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3 components of the geo-bio interface
Cellular physiology
Aqueous environment
Mineralogy
Why take samples
Difficult to measure a whole ecosystem
Heterogeneity makes replication important
Downside of samples
Microenvironment is changed during, so components behave differently
Sampling sediments/soil
Topsoil with trowel
Deeper with boreholes/corers
In lakes with a Jenkin sampler
Sampling water
Johnson-ZoBell → sucks water up into the bottle via a glass tube, maintaining sterility with a rubber stopper to create a vacuum
Groundwater pump
Niskin bottle for deeper water and larger samples, sealing airtight at desired depth
CTD diver measures Conductivity, Temperature and Depth in situ
How do you concentrate biomass in a water sample
Filtration and centrifuge
Methods of sample storage
Freeze between -20 → -70C using liquid nitrogen/dry ice for direct measurement of cellular components
Fixative solution (formaldehyde, alcohol, commercial) for cell counts (cant freeze due to ice crystals rupturing)
Cultivation or activity measurements as soon as possible after sampling or after storage at 4oC
Geochemical analysis of samples
pH probe
Redox probe
Ion Chromatography (IC)
Inductively Coupled Plasma - Atomic Emission Spectrometry
(ICP-AES)
GC
TIC/TOC
Electron microscopy
Xray techniques
3 ways to measure microbial numbers
Direct counts
Biomass estimation
Culturing
Direct counts
Use a microscope
Can be difficult to distinguish between living and dead cells and debris (aided by fluorescent dyes)
Good for larger cells
Overestimates by up to 1-2 orders of magnitude
Biomass estimation
Measures biomass and total numbers
Can target ATP cell envelope components
Culturing
Isolation of selected media
Targets specific organisms
Plate counts
Underestimates diversity
Methods of measuring microbial activity
Radiotracers → uptake of radiolabelled compounds, degredation of C14 measured
Discoveries in the molecular revolution
rRNA gene isolated
PCR for DNA amplification