Cyanobacteria (Blue – Green Algae)
· Cyanobacteria, commonly known as Blue Green
Algae, are ancient Photosynthetic Prokaryotes with significant Ecological and
Evolutionary roles.
· Example
- Anabaena, Nostoc, Oscillatoria, Spirulina,
Gloeocapsa, Microcystis, Synechococcus and Prochlorococcus.
· Number
of Species – Approximately
8,000 species are estimated, though taxonomic debates persist. Around 5,185
species have been formally categorized into seven orders, including
Chroococcales and Synechococcales.
· Habitat
ü Freshwater:
Lakes, ponds, rivers.
ü Marine:
Oceans, seas, intertidal zones.
ü Terrestrial:
Moist soils, rocks, tree bark.
ü Extreme
Environments: Hot springs, hypersaline environments, deserts, polar
regions.
ü Symbiotic
Relationships: With Plants (e.g., Azolla), Fungi (Lichens),
and some animals.
· Mode
of Nutrition – Photoautotrophic (primary mode, using sunlight, CO₂, and water). Some species fix Atmospheric nitrogen (N₂) and convert into Ammonia via Heterocysts
(e.g., Anabaena). A few show Mixotrophy (combining Photosynthesis and
Organic carbon uptake).
· Mode
of Reproduction – Asexual reproduction only (no sexual reproduction):
a)
Binary fission - Simple cell
division form the Mother cell.
b)
Fragmentation - Breaking of filaments or colonies into
smaller pieces that grow into new individuals.
c)
Akinetes - Specialized, thick-walled, dormant cells formed under harsh
environmental conditions. They serve as a survival mechanism, allowing the
organisms to withstand unfavorable conditions and re-emerge when conditions
improve.
d)
Hormogonia - Specialized, short filaments released
from cyanobacteria for vegetative reproduction. They are motile and can
move via gliding motility, often requiring a wet surface or viscous
substrate like agar. Hormogonia are formed when cyanobacterial filaments
break into smaller fragments between necridia (dead cells). These
fragments then detach and become motile, eventually growing into new
filaments.
· Mode
of Respiration
ü Cyanobacteria are generally Aerobic,
meaning they require oxygen for respiration (Oxygenic Photosynthesis). They
have a unique system where Photosynthesis and Respiration can occur in the same
Thylakoid membranes, but these processes are often separated temporally
(Photosynthesis during the day or in the light and Respiration at night or in
the dark).
ü Some can also perform Anaerobic
respiration or Anoxygenic Photosynthesis under Sulfur-rich, low-oxygen
conditions.
· Type
of Photosynthesis – Oxygenic photosynthesis (like plants).
· Pigments
a)
Chlorophyll a - Green pigment
for photosynthesis.
b)
Phycobilins - Water-soluble
pigments located in Phycobilisomes attached to the Thylakoid membranes. These
include:
ü Phycocyanin: Blue
pigment, giving many Cyanobacteria their characteristic Blue-green color.
ü Phycoerythrin: Red
pigment. The relative amounts of Phycocyanin and Phycoerythrin can vary
depending on light conditions, leading to different colors (greenish, bluish,
reddish-brown).
c)
Allophycocyanin - Another type of
Blue pigment involved in Energy Transfer to chlorophyll a.
d)
Carotenoids (β-carotene & Xanthophylls) -
Yellow and Orange pigments that also participate in light absorption and
photoprotection.
· Electron
Donor – Water (H₂O) (in Oxygenic photosynthesis). In Anoxygenic
photosynthesis (rare), Hydrogen sulfide (H₂S) may be used.
· By-products
a)
Oxygen (O₂) (major by-product of oxygenic photosynthesis).
b)
Organic compounds (e.g., sugars).
c)
Some produce Toxins (e.g., Microcystins,
Cylindrospermopsin) in Harmful Algal Blooms.
· Photosystem
– Both Photosystem I and Photosystem II.
·
Ecological role
ü Primary
producers: Contribute significantly to global carbon fixation.
ü Nitrogen
fixation: Enrich soil/water with bioavailable nitrogen (Example
– Anabaena sp.).
ü Oxygen
production: Early Earth oxygenation (Great Oxygenation Event).
ü Bioindicators: Indicate water quality and environmental
conditions.
ü Harmful
blooms: Toxin production and Eutrophication disrupts
ecosystems and human health.
ü Symbiosis: Partner with fungi (Lichens), plants (Azolla),
and Corals to enhance host Nutrient uptake.
ü Carbon sequestration: Contribute to global carbon cycling in
oceans and soils.
ü Formation of Microbial Mats and
Stromatolites: They can
form extensive microbial mats in various environments and contribute to the
formation of stromatolites, ancient layered structures.
Comments
Post a Comment