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oceanography 31

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Photosynthetic organisms – microscopic algae
⬢ Most microscopic algae are phytoplankton. ⬢ Produce food directly or indirectly for 99 % of marine animals. ⬢ We mentioned diatoms (silica shells), coccolithophores (small calcareous plates), dinoflagellates (have 2 flagellae for locomotion). ⬢ Did not mention photosynthetic bacteria.
Photosynthetic bacteria
The very small Prochlorococcus may form half of the ocean’s photosynthetic biomass, making it the most abundant photosynthetic organism on Earth.
Factors affecting primary productivity
⬢ Availability of solar radiation. ⬢ Availability of nutrients. ⬢ Predation
Energy flux:
• Solar radiation – light penetrates the atmosphere, despite its thickness of over 80 km. However, very little light by 1 km depth in the ocean. • Photosynthesis restricted to the euphotic zone which extends from the surface to the compensation depth for photosynthesis. • The compensation depth for photosynthesis is where net photosynthesis is zero (i.e. gross photosynthesis = respiration) • The compensation depth for photosynthesis is approximately 100 m in the open ocean and may be less than 20 m in the coastal zone where the waters are more turbid.
Two factors necessary for photosynthesis; solar radiation and nutrients.
⬢ In open ocean solar energy penetrates deeper into the water column, but the concentration of nutrients is low. ⬢ In coastal waters the light penetration is less, but the nutrient concentration is much higher. ⬢ Because the coastal zone is much more productive, nutrient availability must be the most important factor affecting the distribution of life in the oceans. ⬢ Remember coastal upwelling.
Divide gross primary production into two components:
• New production – generated using nutrients brought in from outside the local ecosystem by processes such as upwelling. • Regenerated production – generated using nutrients that are recycled within the system.
Productivity in tropical Oceans
⬢ Solar radiation high, but nutrients low as the sunlit, surface waters are separated from deeper nutrient⬐rich waters by a permanent thermocline. ⬢ Productivity occurs at a relatively low, steady rate. ⬢ Exceptions includes areas of equatorial upwelling, coastal upwelling and coral reef ecosystems.
Production in temperate oceans
• Winter – nutrients concentrations highest, water column well mixed and isothermal, light relatively low. Light limited. • Spring – Compensation depth for photosynthesis increases as sun is higher in the sky, spring bloom occurs. Spring bloom becomes nutrient limited as a thermocline develops. • Summer– more solar radiation, but phytoplankton nutrient limited as a strong thermocline forms at a depth of about 15 m. • Fall – solar radiation reduced as sun gets lower in the sky, thermocline becomes unstable and breaks up. Nutrients return to surface water resulting in a fall bloom. Fall bloom becomes light limited.
Fate of production
• 90 % of production generated in the euphotic zone is decomposed within this zone. • 10 % sinks to deeper water. • 1 % of this accumulates on the ocean floor and may be buried. • Biological carbon pump – removal of carbon from the surface to deep waters.
Biotic community
assemblage of organisms that live together in a defined area.
Ecosystem
The biotic community and its abiotic environment, exchanging energy and chemicals.
3 categories of organisms
Consumers • Herbivores – feed directly on plants or algae. • Carnivores – feed on other animals. • Omnivores – feed on both. • Bacteriovores – feed on bacteria. Produce • Detritus – waste products, dead and decaying remains of organisms. Used by • Decomposers – break down detritus for their energy requirements. Nutrients released into the environment and become available to autotrophs.
Trophic Levels
– Producers belong to the first trophic level (grass) – primary consumers to the second (sheep) – secondary consumers to the third (wolves)
Conclusion:
⬢ It takes a lot of light to keep a killer whale going. ⬢ Can harvest more small fish (lower trophic level) than large ones.

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