Answer:Water masses give a very robust representation of the thermohaline state of the ocean and ocean circulation. ... This water body shows extremely stable vertical stratification, and its water density changes from ~1,011 kg/m3 at the ocean surface to ~1,016 kg/m3 at 100‐m depth.
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Less, because a glass of water can be from around 8-16 ounces in its expectatio,, but 5 mililiters isn't even a mouthful, so of course it is much less than one expects
D- the relationship benefits both the bee (food) and the flowers (growth and pollination)
