Ch 26: The Origin & Diversity of Life Flashcards
Ribosome activity
- RNA may have been first genetic material - Amino acids polymerized into proteins - Metabolic paths emerged - lipid bubbles could inc. chance of metabolic reactions - leads to cell membranes
Plate Tectonics
Continents moved over geological time.
Earth’s crust formed rigid slabs of rock (plates) under continents and oceans
Microfossils
- Fossilized forms of micro life
- Oldest: 3.5 billion years ago
- Resemble present-day
prokaryotes
Endomembrane system
Nuclear membrane, only found in eukaryotes, accounts for increased complexity
Golgi apparatus and endoplasmic reticulum facilitate intracellular transport
Endosymbiosis
Cells "eat" other cells and become multicellular -how mitochondria and chloroplasts entered euk cells
Mitochondria & Chloroplast evolution
Mitochondria:
descendants of relatives of purple sulfur bacteria and the parasite rickettsia.
Chloroplasts:
derived from cyanobacteria
Multi-cellularity
- Allowed organisms to deal with environment in many ways
- Allows for differentiation of cells into tissues
- Evolved independently in eukaryotes supergroups
Sexual reproduction
-Allows greater genetic diversity
-meiosis
-crossing over
-First eukaryotes probably haploid
-diploid arose independently on
sep occasions (fusion of haploid
cells)
Cambrian explosion
- Evo innovations occurred when life primarily aquatic
- 1st multicell animals appeared 50 mil years ago following explosion
Moving onto land
- Plants, then animals, colonized terrestrial environments after Cambrian radiation
- plants photosynthesis created o2 in ozone layer
Compartmentalization
- Allows increased subcellular specialization - Nuclear membrane allows for additional levels of control of transcription/translation
Hadean Era
Formation of Earth
4.5 BYA
Earth cools around 4 BYA
Archean Era
Life emerged (prokaryotes)
Formation of Rodinia
3.5–2.5 BYA
Proterozoic Era
Eukaryotes First multicellular organisms Appearance of animals and plants Cyanobacteria Appearance of oxygen in the atmosphere
Fossilization
- Organisms buried in sediment
- Calcium in bone shell or other
hard tissue mineralizes - Surrounding sediment hardens
to form rock - Erosion must expose fossils