The History of Life on Earth Chapter 25. Question How have events in the Earth’s history...
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Transcript of The History of Life on Earth Chapter 25. Question How have events in the Earth’s history...
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The History of Life on Earth
Chapter 25
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Question
• How have events in the Earth’s history contributed to life as we know it?
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Bazinga
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How did Life get started?
• One Idea - Chemical Evolution: the evolution of life by abiogenesis.
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Steps
1. Monomer Formation2. Polymer Formation
(macromolecules)3. Protobiont Formation4. Origin of self-replicating
molecules (heredity)
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Primitive Earth Conditions• Reducing atmosphere present.
• Simple molecules–Ex: H2O, CH4, H2, NH3
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Complex Molecule Formation
• Requires energy sources: –UV radiation
–Radioactivity
–Heat
–Lightning
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Oparin and Haldane 1920s
• Hypothesized steps of chemical evolution from primitive earth conditions.
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Results
• Found organic monomers including Amino Acids.
• Suggested that under the primitive Earth’s conditions, monomers could form.
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Self-replicating molecules (Heredity)
• DNA RNA Protein
• Too complex for early life.
• Other forms of genetic information?
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RNA Hypothesis
• RNA as early genetic information:–RNA polymerizes easily.
–RNA can replicate itself.
–RNA can catalyze reactions including protein synthesis.
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DNA
• DNA developed later as the genetic information.
• Why? More stable than RNA
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Alternate View
Life developed in Volcanic Vents.
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Volcanic Vents
• Could easily supply the energy and chemical precursors for chemical evolution.
• Most primitive life forms today are the prokaryotes found in or near these vents.
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New Idea• Life started in cold environments.• Interface between liquid and solid
allows concentration of materials and formation of polymeres.
• Molecules last longer too.
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Hypothesis
• Life as a natural outcome of chemical evolution.
• Life possible on many planets in the universe (?).
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Fossils• Any preserved remnant or
impression of a past organism.
1. Mineralized
2. Organic Matter
3. Trace
4. Amber
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Mineralized Fossils
• Found in sedimentary rock.
• Minerals replace cell contents.
• Ex: bone, teeth, shells
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Organic Matter Fossils
• Retain the original organic matter.
• Ex: plant leaves trapped in shale.
• Comment – can sometimes extract DNA from these fossils.
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Trace Fossils
• Footprints and other impressions. No organic matter present.
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Amber
• Fossil tree resin.
• Preserve whole specimen.
• Usually small insects etc.
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Fossils - Limitations
• Rare event.
• Hard to find .
• Fragmentary.
• Dating.
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Fossil Dating Methods
1. Relative - by a fossil's position in the strata relative to index fossils.
2. Absolute - approximate age on a scale of absolute time.
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Absolute - Methods
1. Radioactive
2. Isomer Ratios
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Radioactive
• Estimated from half-life products in the fossil.
• Ex: Carbon - 14 Potassium – 40
• Different isotopes have different half-lives.
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Key Events in the Origin of Life
• Origin of Life and single-celled organisms
• Ps and Oxygen revolution• First Eukaryotes• Origin of Multicellularity• The Cambrian Explosion• Colonization of Land• Mass extinctions and radiations
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Origin of Life
• Dates to about 3.5 billion years ago
• Stomatolites are a fossil evidence.
• Prokaryotic cells – asexual reproduction only.
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Origin of Multicellularity• Started about 1.2 billion years
ago.
• Time of “snowball” Earth.
• Diversification started about 565 million years ago when Earth thawed.
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Cambrian Explosion• 535-525 million years ago.
• Explosion of life forms especially large predators.
• Many prey capturing adaptations and defense mechanisms seen in fossils.
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Colonization of Land
• Plants – 420 million years ago.
• Animals – 365 million years ago.
• Problems – desiccation, gravity, light, temperature
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Mass Extinctions & Adaptive Radiations
• Fossils indicate that life on earth has shifted regularly.
• Most life has gone extinct.• Severe climate changes have
happened.• Why?
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Continental Drift
• The movement of the earth's crustal plates over time.
• Drift is correlated with events of mass extinctions and adaptive radiations of life.
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Examples
• 5 major extinction events–Permian Extinction
–Cretaceous Extinction
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Result of Mass Extinctions
• Climate changes.• Areas are open for the surviving
species to exploit.• Rapid period of speciation
(adaptive radiation).• Many new species are formed in a
very short period of time.
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Species Selection
• Speciation = birth
• Extinction = death
• Species that leave the most new species are the most successful.
• Encourages “branches” in the Tree of Life.
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Summary
• Chemical Evolution steps.• Recognize the use and limits of
fossils.• Key Evens in Earth’s History.• What happens to evolution in
mass extinctions.
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Bazinga2