Life originated under conditions vastly different from present-day Earth.
Early Earth atmosphere possibly consisted of:
Water vapor
Nitrogen and its oxides
Carbon dioxide
Methane
Ammonia
Hydrogen
Hydrogen sulfide
Initial conditions set the stage for the development of life to be explored.
Conditions of early Earth markedly different:
High presence of gases like nitrogen, methane, and hydrogen sulfide.
Theories proposed in the 1920s:
A. I. Oparin and J.B.S. Haldane's Hypothesis:
Early oceans could have been a "primordial soup" of organic molecules.
The atmosphere was reducing (electron-adding), allowing for organic molecule formation.
Energy sources for organic synthesis included lightning and intense UV radiation.
Conducted experiments based on the early Earth atmosphere hypothesis:
Successfully created organic compounds, notably amino acids.
Subsequent research by others, under extreme conditions, produced polymers without enzymatic assistance.
Protobionts are collections of abiotically produced molecules enveloped by vesicle-like structures.
Early replication may have involved RNA:
Copy errors could stabilize variants leading to selection.
Transition from RNA to DNA:
DNA provides greater stability and fewer replication errors.
Abiotic Synthesis: Formation of small organic molecules (e.g., amino acids).
Micromolecule Assembly: Combining small molecules into macromolecules (e.g., proteins).
Packaging into Protobionts: Forming membranes isolating internal environments.
Origin of Self-Replicating Molecules:
Initially RNA, followed by DNA.
Development of photoautotrophs which significantly contributed to atmospheric oxygen.
RNA likely the first genetic material:
Ribozymes can duplicate RNA given monomer supplies.
RNA is versatile, allowing for various forms and enzymatic functions.
Theory suggests that mitochondria and chloroplasts originated as prokaryotic endosymbionts:
Entered as prey or internal parasites, particularly advantageous if anaerobic.
Evidence supporting this:
Inner membranes share traits with prokaryotes.
Replication processes resemble prokaryotic fission.
Both organelles possess their own DNA and ribosomes.
Carolus Linnaeus (1707-1778):
Developed binomial nomenclature for species classification.
Established taxonomy.
Georges Cuvier (1769-1832):
Studied fossils, noted changes across strata, and inferred extinctions.
Advocated catastrophism as an explanation for observed phenomena.
James Hutton (1726-1797):
Proposed uniformitarianism to explain geological features through gradual processes.
Jean Baptiste Lamarck (1744-1829):
Proposed an early theory of evolution: use and disuse of traits, with hereditary transmission.
Recognized environmental influence on evolution.
Thomas Malthus (1766-1834):
Suggested populations grow rapidly, leading to competition and potential societal collapse.
Charles Lyell (1797-1875):
Advocated gradual geological changes and established uniformitarianism based on Hutton's ideas.
Charles Darwin (1809-1882):
Established foundational theories on evolution through observation and evidence collection during the Beagle voyage.
Noted diversity in species across different geographic locations, particularly the Galapagos Islands.
Evolution rests on four main principles:
Variation among individuals within a population.
Heritable variations passed down.
Overproduction leading to competition for resources.
Natural selection favoring individuals with traits best suited to the environment.
Natural Selection Process:
Variation leads to differential survival and reproduction tailored to the environment, gradually causing evolution and adaptation in populations.
Illustrates evolution based on environmental influences shaping species traits (e.g., beak types).
Represents a key example of Darwin's concept of "descent with modification.
Each branch signifies common ancestral lineage.