fig 27.10
Correlate well with the hypothesis. Early
branches show fewer homeotic gene clusters
and simpler bodies. Later branches show moregene clusters and more complex bodies.
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Fig 27.10
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Genetic Mechanisms
Gene duplication discrepancies
- The number of clusters and the complexity of
the organism do not always correlate, ex. zebrafish and the mouse.
- Loss of gene clusters (?)
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Genetic Mechanisms
Gene Expression
- The time during embryogenesis when homeotic
genes are expressed and the duration of theirexpression affects development.
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Adaptive Radiations or Star
Phylogenies What are they? Fig 27.11.
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Fig 27.11
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Adapti
ve Radiations
What causes radiations?
Ecological Opportunity:
Morphological Innovation:
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Extinctions
Mass extinctions - disappearances of large
numbers of species by an extraordinary,
sudden, temporary change in theenvironment.
Background Extinctions the average rate
of disappearances of organisms caused by
normal variations in the environment or
competition.
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Fig 27.14