While the sediments and rocks in the Earth's crust are the largest carbon reservoir, CO2 in the atmosphere is the most rapidly transferred carbon reservoir
CO2 is removed from the atmosphere by
Photosynthetic land plants and marine microbes
Syntrophy
Two or more organisms cooperate to benefit nutritionally from the presence of the other
Biochemical oxygen demand (BOD)
The microbial oxygen-consuming capacity of a body of water
Methanogens
Team up with partners (syntrophs) that supply them with substrates and remove products
Influx of organic material (e.g., from sewage)
Increases BOD, then decreases over time
Most microbes cannot be cultivated in the lab due to environmental factors, nutritional factors, and syntrophy
The Nitrogen Cycle
Nitrogen is a key constituent of cells and exists in a number of oxidation states, with four major nitrogen transformations: nitrification, denitrification, anammox, and nitrogen fixation
Open ocean environment
Saline
Low in nutrients (oligotrophic), especially with respect to nitrogen, phosphorus, and iron
Cooler
Microbial activities taking place in the oceans are major factors in Earth's carbon balance
Nitrification
NH4+ to NO3-
Oligotroph
An organism that grows best at very low nutrient concentrations
Denitrification
NO3- to N2
Pelagibacter
The most abundant marine heterotroph
Anammox
Anaerobic oxidation of ammonia to N2 gas
Proteorhodopsin
A form of rhodopsin that allows cells to use light energy to drive ATP synthesis
Fermentations
Energy conservation depends on substrate-level phosphorylation
Defined by lack of external electron acceptor
No ETC or PMF
Achieve redox balance by donating electrons to metabolic intermediates excreted as fermentation products
Conserve much less energy (via Substrate-Level Phosphorylation) than respiratory organisms
Tremendous reaction diversity
Nitrogen Fixation
N2 + 8 H → 2 NH3 + H2
Deep-sea hydrothermal vents
Thriving animal and microbial communities are associated with them
Chemolithotrophic bacteria predominate at vent
Thermophiles and hyperthermophiles are present
Chemolithotrophic prokaryotes utilize inorganic materials from the vents
N2 Fixation: Azotobacter (aerobic), Clostridium, purple and green phototrophic bacteria, Methanobacterium (Archaea) (anaerobic), Rhizobium, Bradyrhizobium, Frankia (symbiotic)
Chemolithotrophic Bacteria and Archaea Present Near Deep-Sea Hydrothermal Vents
Sulfur-oxidizing
Nitrifying
Sulfate-reducing
Methanogenic
Hydrogen-oxidizing
Iron- and manganese-oxidizing
Methylotrophic
N2 is the most stable form of nitrogen and is a major reservoir, as it is ~70 percent of the Earth's air
Alcoholic fermentation
Hexose gives 2 ethanol + 2 CO2
Only a few prokaryotes have the ability to use N2 as a cellular nitrogen source. They convert inorganic to organic nitrogen through an energy-intensive process called nitrogen fixation.