microbial ecology 1 Flashcards
Competition
a conflict of resources, affecting the growth of both organisms
Commensalism
one member benefits from another member, which itself is unaffected
Mutualism
both organism benefit from each other
- Interspecies hydrogen transfer
- Holobiont concept
Amensalism
one population adversely affects the growth of another populations, while itself is being unaffected by the other population
Parasitism
one organism, the parasite, consumes another organism, the host, often in a subtle way
Predation
one organism, the predator, engulfs and digest another organism, the prey
16S rRNA sequencing
This method targets a specific region of the 16S ribosomal RNA (rRNA) gene, which is present in the genetic material of these microorganisms
Syntrophy
process in which two or more organisms cooperate in the anaerobic degradation of organic compounds
Methanogenesis
the biological production of CH4: carried out by strictly anaerobic Archaea
- methane is produced in anoxic environments by methanogens from the reduction of Co2 with hydrogen H2 or from the splitting of acetate into CH4 and CO2
Complete nitrification by Nitrospira
comammox
Symbioses
mutualistic relationship where one species lives on or within another species
Phycosphere
a region surrounding phytoplankton calles that results from the basic physics of the diffusive boundary layer and has a higher concentrations of organic matter (produced by the eukaryote) than local waters
Mixotrophic predation
a combination of phototrophic and heterotrophic metabolism.
Kleptoplasty
a symbiotic phenomenon whereby plastids, notably chloroplast from algae, are sequestered by host organisms
Intermezzo
What can be the reason that only a minute fraction of bacteria in Natura can be isolated in pure culture? only a few can live separately from the colony, they depend on each other. Some don’t like to grow on a medium. we can’t mimic the natural environment on a Petry dish
Redox cascade
microbial processes in marine sediments: Pathways of organic carbon degradation (mineralization) in marine sediments and their relation to the geochemical zonation and consumption of oxidants.
Advective-driven sediments
mostly permeable (sandy), where bottom water currents
produce deep oxygen penetration and high aerobic mineralization. (water diffusive trough by force) aerobic respiration nitrification
Bioturbated sediments
where particle reworking and ventilation of burrow structures by
fauna alter the reoxidation zones in the sediment.
Diffusive sediments
with overlapping O2 and H2S, with no bioturbation and small grain
size. Chemical gradients are driven by diffusion
CO2
carbon dioxide
CH4
methane
NO3
nitrate
NO2
nitrite
N2O
nitrogen oxide
NH3
ammonia
NH4
ammonium
SO4
sulfate
SO3
sulfite
S
Sulfide
nitrification
conversion of ammonia into easily absorbable form of nitrogen
denitrification
nitrate to nitrogen gas
hydrolysis
molecule broken down in >2 smaller molecules through addition of water
oxidation
electron-donating reaction
reduction
electron accepting reaction
colourless sulfur bacteria (CSB)
use reduced sulfur compounds as energy source -> H2S
sulfate reduction
production of hydrogen sulfide (H2S)
phototrophs
use light as E-source and produce ATP