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5. Thermohaline circulation is best described as:
a) Cold, oxygen rich waters moving across the ocean bottoms where they remain
b) A worldwide system of rising and sinking water masses due to density changes caused by changes in temperature and salinity.
c) A slow circulation (on the order of a thousand years for one cycle).
d) B and C
e) All of the above
a) Cold, oxygen rich waters moving across the ocean bottoms where they remain
b) A worldwide system of rising and sinking water masses due to density changes caused by changes in temperature and salinity.
c) A slow circulation (on the order of a thousand years for one cycle).
d) B and C
e) All of the above
6. Is the oxygen a limiting factor for organisms in the deep ocean?
a) No, as oxygen diffuses from the epipelagic zone
b) Yes, but only in areas where primary producers (e.g., oxygen-producing
bacteria from deep trenches) cannot sustain efficient production of oxygen
c) No, as the rates of oxygen consumption in deep-water environments are low compared to the supply of waters from polar regions
d) Depends on the proximity to the thermocline
a) No, as oxygen diffuses from the epipelagic zone
b) Yes, but only in areas where primary producers (e.g., oxygen-producing
bacteria from deep trenches) cannot sustain efficient production of oxygen
c) No, as the rates of oxygen consumption in deep-water environments are low compared to the supply of waters from polar regions
d) Depends on the proximity to the thermocline
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