Theme: Unity and Diversity - Level of Organization: Cells
Subtopics
A2.1.1 - Conditions on early Earth and the pre-biotic formation of carbon compounds.
A2.1.4 - Evidence for the origin of carbon compounds.
A2.1.5 - Spontaneous formation of vesicles by coalescence of fatty acids into spherical bilayers.
A2.1.6 - RNA as a presumed first genetic material (HL – Higher Level).
A2.1.7 - Evidence for a last universal common ancestor.
A2.1.8 - Approaches used to estimate dates of the first living cells and the last universal common ancestor.
A2.1.9 - Evidence for the evolution of the last universal common ancestor in the vicinity of hydrothermal vents (HL).
Early Earth Conditions and Pre-biotic Formation of Carbon Compounds
A2.1.1 - Conditions on early Earth and the pre-biotic formation of carbon compounds:
Early Earth had a reducing atmosphere (little to no free oxygen), volcanic activity, and intense UV radiation.
Key compounds like water, methane, ammonia, and hydrogen sulfide were present.
Energy sources included lightning, volcanic activity, and UV radiation, facilitating chemical reactions.
A2.1.4 - Evidence for the origin of carbon compounds:
Miller-Urey experiment: Demonstrated that amino acids could be formed from inorganic precursors under early Earth conditions.
Analysis of meteorites: Carbonaceous chondrites contain amino acids, lipids, sugars, and nitrogenous bases.
Deep-sea hydrothermal vents: Provided environments rich in chemical energy and minerals for the synthesis of organic compounds.
A2.1.5 - Spontaneous formation of vesicles by coalescence of fatty acids into spherical bilayers:
Fatty acids can spontaneously form vesicles in water, creating enclosed structures similar to cell membranes.
These vesicles can encapsulate other molecules, providing a mechanism for concentrating and protecting early biochemical reactions.
A2.1.6 - RNA as a presumed first genetic material (HL – Higher Level):
RNA has simpler structure than DNA and can act as both a carrier of genetic information and a catalyst (ribozymes).
RNA world hypothesis: Suggests that RNA was the primary form of genetic material before DNA evolved.
Last Universal Common Ancestor (LUCA)
A2.1.7 - Evidence for a last universal common ancestor:
Universal genetic code: All known life forms use the same set of genetic codons, suggesting a common origin.
Conservation of core metabolic pathways: Key biochemical pathways, such as glycolysis and ATP synthesis, are conserved across diverse organisms.
Ribosomal RNA (rRNA): Highly conserved sequences in rRNA genes are used to infer phylogenetic relationships and identify LUCA.
A2.1.8 - Approaches used to estimate dates of the first living cells and the last universal common ancestor:
Molecular clocks: Using mutation rates in conserved genes to estimate the time of divergence between species.
Geological evidence: Analyzing ancient rocks and fossils to determine the age of the earliest life forms.
A2.1.9 - Evidence for the evolution of the last universal common ancestor in the vicinity of hydrothermal vents (HL):
Hydrothermal vents provide a stable and energy-rich environment for early life.
Chemosynthesis: LUCA likely used chemosynthesis to derive energy from chemical compounds, such as hydrogen sulfide, available at hydrothermal vents.
Phylogenetic analysis: Indicates that the earliest branches of the tree of life are microorganisms that thrive in high-temperature environments, similar to those found near hydrothermal vents.