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Oceans can be layered with
upper waters that are distinctly less dense than deeper waters.
This causes a physical "barrier" to form, separating the surface
from the nutrient-rich colder waters below. At
left (<<<), the thermocline
-- a thin layer where temperature changes abruptly -- separates
shallow from deep waters. The lower plot
(<<<) shows how low salinity water can "float"
above high salinity water.
Under mixed conditions, temperature
and salinity DO NOT vary much from shallow to deep. During high
mixing, phytos are suspended in a turbulent
ocean, spending time in both the sunlit upper ocean and the deeper
dark zone.
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#1) Discover whether
stations had layered or mixed conditions when sampled.
STEP A: Look at each season's temperature profiles
(background)
for: Station 3 | Station
4 | Station 5 | Station
6 | Station 7 | Station
8 | Station 9 | Station
10 | Station 11 | Station
12
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- At these stations, is the salinity profile consistent
with the temperature profile for that season? In other words,
do stations with layered temperature profiles also have layered
salinity profiles? And do stations with "well-mixed" temperature
profiles also have "well-mixed" salinity profiles?
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#2) Compare the top of the thermocline with
the depth of fluorescence.
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- Compare the depths you found in Step A (the
top of the thermocline) with those you found in Step B (where
fluorescence has dramatically diminished).
- Is the top of the thermocline at the depth where
fluorescence declines sharply? Can you
guess why or why not?
- Quickly examine a few (6 or so) fluorescence
profiles for mixed conditions (based on Activity #1 results):
are their traces different from those of layered stations? Why
or why not?
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#3) Examine whether phytoplankton
species diversity is tied to layered versus mixed ocean conditions.
STEP B: When possible, compare these findings
with whether each station is "layered" or "mixed"
during that season (analyzed during Activity
#1).
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One view of the relationship between
physical conditions and phytoplankton is shown at right (>>>).
According to your Gulf of Maine research, are certain types of
phytoplankton thrive better under layered conditions? How
about mixed conditions?
Does the diversity of "successful
species" change from season to season? Why or why not?
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