3 domains
Bacteria, archaebacteria, eukarya
Bacteria
Prokaryotes, ester links plasma membrane lipids
Archaebacteria
Prokaryotes, ether links plasma membrane lipids
Eukarya
Eukaryotes, ester links plasma membrane lipids
Darwin’s main propositions in 1859
Weaknesses of Darwin’s propositions
Weaknesses of Darwin’s propositions Time is needed for evolutionary change, nut teacart s 4500 MYA old
Heritability mechanisms unknown
Evidence for Darwin’s propositions
Mechanisms for evolutionary change
Stabilisation forces
Species isolating mechanisms
Ecological - spacial and temporal (pre mating)
Reproductive - permeating (teportal, ethological mechanical) and postmating (prezyogitic and pos-zygotic)
Speciation
Panmaxis
Fully random mating (unlikely)
Interbreedng
Self fertilisation or cross fertilisation of closely relayed
Outbreeding
Higher inter breeding levels
Polymorphic phenotypes
Change in local phenotype - different local environment and selection pressures
Polyploidy
Changes in chromosome completes AA => AAA
Hadean
3800 MYA, high tops, v high CO2, water, no life, organic molecules
Archean
The beginning - 3800-2500 MYA, much ocean, v high CO2, negligible oxygen. First prokaryotes with self rep all marine. Photosynthetic cyanobacteria generate oxygen.
Proterozoic
2500-542 MYA, oxygen deposits build up further, marine eukaryotes 1500 MYA,
Cambrian
542-488 MYA, oxygen levels similar to today, rapid diversification, almost entirely marine (cambrian explosion), earliest vertebrates
Ordovican
488-444 MYA, massive glaciers over Gondwanaland, drop sea level - 75% animal species extinct
Silurian
444-416 MYA, marine life recovered, jawless fish, first terrestrial vascular plants and arthropods
Devonian
416-259 MYA, Most jawless fish extinct, mass extinction of text at end. Terrestrial plants more diverse. First tetrapods
Carboniferous
359-297 MYA, large glaciers, extensive swamp forests, diversity of terrestrial animals increased, flight evolved in insects