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Origin and History of Life. Where it came from and how it got here. Chapter Outline. Primitive Earth Origin of First Cells Fossils The Precambrian The Paleozoic The Mesozoic The Cenozoic Continental Drift Mass Extinctions. Beginnings. The Universe (maybe)
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Origin and History of Life Where it came from and how it got here
Chapter Outline • Primitive Earth • Origin of First Cells • Fossils • The Precambrian • The Paleozoic • The Mesozoic • The Cenozoic • Continental Drift • Mass Extinctions
Beginnings • The Universe (maybe) • Primitive Earth—Not paradise as we know it—much different than Earth today
Simple to complex • Question: How could these simple molecules be made into more complex ones? • Answer: Abundant energy sources, lots of time.
Origin of organic molecules • Alexander Oparin (1938) — a Russian biochemist with vision • Stanley Miller (1953) – tested the hypothesis
Other models • Carbonaceous chondrites • Panspermia
Panspermia • Life brought in on asteroids and comets • EX. Deinococcus radiodurans
Abiotic Chemical Evolution • Synthesis and accumulation • Polymerization • Aggregation • Origin of heredity
Keep in mind!!! • Chemical natural selection • Conditions of primitive earth • Timescale
Evolution of Macromolecules • RNA first hypothesis • Protein first hypothesis • Clay hypothesis
RNA first hypothesis • RNA contains information like DNA • RNA is catalytic-- -- ribozymes.
Protein First Hypothesis • Most enzymes are proteins • Proteinoids • Proteinoid microspheres • Faithful replication?
Clay hypothesis • Unique chemical properties of clay. • Combines parts of the RNA first and protein first ideas.
Protocell Evolves • Protocells -- precursors to the first true cells. • lipid-protein membrane • Proteinoid microspheres • Coacervates • Liposomes
Energy Management Were the first protocells heterotrophs or autotrophs?
Fossils • Fossils are remains and traces of past life • Why are they so rare?
Dating Fossils Relative Dating Absolute dating Combination
The Precambrian Age of microbes • 570 mya - 4.6 bya • The First Cells —3.5-4 billion years ago • What were they like? • Energy management? • Aquatic or terrestrial? • Prokaryote or eukaryote?
Evolution of Autotrophs • Life as Energy Management • Chemoautotrophs • Photoautotrophs • Atmospheric O2 ~2 BYA
Atmospheric O2—SO WHAT? O2 is very reactive—Poison. Cells had to deal with this Aerobic Anaerobic Facultative anaerobes Changes in atmosphere– O2 and ozone. So? Consequences for energy acquisition
Circle of Life Energy Respiration Carbon compounds, O2 CO2, H2O Photosynthesis Energy
Eukaryotes evolve • More complex • Origin? Endosymbiont hypothesis
nucleoid (DNA) ribosomes food granule prokaryotic flagellum plasma membrane cell wall cytoplasm
nuclear pore chromatin (DNA) nucleus nucleolus nuclear envelope flagellum intermediate filaments cytoplasm plasma membrane rough endoplasmic reticulum ribosome lysosome microtubules smooth endoplasmic reticulum Golgi complex free ribosome vesicle mitochondrion vesicle
1. Anaerobic, predatory prokaryotic cell engulfs an aerobic bacterium. aerobic bacterium 2. Descendants of engulfed bacterium evolve into mitochondria. 3. Mitochondria-containing cell engulfs a photosynthetic bacterium. 4. Descendants of photosynthetic bacterium evolve into chloroplasts.
Multicellularity Evolves Examples? Volvox—Simple, multicellular Advantages?
Summary of Precambrian • Earth forms • Prokaryotes evolved • Photosynthesis • Eukaryotes • Multicellularity • Sexual reproduction
Paleozoic 2 • Mass extinction---Disappearance of a large number of species within a relatively small time interval. • opportunities for speciation
PALEOZOIC- MAJOR EVENTS • What were the major events of the Paleozoic? • three mass extinctions • Invertebrates dominated – exoskeleton • Primitive plants invaded land
PALEOZOIC- MAJOR EVENTS • Vertebrates appeared (jawless fishes) -- internal skeleton • Insects and amphibians invaded the land -- -- evolution of flight, evolution of lungs, evolution of stronger limbs, strengthened internal skeleton
PALEOZOIC- MAJOR EVENTS • Reptiles appear • Shelled egg • Scaly skin • Reptiles diversify amphibians declined • Coal forming forests • Conifers appear
Invasion of Land • Plants • Invertebrates • Vertebrates
MESOZOIC- MAJOR EVENTS • The age of reptiles • Angiosperms evolve-insects diversify • Mammals and birds • Evolution of endothermy
QUESTIONS • From what to did dinosaurs evolve? • From what to do to mammals evolve? • From what did birds evolve? • What caused the mass extinction of dinosaurs? • Were the dinosaurs endothermic?
Endothermy Warm –blooded Requires a high use of energy High metabolic rate Disadvantages? Ectothermy Cold blooded Less energy necessary Regulation? behavioral structural inertial ectothermy Endothermy vs Ectothermy
Cretaceous Mass Extinction • Bolide theory -- -- the most widely accepted theory of the Cretaceous Mass extinction. • Bolide -- -- and exploding asteroid.
CENOZOIC- MAJOR EVENTS • Three mass extinctions • Decline of reptiles • Diversification of • Angiosperms • Insects • Birds • Mammals