Energy Capture and Allocation Flashcards
Primary Production
The formation of organic matter through the trapping of light energy and assimilation of inorganic elements
Mangroves, Salt Marsh, and Seagrass Coverage
These ecosystems cover less than 0.5% of the marine area yet account for between 50 and 71% of carbon storage in marine sediments
Primary Producers of the Ocean
Seaweeds (macro-algae), seagrasses, and microscopic algae (phytoplankton) and bacteria
Algal Bloom
When phytoplankton rapidly proliferate under proper light and nutrient conditions
Needs of Photosynthetic Organisms
Light, carbon dioxide, oxygen, macro-nutrients (phosphate, nitrate, silicate)
Oligotrophic
Low concentrations of nutrients for algal blooms and low primary productivity (<100 g carbon m-2 per year)
Eutrophic
High concentrations of essential nutrients for algal blooms and high primary productivity (300 to 500 g carbon m-2 per year)
Mesotrophic
In between eutrophic and oligotrophic waters (100 to 300 g carbon m-2 per year)
Eutrophication
Rapid increase in the primary productivity of an area, often caused by a rise in an essential inorganic nutrient like nitrogen or phosphorus
Biomass-Limiting
The nutrients are so exhausted that no more mass can be produced
Rate-Limiting
The nutrients limit the rate of new biomass production by their rate of supply
Diffusive Boundary Layer
Surrounds each cell or surface in water and restricts the molecular diffusion and the movement of water // Smaller cells have a thinner/lower DBL and have a physiological advantage in low nutrient waters
HNLC Areas
High nutrient, Low-chlorophyll areas are potentially limited by light or depletion of standing stocks, yet more likely by the absence of iron (a necessary micro-nutrient for primary production)
Succession of Phytoplankton Species
Controlled by a complex mosaic of factors, like temperature, irradiance, growth rates, and nutrient supply
Governing Factors of Marine Primary Production
Light, nutrients, stability, and mixing
Tropical and Subtropical Areas (PP)
Normally have permanent thermal stratification and less mixing, so more nutrient-limiting, resulting in lower levels of productivity that are fairly consistent
Polar Areas (PP)
Significant mixing which brings good nutrient concentrations, yet more light-limiting through irradiance, and limited times of production
Temperate Waters (PP)
Seasonal fluctuation of primary productivity due to the complex range of factors, so low in the summer/winter and higher in the spring/summer
Coriolis Effect
Deflects currents northwards in the northern hemisphere and southwards in the southern hemisphere, drawing surface waters away from the equator and allowing for upwelling to occur there
Coastal Waters // Continental Shelf Waters (PP)
These waters have the highest primary productivity, shallow enough for good light and receive nutrients from river sources
Marine and Terrestrial Primary Production
Roughly the same, at 50 Pg of carbon each per year
Primary Production
Usually defined by the amount of bacterial, algal, or plant biomass built up through the process of photosynthesis over time