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Speciation II

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Ant fossil preserved in amber, some 100 million years old. No different from the ants in our day. There is no difference between fossil life forms dating ... – PowerPoint PPT presentation

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Title: Speciation II


1
There is no difference between fossil life forms
dating back hundreds of millions of years and
their counterparts living today. This fact
utterly disproves the evolutionary claim.

http//www.invitation2truth.com/evidences-of-creat
ion/tellme20.htm
2
Punctuated Equilibrium Hypothesis
  • Stasis is the retention of form through long
    segments of geological time
  • Stasis is common following a brief event of
    innovation
  • Speciation and innovation are coincident in time,
    and possibly linked as processes
  • Periods of innovation are very brief,
    punctuating longer periods of stasis
  • Credit to Niles Eldridge (with S. J. Gould)

3
Who cares?
  • Why did Darwin emphasize gradualism?
  • Why are some scientists skeptical about
    punctuated equilibrium?
  • How are these hypotheses related to
    microevolution?

4
Case study 1 Bryozoa organisms
5
Bryozoa fossils
6
Bryozoa - lineages
7
Foraminifera - living
8
Foraminifera - fossils
microbewiki.kenyon.edu/index.php/Foraminifera
9
Case study 2 foraminiferan Globoratalia
10
Trilobites Stratiography and fossil characters
11
Methods
  • Geometric shape analysis
  • define landmarks (51)
  • quantify shifts in landmark relative positions

12
Stasis, rapid change, gradual change Hypothesis
environmental tracking
13
gradualism or punctuation?
  • For some characters, gradual change is seen in
    the fossil record, but . . .
  • For other characters, no systematic change
  • MOSAIC EVOLUTION within a genetic lineage

14
Interpreting pattern
15
Resolution -- scales of time
  • Geological vs. ecological perspectives
  • Jumps are more likely to be perceived in coarse
    data sets
  • What temporal resolution is needed before
    rejecting or accepting gradualism?

16
Does conservative morphology mean no evolution?
Genetic vs. phenotypic change
17
Historical evolution
  • What were the major revolutions?
  • When did they occur?
  • What is the evidence?
  • Why did they occur?

18
Age of earths crust Evidence from
ZirconScientific American 2005 October Jack
Hills (Australia)
Zircon zirconium silicon oxygen
19
Two isotope decay patterns
20
Stable isotope ratios indicate cool environment
at 4.4 billion years BP
21
Why would we care about the age of the crust?
22
Major revolutions in evolution
  • Pulses of unusually extensive adaptive radiation
    and increase in biodiversity
  • Why is adaptive radiation punctuated?
  • Why do groups undergo adaptive radiation?

23
I. Life from non-life
  • Multiple hypotheses
  • Some potential mechanisms can be tested
    experimentally
  • RNA world hypothesis
  • Feasibility is testable we are a long way from a
    widely accepted hypothesis

24
II. Biochemical diversification
  • Began with the evolution of prokaryotes
  • Proceeded for 1.5 billion years before the
    evolution of the first eukaryotes 3 billion
    years prior to multicellular diversification
  • What are some examples of biochemical
    diversification for prokaryotes?

25
Forms of biochemical adaptations
26
III. Cellular diversification
  • Eukaryotes at least 2 billion years bp
  • Genomes with introns
  • Organelles (endosymbiosis theory)

27
IV. Body plan diversity
  • Multicellularity
  • Sexual reproduction developmental processes
  • Alternative solutions to problems
  • Surfacevolume issues
  • Transport issues
  • Nutrient acquisition issues
  • Protection issues

28
Evidence for multiple origins of multicellularity
  • Plants and animals (clades with different trophic
    strategies)
  • Within animals, creation of embryonic tissues
  • diploblast vs triploblast
  • symmetry none, radial, bilateral
  • Strategy of blastula infolding
  • gastrulation
  • protostome vs. deuterostome (mouth first or
    second)

29
When did multicellularity arise?
  • Cambrian Explosion seen well after 1st forms
  • 610 Ma radially symmetric form first seen
  • 565 Ma to 525 Ma major phyla appear in fossils
  • 0.8 of earths history accounted for almost all
    major diversity of multicellular strategies

30
Why did body plans diversify?
  • Changes in continents, oceans
  • Changes in environment
  • Rising oxygen concentrations in ocean
  • Increasing complexity of biotic interactions

31
V. Colonization of land
  • Major adaptations to utilize a new environment
  • Plant-animal coevolution
  • Plant-herbivore coevolution
  • Plant-pollinator coevolution
  • Plant-disperser coevolution
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