MIDTERM 1 Flashcards
chlorophyll
pigment that plays a key role in photosynthesis
Why does distribution of surface [chl] vary seasonally?
1) sunlight: longer daylight hours and more intense sunlight means higher chl production in surface waters
2) temperature: warmer temperatures generally promote faster growth rates for phytoplankton
3) nutrient availability
What units are used to express [chl] and what is the typical range?
Units: mg/m^3 or micrograms / L
Typical range: 0.05 - 50 mg/m^3
What is the range of annual oceanic primary productivity?
less than 10 gC m-2 y-1 to over 300 gC m-2 y-1
How does productivity vary and why is it distributed that way?
Western sides of continents are often more productive due to upwelling (wind patterns and ocean currents bringing nutrient-rich waters from the deep ocean to the surface_ as well as coastal currents (currents transporting nutrients from offshore regions to coastal areas). The middle of gyres is often low productivity due to nutrient depletion.
cold-core ring
forms when a meander in an ocean current or frontal zone pinches off, creating a closed circulation pattern – cooler nutrient rich water from deeper ocean layers becomes isolated within the closed circulation of the ring. Rotate counterclockwise (Gulf Stream)
warm-core ring
rotating warm masses of water surrounded by colder water – rotate clockwise (Sargasso sea)
upwelling
near the equator, water is deflected polewards causing water to be upwelled. on the western shores of continents, strong winds and the movement of the water towards the equator caused water to be upwelled.
How do we make ocean measurements (profile)
Using a rosette with Niskin bottles and a CTD for measuring Conductivity, Temperature, and Depth (pressure)
The maximum depth of light penetration shifts from …
blue to yellow as light penetration decreases.
critical depth model
a simple but powerful model for predicting the timing of the spring bloom in the North Atlantic. It is the depth at which the integrated amount of C fixed and C respired are equal for the water column, meaning there is no increase of biomass
Rober Koch (1881)
- cultured bacteria on gelatine
- known for Koch’s postulates
Certes (1884)
- cultivated aerobic bacteria from 5100 m sediments
Russell (1893)
- quantified bacteria in the water column and sediments
- 10s of bacteria / mL of water
- 10^4 to 10^5 bacteria / cc of sediment
Fischer (1880s)
- isolated bioluminescent bacteria from water and fish light organs
- discovery of the lux system
Claude Zobell (1930s-60s)
- distribution and physiology