Title: Speciation II
1There 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
2Punctuated 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)
3Who cares?
- Why did Darwin emphasize gradualism?
- Why are some scientists skeptical about
punctuated equilibrium? - How are these hypotheses related to
microevolution?
4Case study 1 Bryozoa organisms
5Bryozoa fossils
6Bryozoa - lineages
7Foraminifera - living
8Foraminifera - fossils
microbewiki.kenyon.edu/index.php/Foraminifera
9Case study 2 foraminiferan Globoratalia
10Trilobites Stratiography and fossil characters
11Methods
- Geometric shape analysis
- define landmarks (51)
- quantify shifts in landmark relative positions
12Stasis, rapid change, gradual change Hypothesis
environmental tracking
13gradualism 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
14Interpreting pattern
15Resolution -- 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
17Historical evolution
- What were the major revolutions?
- When did they occur?
- What is the evidence?
- Why did they occur?
18Age of earths crust Evidence from
ZirconScientific American 2005 October Jack
Hills (Australia)
Zircon zirconium silicon oxygen
19Two isotope decay patterns
20Stable isotope ratios indicate cool environment
at 4.4 billion years BP
21Why would we care about the age of the crust?
22Major revolutions in evolution
- Pulses of unusually extensive adaptive radiation
and increase in biodiversity - Why is adaptive radiation punctuated?
- Why do groups undergo adaptive radiation?
23I. 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
24II. 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?
25Forms of biochemical adaptations
26III. Cellular diversification
- Eukaryotes at least 2 billion years bp
- Genomes with introns
- Organelles (endosymbiosis theory)
27IV. Body plan diversity
- Multicellularity
- Sexual reproduction developmental processes
- Alternative solutions to problems
- Surfacevolume issues
- Transport issues
- Nutrient acquisition issues
- Protection issues
28Evidence 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)
29When 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
30Why did body plans diversify?
- Changes in continents, oceans
- Changes in environment
- Rising oxygen concentrations in ocean
- Increasing complexity of biotic interactions
31V. Colonization of land
- Major adaptations to utilize a new environment
- Plant-animal coevolution
- Plant-herbivore coevolution
- Plant-pollinator coevolution
- Plant-disperser coevolution