Prokaryotes: Bacteria and Archaea Flashcards
Evolution of Life Over Geologic Time
The history of life is a story of DIVERSIFICATION - the rapid increase of new taxa and extinction. There are 4 eons of geologic time:
1. Hadean
2. Archaean
3. Proterozoic
4. Phanerozoic
Hadean Eon
- 4.6-4.0 BYA
- occurred before life arose
- before compelling evidence of life
Archaean Eon
- 4.0-2.5 BYA
- featured the evolution of early life including bacteria, archaea, and the first CYANOBACTERIA capable of oxygenic photosynthesis
Proterozoic Eon
- 2.5 BYA-542 MYA
- featured oxygen accumulation (the Oxygen Revolution)
- first single-celled and multicellular eukaryotes
- flourishing of early microbial and multicellular life
Phanerozoic Eon
- 542 MYA-Present
- beginning with the Cambrian explosion
- features the increase of plant and animal life
Three Domains of Life
- all share a single common ancestor
- fossils indicates prokaryotes (A + B) were the first living organisms
Bacteria Unique Traits
- Bacterial cell walls are composed of peptidoglycan, a protein and sugar complex
Archaea Unique Traits
- Archaeal cell walls are composed of polysaccharides (sugar)
- Archaeal membranes contain branched isoprene chains
Eukarya Unique Traits
- DNA in nucleus
- unicellular and multicellular
- membrane bound organelles
- multiple linear chromosomes
- reproduce through mitosis
- plant cells walls (cellulose) and fungi cell walls (chitin)
Earliest Life on Earth
Evidence suggests life arose during the ARCHEAN:
- Microfossils
- Biosignatures
- Stromatolites
Earliest Life on Earth: Microfossils
suggest life arose between 3.5-3.8 BYA
Earliest Life on Earth: Biosignatures
suggests life may have been present as early as 4.1 BYA
- include chemical isotopes/molecules that suggest biological activity life specific carbon isotopes and components of FA, proteins, and nucleic acids
- First living things were single-celled prokaryotic anaerobes and likely chemotrophic
Earliest Life on Earth: Stromatolites
layered sedimentary structures produced by microbes as they create a series pf multi-layered sheets composed of successive generations of microorganisms
- Date 3.48-3.7 BYA
- Might have included photosynthetic bacteria (though not oxygenic yet)
The Oxygen Revolution
the evolution of oxygenic photosynthesis of early cyanobacteria that began near end-Archean (2.6 BYA)
- Cyanobacteria split water to produce oxygen byproduct, generating the first free molecular O2 in early Earth’s atmosphere
- Free O2 reacted with soluble iron in the oceans, causing iron oxide to precipitate
- Oceans were not fully oxygenated until 850 MYA near the end-Proterozoic
- Evidence of SLOW ACCUMULATION of O2 is BANDED IRON FORMATIONS in sedimentary rocks
Origin of Eukaryotes
Microfossil evidence suggests that eukaryotes arose between 1.6-2.2 BYA during the Proterozoic after the start of the Oxygen Revolution