- •Contents
- •Preface to the first edition
- •Flagella
- •Cell walls and mucilages
- •Plastids
- •Mitochondria and peroxisomes
- •Division of chloroplasts and mitochondria
- •Storage products
- •Contractile vacuoles
- •Nutrition
- •Gene sequencing and algal systematics
- •Classification
- •Algae and the fossil record
- •REFERENCES
- •CYANOPHYCEAE
- •Morphology
- •Cell wall and gliding
- •Pili and twitching
- •Sheaths
- •Protoplasmic structure
- •Gas vacuoles
- •Pigments and photosynthesis
- •Akinetes
- •Heterocysts
- •Nitrogen fixation
- •Asexual reproduction
- •Growth and metabolism
- •Lack of feedback control of enzyme biosynthesis
- •Symbiosis
- •Extracellular associations
- •Ecology of cyanobacteria
- •Freshwater environment
- •Terrestrial environment
- •Adaption to silting and salinity
- •Cyanotoxins
- •Cyanobacteria and the quality of drinking water
- •Utilization of cyanobacteria as food
- •Cyanophages
- •Secretion of antibiotics and siderophores
- •Calcium carbonate deposition and fossil record
- •Chroococcales
- •Classification
- •Oscillatoriales
- •Nostocales
- •REFERENCES
- •REFERENCES
- •REFERENCES
- •RHODOPHYCEAE
- •Cell structure
- •Cell walls
- •Chloroplasts and storage products
- •Pit connections
- •Calcification
- •Secretory cells
- •Iridescence
- •Epiphytes and parasites
- •Defense mechanisms of the red algae
- •Commercial utilization of red algal mucilages
- •Reproductive structures
- •Carpogonium
- •Spermatium
- •Fertilization
- •Meiosporangia and meiospores
- •Asexual spores
- •Spore motility
- •Classification
- •Cyanidiales
- •Porphyridiales
- •Bangiales
- •Acrochaetiales
- •Batrachospermales
- •Nemaliales
- •Corallinales
- •Gelidiales
- •Gracilariales
- •Ceramiales
- •REFERENCES
- •Cell structure
- •Phototaxis and eyespots
- •Asexual reproduction
- •Sexual reproduction
- •Classification
- •Position of flagella in cells
- •Flagellar roots
- •Multilayered structure
- •Occurrence of scales or a wall on the motile cells
- •Cell division
- •Superoxide dismutase
- •Prasinophyceae
- •Charophyceae
- •Classification
- •Klebsormidiales
- •Zygnematales
- •Coleochaetales
- •Charales
- •Ulvophyceae
- •Classification
- •Ulotrichales
- •Ulvales
- •Cladophorales
- •Dasycladales
- •Caulerpales
- •Siphonocladales
- •Chlorophyceae
- •Classification
- •Volvocales
- •Tetrasporales
- •Prasiolales
- •Chlorellales
- •Trebouxiales
- •Sphaeropleales
- •Chlorosarcinales
- •Chaetophorales
- •Oedogoniales
- •REFERENCES
- •REFERENCES
- •EUGLENOPHYCEAE
- •Nucleus and nuclear division
- •Eyespot, paraflagellar swelling, and phototaxis
- •Muciferous bodies and extracellular structures
- •Chloroplasts and storage products
- •Nutrition
- •Classification
- •Heteronematales
- •Eutreptiales
- •Euglenales
- •REFERENCES
- •DINOPHYCEAE
- •Cell structure
- •Theca
- •Scales
- •Flagella
- •Pusule
- •Chloroplasts and pigments
- •Phototaxis and eyespots
- •Nucleus
- •Projectiles
- •Accumulation body
- •Resting spores or cysts or hypnospores and fossil Dinophyceae
- •Toxins
- •Dinoflagellates and oil and coal deposits
- •Bioluminescence
- •Rhythms
- •Heterotrophic dinoflagellates
- •Direct engulfment of prey
- •Peduncle feeding
- •Symbiotic dinoflagellates
- •Classification
- •Prorocentrales
- •Dinophysiales
- •Peridiniales
- •Gymnodiniales
- •REFERENCES
- •REFERENCES
- •Chlorarachniophyta
- •REFERENCES
- •CRYPTOPHYCEAE
- •Cell structure
- •Ecology
- •Symbiotic associations
- •Classification
- •Goniomonadales
- •Cryptomonadales
- •Chroomonadales
- •REFERENCES
- •CHRYSOPHYCEAE
- •Cell structure
- •Flagella and eyespot
- •Internal organelles
- •Extracellular deposits
- •Statospores
- •Nutrition
- •Ecology
- •Classification
- •Chromulinales
- •Parmales
- •Chrysomeridales
- •REFERENCES
- •SYNUROPHYCEAE
- •Classification
- •REFERENCES
- •EUSTIGMATOPHYCEAE
- •REFERENCES
- •PINGUIOPHYCEAE
- •REFERENCES
- •DICTYOCHOPHYCEAE
- •Classification
- •Rhizochromulinales
- •Pedinellales
- •Dictyocales
- •REFERENCES
- •PELAGOPHYCEAE
- •REFERENCES
- •BOLIDOPHYCEAE
- •REFERENCE
- •BACILLARIOPHYCEAE
- •Cell structure
- •Cell wall
- •Cell division and the formation of the new wall
- •Extracellular mucilage, biolfouling, and gliding
- •Motility
- •Plastids and storage products
- •Resting spores and resting cells
- •Auxospores
- •Rhythmic phenomena
- •Physiology
- •Chemical defense against predation
- •Ecology
- •Marine environment
- •Freshwater environment
- •Fossil diatoms
- •Classification
- •Biddulphiales
- •Bacillariales
- •REFERENCES
- •RAPHIDOPHYCEAE
- •REFERENCES
- •XANTHOPHYCEAE
- •Cell structure
- •Cell wall
- •Chloroplasts and food reserves
- •Asexual reproduction
- •Sexual reproduction
- •Mischococcales
- •Tribonematales
- •Botrydiales
- •Vaucheriales
- •REFERENCES
- •PHAEOTHAMNIOPHYCEAE
- •REFERENCES
- •PHAEOPHYCEAE
- •Cell structure
- •Cell walls
- •Flagella and eyespot
- •Chloroplasts and photosynthesis
- •Phlorotannins and physodes
- •Life history
- •Classification
- •Dictyotales
- •Sphacelariales
- •Cutleriales
- •Desmarestiales
- •Ectocarpales
- •Laminariales
- •Fucales
- •REFERENCES
- •PRYMNESIOPHYCEAE
- •Cell structure
- •Flagella
- •Haptonema
- •Chloroplasts
- •Other cytoplasmic structures
- •Scales and coccoliths
- •Toxins
- •Classification
- •Prymnesiales
- •Pavlovales
- •REFERENCES
- •Toxic algae
- •Toxic algae and the end-Permian extinction
- •Cooling of the Earth, cloud condensation nuclei, and DMSP
- •Chemical defense mechanisms of algae
- •The Antarctic and Southern Ocean
- •The grand experiment
- •Antarctic lakes as a model for life on the planet Mars or Jupiter’s moon Europa
- •Ultraviolet radiation, the ozone hole, and sunscreens produced by algae
- •Hydrogen fuel cells and hydrogen gas production by algae
- •REFERENCES
- •Glossary
- •Index
CRYPTOPHYTA 325
Fig. 9.5 (a) General organization of an ejectisome showing the two subparts. (b) A model of an ejectisome being fired outside of the cell. (c) A drawing of a discharged ejectisome. (After Hovasse et al., 1967.)
(a) |
|
(b) |
|
(c) |
|
|
|
|
|
Ecology
In comparison with other algal groups, the Cryptophyta appear to be especially light sensitive, often forming the deepest living populations in clear oligotrophic lakes (Nauwerk, 1968). In higher mountain and north temperate lakes, cryptomonads and other flagellates are present in the water column throughout the winter. Because of the low light intensity under snow and ice cover, these algae concentrate in surface waters to receive sufficient light from net photosynthesis (Wright, 1964; Pechlauer, 1971). Survival at these extremely low light levels depends not only on a highly efficient photosynthetic system, but also on slow rates of cell respiration at low water temperatures and reduced winter zooplankton grazing. In spring, with the disappearance of snow and resulting sudden increase in light in Arctic and mountain lakes, cryptomonads suffer considerable light stress, such that the biomass maximum moves to deeper waters (Kalff and Welch, 1974).
Cryptophytes will often undergo diel vertical migrations with an amplitude less than 5 meters. In small humic forest lakes, species of Cryptomonas are positively phototactic in the morning, moving into the phosphorus-depleted upper layer. Later in
the day the cells move away from the uppermost water layer, avoiding high levels of irradiance, and move into the phosphorus-rich hypolimnion (Knapp et al., 2003). A further advantage of this cycle is the reduction of grazing pressure by zooplankton (for which cryptophytes are a preferred food) (Loret et al., 2000) which often migrate in the reverse direction.
Cryptophyte algae are mixotrophic, capable of phototropy and phagotrophy. Phagocytotic ingestion of bacteria is thought primarily to provide a source of phosphorus and nitrogen in nutrientlimiting conditions (Urabe et al., 2000). These algae are also chemotactic, swimming in a straight line until they reach a nutrient patch, at which time the cells stop and tumble in the volume of high-nutrient concentration (Lee et al., 1999).
Cryptophytes are the dominant algae in the freshwater lakes of Antarctica. The best studied lakes are those in the McMurdo Dry Valleys (Fig. 9.6) (Roberts and Laybourne-Parry, 1999; McKnight et al., 2000). The McMurdo Dry Valleys are the largest ice-free areas in Antarctica (about 4000 km2) and constitute a polar desert with temperatures ranging from 45 C to 5 C. These valleys remain ice free because the Trans-Antarctic Mountains not only block the flow of the ice sheet, but also block the flow of moisture, the valleys