Photosynthesis Primary Production Requirements for photosynthesis sunlight and

Photosynthesis (Primary Production) Requirements for photosynthesis: • sunlight (and chlorophyll to capture energy) • nutrients (nitrogen, phosphorus. . ), space photosynthesis CO 2 + H 2 O C 6 H 12 O 6 respiration + O 2 + H 2 O sugars, fixed carbon

Spatial Distribution • Fig. 2. 1 A spatial classification of marine organisms.

sperm whale 1150 m giant squid 1500 m octopus, 5000 m deepest fish, 8370 m Trieste, 1960, 10, 912 m (Marianas Trench, 10, 923 m)

Light in the ocean Water not very transparent to light Photic zone = where enough light penetrates for photosynthesis Range = few meters in coastal zone, to 200 m in clear, tropical ocean Affected by: transparency of water angle of sunlight hitting the water atmospheric absorption of light

Primary Production in the Sea Factors that Affect Primary Production ôLight in Water. • Fig. 1. 21 Fate of sunlight as it enters sea water. The violet and red ends of the visible spectrum are absorbed first.

Primary Production in the Sea • Measurement of Primary Production Fig. 3. 20 The results of a hypothetical light- and dark-bottle experiment.

Primary Production in the Sea • Fig. 3. 22 This phytoplankton bloom along the California coast, was imaged by Sea. Wi. FS on 10 -11 August, 2003 for true color (left) and for chlorophyll a concentrations.

Primary Production in the Sea • Factors that Affect Primary Production – Nutrient Regeneration. Marine producers rely on a number of mechanisms of nutrient regeneration, such as turbulent mixing, convective mixing, and upwelling.

Primary Production in the Sea ô Nutrient regeneration Fig. 3. 35 Seasonal growth and decline of thermoclines in tropical (top), temperate (center), and polar (bottom) ocean waters.

Primary Production in the Sea • Factors that Affect Primary Production – Nutrient Regeneration. Fig. 3. 36 Coastal upwelling in the Northern Hemisphere.

Productivity in the oceans

Primary Production in the Sea • Factors that Affect Primary Production – Grazing. Small herbivorous grazers routinely occur at such high concentrations that phytoplankton communities may be destroyed over a period of just a few weeks.

Primary Production in the Sea Factors that Affect Primary Production ôGrazing. • Fig. 3. 24 Generalized population changes of a prey species and its predator, oscillating between unlimited (solid) and limited (dashed) phases of population growth.

Contribution to Primary Production in Ocean • One-celled plankton contribute 90%-95% of primary productivity in the ocean • Macroalgae (large, attached algae in the coastal zone) contribute 5 -10%

marine snow = particulate organic matter that originates in the ocean Formed by collisions of debris and large particles, or decaying material, with bacteria and protists attached. Sinks to bottom, carrying nutrients away from surface. e. g. , dead pelagic tunicate covered with bacteria and protists http: //life. bio. sunysb. edu/marinebio/plankton. html

Vertical migration of zooplankton Definition: Migration pattern over 24 hrs, typically upwards at dusk and downwards at dawn, poorly understood, Why migrate? Several hypotheses: *Avoid visual predators during daylight at greater depths and return to shallow zones with abundant food during night *Save energy during non-feeding daylight time in deeper, colder water *Exploit different currents at different depths and remain in same general area, or ascend to fresh, ungrazed food resources the next day Range: up to 200 m (copepods) to 800 m (krill); speed 10 – 200 m/hour http: //www. jochemnet. de/fiu/OCB 3043_25. html

Vertical migration of zooplankton *Consequences: • faster transport of organic matter into deep water: animals capture prey at shallower depths and transport it downwards either as their body mass or fecal products; both are faster than sedimentation *Not all individuals migrate the same range at the same time; population will lose some and gain others, enhances genetic mixing *Samples from same depths taken during day and night will differ in species composition and total biomass http: //www. jochemnet. de/fiu/OCB 3043_25. html

Vertical migration of zooplankton *Deep Scattering Layers: False echosound signals by larger zooplankton (krill, shrimp) and fish, but sometimes also copepods, makes ocean seem to have a false bottom Military interest in this DSL (submarines can hide under the layer) http: //www. jochemnet. de/fiu/OCB 3043_25. html

sexual reproduction Fig. 2. 3 The basic components of sexual reproduction. The chromosome arrangement of each cell is shown to the right.

Sexual vs Asexual Reproduction • Asexual reproduction = no genetic recombination: cloning, budding, fission • Sexual reproduction = reduction division to produce gametes (half of parent DNA), combine to form a genetically mixed zygote different from either parent