Classifying, describing, identifying and naming the organisms
Physical traits used to classify bacteria
Shape (cocci, rod, spiral, filamentous)
Number of cells (single, two, tetra, chain etc)
Cell wall (Gram staining)
Growth temperature range
Anaerobic/aerobic/facultative anaerobe
Mode of metabolism
Modern classification started with Carl Linnaeus in 18th century
Scientific nomenclature
2 scientific (latin) names: 1st name is genus, 2nd name is species
Examples of scientific names: Homo sapiens, Escherichia coli
16S rRNA
A sequence of DNA that encodes the RNA component of the smaller subunit of the bacterial ribosome
Carl Woese rewrote the tree of life
Why use 16S rRNA?
Present in all cells
Conserved across all prokaryotic species
Essential for cell survival
Changes at DNA level acquired slowly
Unlikely to go through lateral or horizontal transfer
The three domain model is the accepted biological classification
Woese's classification emphasises separation between Bacteria and Archaea
The split is based on genetic rather than morphological traits
Comparison of 16S rRNA sequences
Methanococcus
Thermococcus
E.coli
Humans
Analysis of SSU rRNA allows construction of "The Tree of Life"
Prokaryotic Microbes
Bacteria
Archaea
Eukaryotic Microbes
Fungi
Protozoa
Algae
Principle differences between prokaryotic and eukaryotic microbes
Size of cell
Nucleus
Membrane-enclosed organelles
Flagella
Cell membrane
Cell wall
Ribosomes
Bacterial Classification
Cyanobacteria
Proteobacteria
Firmicutes
Archaea
More closely related to humans than bacteria
Found in extreme environments
Have structural, chemical and metabolic adaptations
Archaeal Diversity
Euryarchaeota
Crenarchaeota
Asgard
DPANN
TACK
Microbial Eukaryotes
Unicellular and multicellular eukaryotes, have membrane bound organelles, include plants, animals etc.
Microbial Eukaryotes
Fungi
Protozoa
Algae
Unicellular Eukaryotes
Typically microscopic (from 2.5 µm)
Single-celled, sometimes form colonies with division of labour
Multicellular Eukaryotes
At least 20 cells
Typically have tissues and organs
Can be self-propelled
Classification of Microbial Eukaryotes
Environment (terrestrial, freshwater, marine)
Body size (picoplankton, nanoplankton)
Functional ecology (phytoplankton)
Feeding strategy (photosynthesisers, predators)
Trophic level of Microbial Eukaryotes
Autotrophic (produce own carbon compounds)
Phagotrophic (ingest particles)
Plankton
Typically small, multicellular organisms, especially animals, critical part of aquatic ecology, present in huge numbers and major components of ecosystems
Dinoflagellates
Unicellular protists, marine plankton but can be found in freshwater, photosynthetic and heterotrophic, about 1555 described species
Diatoms
Group of algae, very large in size, account for ~20% of global photosynthetic carbon fixation, unicellular but can form filaments and stars, have calcium carbonate shells, very important for carbon cycle
The fossil record is a tool to investigate and understand paleoclimates and how climate has changed
Freshwater diatoms and other planktonic micro-algae are important indicators of water type and conditions
The fossil record is an important source of historical data on the nature of the water, changes in environment, and past changes in nutrients
55 described species!
Diatoms
Group of algae (very common)
Diatoms
Very large in size and significant because they account for ~20% of global photosynthetic carbon fixation
They are unicellular but can form a shape of filaments, stars
They have calcium carbonate shells
Very important for carbon cycle
A teacup of Lake Windermere water contains approx. 2 million Asterionella
Annual production 400 tons!
Fossil record
A tool to investigate and understand paleoclimates, i.e. the Earth's past climates and environments, and how climate has changed
Freshwater diatoms and other planktonic micro-algae
Important indicators of water type and conditions
Information available from fossil record
The nature of the water where they live
Changes in environment e.g. changes in sea levels reflected by species in saline vs brackish waters
Indicate past changes in nutrients in the water. Diatoms from nutrient-poor lakes (oligotrophic) are different in abundance and species composition than those that grow in nutrient-rich (eutrophic) lakes
pH variation over time e.g. acidification of lakes
Information available from fossil record
The community itself, e.g. the species that live in the sampled area. Different aquatic animal communities thrive in different salinity concentrations
The community assemblage (composition and abundance): how it varies over time and season
The morphology of shells - smooth, lobate, chamber size, spines. No spines in low oxygen concentrations