latitudinal gradient
depth gradient
coastal to open water gradient
intensity of sunlight
amount of daylight hours
near the poles it is less intense than near the equator
based on the latitude we're at and the season we're in
time of day
amount of cloud cover
latitude
season
reflects - hits a particle and reflects the light
scatters - hits a particle and goes in a random angle
absorbs - lights sucked in
the intensity of light decreases
wavelength changes
light
temperature
pressure
amount of dissolved gas
amount of dissolved nutrients
surface mixing
to get bigger
gaining new physical and behavioral traits
nitrates
phosphates
calcium
magnesium
producers absorb nutrients from the environment in a process called uptake
in the photic zone, they uptake nutrients reducing their overall abundance
as organisms die, they are decomposed and release nutrients with sinks
divided into 3 zones
littoral zone
pelagic zone
neritic zone
area between high tide and low tide
characterized by extreme shallowness of water
this change in depth of water causes extreme environmental conditions
wet to dry
large temperature change
swings in salinity
area above the continental shelf
the area tends to be well lit
temperature tends to be fairly stable
the area tends to be well mixed
the area over continental slope and the abyssal plain
characterized by extreme depth of water