the history of life chapter 17. fossils preserved traces and remains of ancient life
TRANSCRIPT
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The History of Life
Chapter 17
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Fossils Preserved traces and remains of ancient life.
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The Fossil Record Paleontologists study ancient life through
fossils. They make inferences about past life and group similar
organisms together to create the fossil record. Fossils show that more than 99% of all living species
that have ever existed have become extinct.
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How Fossils Form Is the fossil record complete?
Many more organisms die without leaving traces than those that do.
Most fossils form in sedimentary rock.
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Water carries small rock particles to lakes and seas.
Dead organisms are buried by layers of sediment, which forms new rock.
The preserved remains may later be discovered and studied.
Section 17-1
Figure 17-2 Formation of a Fossil
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Interpreting Fossil Evidence Relative Dating –
Estimates a fossil’s age by comparing to other fossils present in the same layer. Index fossils identify a
particular era
Absolute (Radioactive) Dating – A more exact method of
determining a fossil’s age by determining the percent of a radioactive element left in the sample.
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Relative Dating
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Relative Dating
Can determine
Is performed by
Drawbacks
Absolute Dating
Comparing Relative and Absolute Dating of Fossils
Section 17-1
Compare/Contrast Table
Imprecision and limitations of age data
Difficulty of radioassay laboratory methods
Comparing depth of a fossil’s source stratum to the position of a reference fossil or rock
Determining the relative amounts of a radioactive isotope and nonradioactive isotope in a specimen
Age of fossil with respect to another rock or fossil (that is, older or younger)
Age of a fossil in years
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Geologic Time Scale Represents evolutionary time. Precambrian time - before complex life Eras – after Precambrian time.
Paleozoic – fish and amphibiams Mesozoic – age of dinosaurs Cenozoic – age of mammals
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Section 17-3
Geologic Time Scale with Key Events
Glaciations; mammals increased; humans
Mammals diversified; grasses
Aquatic reptiles diversified; flowering plants; mass
extinction
Dinosaurs diversified; birds
Dinosaurs; small mammals; cone-bearing plants
Reptiles diversified; seed plants; mass extinction
Reptiles; winged insects diversified; coal swamps
Fishes diversified; land vertebrates (primitive
amphibians)
Land plants; land animals (arthropods)
Aquatic arthropods; mollusks; vertebrates (jawless
fishes)
Marine invertebrates diversified; most animal phyla
evolvedAnaerobic, then photosynthetic prokaryotes; eukaryotes, then multicellular life
Cenozoic
Mesozoic
Paleozoic
PrecambrianTime
Quaternary
Tertiary
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
1.8–present
65–1.8
145–65
208–145
245–208
290–245
363–290
410–363
440–410
505–440
544–505
650–544
Key EventsEra Period Time(millions of years ago)
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Earth’s Early History Ancient earth was hostile.
Poisonous atmosphere ; no oxygen Oceans were a “hot thin soup” UV radiation, lightening, volcanos… So how did life begin?
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Mixture of gases simulating atmospheres of early Earth
Spark simulating lightning storms
Condensation chamber
Cold water cools chamber, causing droplets to form
Water vapor
Liquid containing amino acids and other organic compounds
Section 17-2
Figure 17-8 Miller-Urey Experiment
Stanley Miller recreated early earth’s atmosphereMade simple organic molecules (amino acids…)
The first organic molecules…
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Coacervates
Proteinoid microspheres may have formed in shallow pools as precursors to cells.
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Evolution of RNA and DNA
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Stromatolites Ancient prokaryotes added oxygen to the
atmosphere. The rise of oxygen caused drove some life
forms to extinction while others evolved.
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Aerobic bacteria
Ancient Prokaryotes
Ancient Anaerobic Prokaryote
Primitive Aerobic Eukaryote
Primitive Photosynthetic Eukaryote
Chloroplast
Photosynthetic bacteria
Nuclear envelope evolving
Mitochondrion
Plants and plantlike protists
Animals, fungi, and non-plantlike
protists
Figure 17-12 Endosymbiotic TheoryEndosymbiotic Theory – origin of eukaryotic cells
This theory proposes that eukaryotic cells arose from symbiotic relationships between bacteria and cells.
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Sexual Reproduction and Multicellularity
This ancient jellyfish was an early multicellular animal.
With the advent of sexual reproduction the rate of evolution took off.
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Evolution of LifeEarly Earth was hot; atmosphere contained poisonous gases.
Earth cooled and oceans condensed.
Simple organic molecules may have formed in the oceans..
Small sequences of RNA may have formed and replicated.
First prokaryotes may have formed when RNA or DNA was enclosed in microspheres.
Later prokaryotes were photosynthetic and produced oxygen.
An oxygenated atmosphere capped by the ozone layer protected Earth.
First eukaryotes may have been communities of prokaryotes.
Multicellular eukaryotes evolved.
Sexual reproduction increased genetic variability, hastening evolution.
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Heterotroph Hypothesis The first cells were…
Heterotrophs autotrophs Anaerobic aerobic Unicellular multicellular Asexual sexual
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Patterns of Evolution Extinction
The last member of a species dies….(failure of a species to adapt)
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Patterns of Evolution Adaptive radiation
An ancestral form evolves into diverse forms through natural selection
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Patterns of Evolution Convergent evolution
Unrelated species evolve similar adaptations due to similar environments
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Patterns of Evolution Coevolution -
Evolution of two different species in response to each other: symbiosis
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Patterns of Evolution Gradualism –
A slow and steady rate of evolution
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Patterns of Evolution Punctuated equilibrium –
Periods of rapid evolution followed by long stretches of stability
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Section 17-4
Flowchart
that are
can undergo can undergo can undergo can undergo can undergo
in underunderform inin
Species
Unrelated Related
Inter-relationshiops
Similar environments
Intense environmental
pressure
Small population
s
Different environments
Coevolution Convergent evolution
ExtinctionPunctuate
d equilibrium
Adaptive radiation