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Marine Bacteria and Archaea
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Metabolic diversity
• Organisms have two fundamental nutritional needs: • 1. Obtaining carbon in a form that can be used to
synthesize fatty acids, proteins, DNA, and RNA
• Autotrophs get their carbon from CO2
• Heterotrophs get carbon from organic sources vs
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Metabolic diversity
• Organisms have two fundamental nutritional needs: • 2. Acquiring chemical energy in the form of ATP
• Phototrophs: energy from light
• Lithotrophs (or Chemotrophs): energy from inorganic chemicals
such as H2S, ammonia NH3, methane CH4
• Organotrophs: energy from organic sources, such as sugars
Metabolic diversity
Category Energy source Carbon source Hydrogen or electron source
Examples
Photolithoautotrophy Light CO2 Inorganic Cyanobacteria, purple sulfur bacteria
Photoorganoautotrophy
Light Organic compounds Organic compounds or H2
Purple non-sulfur bacteria, aerobic, anoxygenic bacteria, archaea (?)
Chemolithoautotrphy Inorganic CO2
Inorganic Sulfur-oxidizing bacteria, nitrifying bacteria, archaea
Chemoorganoautotrophy
Organic compounds
Organic compounds
Organic compounds Wide range of bacteria and archaea
Mixotrophy (combination of lithoautotrophy and organoheterotrophy)
Organic compounds
Organic compounds
Inorganic Sulfur-oxidizing bacteria
Evolution of life
Prebiotic chemistry
Precellular life
Early cellular life
LUCA Evolutionary diversification
Biological building blocks Amino acids Nucleosides Sugars
4.3-3.8 bya 3.8-3.7 bya
RNA world
Protein synthesis
DNA Lipid bilayers
Divergence of Bacteria and Archaea
Catalytic RNA Self-replicating RNA
RNA – templated translation
Replication Transcription
Cellular compartments Early cells likely had high rates of HGT
Components of DNA replication, transcription, and translation all in place
Submarine mounds and their possible link to the origin of life. Model of the interior of a hydrothermal mound with hypothesized transitions from prebiotic chemistry to cellular life depicted
Differences between Archaea, Bacteria and Eukaryotes
Characteristic Bacteria Archaea Eukaryotes
Cell type Prokaryotic Prokaryotic Eukaryotic
Histones No histones Have proteins similar to histones
Have histones
Introns No introns Some introns Most contain introns
Ribosome size 70S ribosomes 70S ribosomes 80S ribosomes
Cell wall composition
Peptidoglycan Made of protein (lack peptidoglycan) plasma membrane
Not always present Plants: cellulose Fungi: Chitin
Cell membrane composition
Ester linked lipids with D-Glycerol (straight chain)
Ester linked lipids with L-Glycerol (branch chain)
Ester linked lipids with proteinf (straight chain)
Themes: Growth & reproduction by fission
A. Bacterium before DNA replication. Bacterial chromosome is attached to the plasma membrane.
B. DNA replication starts. It proceeds in two directions
C. The new copy of DNA is attached at a membrane site near the parent DNA molecule.
D. New membrane grows between the two attachment sites.
E. Deposits of new membrane and new wall material extend down into the cytoplasm.
F. The ongoing deposition of membrane and wall material divides the cell in two.
Themes: conjugation
A. A conjugation tube forms between a donor and a recipient cell. An enzyme has nicked the donor’s plasmid.
B. DNA replication starts on the nicked plasmid. The displaced DNA strand moves through the tube and enters the recipient cell.
C. In the recipient cell, replication starts on the transferred DNA.
D. The cells separate from each other; the plasmids circularize.
nicked plasmid conjugation tube
Themes: Morphological diversity
• Many have flagella for swimming and pili for clinging to surfaces
• Typical Shapes:
Pili
Cocci Bacilli Spirochetes
Marine bacteria
Planktonic Bacteria and Archaea
• Relatively few major clades Bold = ubiquitous in seawater, others are specialized
Roseobacter • 25% marine bacteria • Plankton • Sediments • Microbial mats • Sea ice • Association with animals • Important in carbon and sulfur cycles
Marine bacterial phenotypes
• Anoxygenic • Eg Purple phototrophs • Do not evolve Oxygen during photosynthesis • Bacteriochlorophyll as photosynthetic pigment • Many in shallow marine sediments
Rhodospirillum
CO2 + H2S + H2O = (CH2O) + S + H2O
Marine bacterial phenotypes
• Oxygenic Photosynthesis • Cyanobacteria
• Ancestors – evolution of oxygen • Chlorophyll a and accessory photosynthetic pigments • “Blue green algae” but many “red orange” • Very diverse habitats, including extreme temperatures and hypersaline environments • Plankton, sea ice, shallow sediments, microbial mats • Many carry out nitrogen fixation • Only recently grouped together (16S sequencing)
Synechococcus Prochlorococcus
Account for between 15-40% of carbon input to ocean food webs
• Nitrifying bacteria • Major role in nitrogen cycling, especially shallow coastal sediments, and
beneath upwelling areas • Nitrosomonas and Nitrosococcus oxidize ammonia to nitrate
• Chemolithoautotrophs
• Nitrosobacter, Nitrobacter, and Nitrococcus oxidize nitrite to nitrate • Usually chemolithoautotrophs also mixotrophs
Marine bacterial phenotypes
• Chemolithotrophs
Beggiatoa Aerobe in top few mm of marine sediments Uses reduced sulfur compounds
Thioploca Multicellular filamentous bacteria Upwelling Anoxic reduction of H2S and reduction nitrogen Auto- or mixo-trphic
Thiomargarita namibiensis Largest known bacteria, filaments with common mucus sheath Upwelling Oxidizes sulfite using nitrate
Marine Archaea
Archaea
• Methanogens • Anaerobic process carried out only by Euryarchaeota (major clade) • Large amount of methane is produced in marine sediments, but
disappears before oxygen zone, where methane would be reduced • Sulfate-reducing bacteria oxidize methane using sulfur
Methanosarcina Desulfococcus
Archaea • Extreme Thermophiles
Thermococcus Anaerobic chemoorganotroph, optimum growth at 800C
Pyrococcus Anaerobic chemoorganotroph Optimal growth at 100oC
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Archaea
• Halophiles • Grow in concentrations
greater than 9% NaCl