Evolution of Microbial Life and Macroevolution
Evolution of Microbial Life
Timeline:
Earth formed: 4.5 ext{ BYA}
Stable hydrosphere: 4.2 ext{ BYA}
Prebiotic chemistry to Origin of life: Before 4.0 ext{ BYA}
Worlds progression: Pre-RNA $\rightarrow$ RNA $\rightarrow$ RNA/Protein $\rightarrow$ DNA/RNA/Protein
Oldest microbial fossils (stromatolites): ~3.5 ext{ BYA} (resemble modern cyanobacteria)
First microbial life evidence (carbon signatures): 3.7-3.8 ext{ BYA} (anoxygenic phototrophic filamentous bacteria)
Oxygen-rich atmosphere: 2.8-2.5 ext{ BYA}
Origin of Life Hypotheses
Early Theory: Spontaneous generation (disproven by Louis Pasteur in 1862).
Modern Hypothesis (4 Stages):
Abiotic synthesis of monomers (nucleotides, amino acids).
Polymerization of monomers (DNA, RNA, proteins).
Packaging of polymers into protobionts (membrane-enclosed).
Evolution of cellular properties (self-replication).
Early Earth Conditions:
Atmosphere: Reducing environment, rich in H2O, CO2, SO2, H2, H2S (no O2).
Energy Sources: Intense volcanic activity, lightning, UV radiation.
Stage 1: Monomer Formation:
Reducing Atmosphere Hypothesis (Oparin & Haldane, 1920 ext{s}): Complex organic molecules arose spontaneously.
Miller & Urey Experiment (1953): Simulated early Earth, generating amino acids. Later experiments showed other organic compounds in neutral (N2, CO2) atmospheres.
Deep-Sea Vent Hypothesis: Alkaline deep-sea vents (40-90^ ext{o} ext{C}, pH 9-11) may have been suitable.
Stage 2: Polymer Formation:
Monomers polymerize, possibly on clay substrates to overcome hydrolysis.
Stage 3: Protobiont Packaging:
Polymers aggregated into cell-like structures, e.g., liposomes encapsulating polymers.
Stage 4: Cellular Properties ("RNA World"):
RNA is favored as the first macromolecule due to its 3 key functions:
Information storage.
Capacity for replication.
Enzymatic function (ribozymes).
Chemical Selection: Favored RNA molecules with self-replication and ribonucleotide synthesis abilities.
Fossil Record and Geologic Time
Fossil Formation: Organisms buried by sediments, hard parts replaced by minerals.
Radiometric Dating:
Carbon-14: Dates fossils up to 75,000 years (half-life 5,730 years, decays to Nitrogen-14).
Potassium-40: Dates volcanic rocks hundreds of millions of years old (half-life 1.3 billion years, decays to Argon-40).
Geologic Record: Defined by major transitions; composed of Eons (Archaean, Proterozoic, Phanerozoic) and Eras (Paleozoic, Mesozoic, Cenozoic).
Emergence of Life Groups:
Prokaryotes: 3.8 ext{ BYA}
Atmospheric Oxygen (from prokaryotic photosynthesis): 2.7 ext{ BYA}
Single-celled Eukaryotes: 2.1 ext{ BYA}
Multicellular Eukaryotes: 1.5 ext{ BYA}
Animals: 600 ext{ MYA}
Fungi, Plants, Animals colonize land: ~500 ext{ MYA}
Hominids: 6-7 ext{ MYA}
Humans: ~200,000 years ago
Mechanisms of Macroevolution
Macroevolution: Evolutionary processes and patterns at or above the species level.
Continental Drift:
Slow, continuous movement of Earth's crustal plates.
Pangaea formed 250 ext{ MYA}, its breakup altered habitats, triggered mass extinctions, and influenced species distribution (e.g., lungfishes, marsupials).
Mass Extinctions:
5 major events: Ordovician-Silurian (86\% species), Late Devonian (75\%), Permian-Triassic (90\%$, greatest, 252 ext{ MYA}), Triassic-Jurassic (80\%), Cretaceous-Tertiary (76\%$, dinosaurs extinct, 65 ext{ MYA}).
Current extinction rates are 100-1,000 times background rate, potentially leading to a 6^ ext{th} mass extinction primarily due to human habitat loss.
Adaptive Radiations:
Rapid formation of new species filling new habitats/roles.
Often follow mass extinctions (e.g., mammals after dinosaur extinction) or the evolution of novel adaptations (e.g., land plants with waxy coats, stomates, vascular tissue, seeds, flowers).
Role of Developmental Genes:
Slight changes in genes controlling development can lead to major morphological differences.
Evolutionary Novelties:
Complex structures (e.g., eyes) arise through incremental modifications, with each step providing selective advantage.
Evolution is not goal-directed; intermediate stages must be adaptive. Example: bird wings may have initially served for insulation or display before flight.
Evolutionary Trends:
Natural selection can lead to trends (e.g., predator-prey arms races), but trends can cease or reverse if the environment changes.