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Test #2 Results by Next Week
From Friday’s The Blue Planet
PREDATOR
PREY
Sardines
Flying fish
Surgeonfish eggs
Yellowfin tuna eggs
PLANKTON
NUTRIENTS
Striped tuna, Bluefin tuna
Marlin
Sei whale
Manta ray, Ray
Pacific Mackeral
Spotted Dolphin
Sailfish
Blue Shark
Deepwater crab
• Sunfish with half-moon fish and seagull
Wahoo
• Fish with flotsam
The Marine Food Web
Chapter 10:
Biological Productivity
Conditions for Life in the Sea
Consider the main biochemical reaction for
life in the sea, and on earth in general:
6H2O + 6CO2 + energy + nutrients = C6H12O6 + 6O2
Focus on left side of equation
What is in short supply in the sea and thus
limits the amount of life in the ocean??
Absorbing Nutrients
6H2O + 6CO2 + energy + nutrients = C6H12O6 + 6O2
Phytoplankton
are
base of the food chain
Most important
primary producers of
complex sugars and
oxygen
Lauderia sp.
The Marine Food Web
Absorbing Nutrients
Nutrients
absorbed by
plants through
diffusion across a
semi-permeable
membrane
Lauderia sp.
Diffusion:
molecules move from high to low concentrations
Which Nutrients are in Short
Supply?
Nitrogen
(N) as Nitrate NO3 (-2)
Phosphorus (P) as Phosphate PO4 (-2)
Silicon (Si) as Silicate SiO4 (-2)
Phosphate and Nitrate in the Pacific
Silicate in the Pacific
Biolimiting Nutrients
N,
P, and Si are exhausted first in Eq.
surface waters during photosynthesis
Essential to the growth of phytoplankton
If these biolimiting nutrients increase in
sea water, life increases
If these biolimiting nutrients decrease in
sea water, life decreases
Where would you expect to find the highest
biomass in the Pacific??
CZCS Global Primary Production
How Does Nutrient Distribution Compare w/
Dissolved Oxygen?
Dissolved O2 Reverse of
Nutrients
O2
is high in the
surface and mixed
layer
O2 decreases to a
minimum at base of
thermocline
O2 then steadily
increases with depth
Why is the Concentration of
Oxygen High in the Mixed Layer??
Hint #1: How and where is oxygen produced
in the sea???
6H2O + 6CO2 + energy + nutrients = C6H12O6 + 6O2
Hint #2: How can oxygen be mixed
downward from the atmosphere into the
ocean?
How is Oxygen Removed from the
Thermocline & Slightly Below??
Dead and decaying organic matter sinks
downward from surface waters
Rate of sinking decreases
as it encounters the cold,
dense water of the
thermocline
Material decays (oxidizes)
at the thermocline, which
strips O2 out of the water
and returns nutrients to
the sea
Cold, nutrient-rich water
of the thermocline is
returned to sunlit surface
waters by way of
upwelling
CZCS Global Primary Production
Marine Ecology
Chapter 9
Basic Ecology
physical
and chemical parameters
affecting distribution and abundance
An ecosystem includes both the living
(biotic) and non-living (abiotic) portions
of the environment.
– Examples include: salt marshes, estuaries,
coral reefs, the North Pacific Gyre.
Classification of Organisms
by Environment
horizontal:
neritic | oceanic
vertical:
– epipelagic (top) / euphotic (good)
– mesopelagic (middle) / disphotic (low)
– bathypelagic (deep) / aphotic (without)
– abyssopelagic (“bottomless”)
Divisions of the Marine Environment
Figure 9-1
Classification of Organisms
by Lifestyle
Scientists
have established another
classification scheme to categorize biota
on the basis of lifestyle. The major groups
are:
– plankton (floaters)
– nekton (swimmers)
– benthos (bottom dwellers)
Plankton
weak
swimmers, drifters, unable to
counteract currents.
– Phytoplankton (plants)
– Zooplankton (animals)
Nekton
active
swimmers capable of counteracting
currents.
– Fish
– Squids
– Reptiles
– Birds
– Mammals
Distribution of
Marine Lifestyles
16.7%
of Earth’s animals are marine
2% inhabit pelagic environment (most of
the oceans are cold and dark)
98% are benthic!
Benthos
Epiflora
or epifauna live on the sea
bottom.
Infauna live in the sea bottom.
Benthic
plants - restricted to shallow
waters (light)
Benthic animals occur everywhere from
shallow depths to the deep sea.
Research Video Clips:
“Live fast, die young...”
Basic Ecology
physical
and chemical parameters
affecting distribution and abundance
an ecosystem includes both the living
(biotic) and non-living (abiotic) portions
of the environment.
Temperature, salinity …
Hydrostatic Pressure
Pressure
caused by the height of water.
Function of water height and water density
Pressure generally increases at a rate of 1
atm per 10 m of water.
( or 16 psi per 10 m depth)
Think You’re Under
Pressure Now?
Hydrostatic Pressure
(Cont.)
enormous
in the deep sea yet animals live
there.
Animals do not contain gases.
However, mesopelagic fish which have
gas-filled swim bladders to help maintain
neutral buoyancy
– unable to move rapidly between depths
– pressure change could cause bladder explode.
Oregon Coast Field Trip Sat., June 2nd
dusk.geo.orst.edu/oceans/field.html
Be
here by 7:15
a.m.
7:30 - Busses leave
from Wilkinson lot
8:30 - Seal Rock
volcanic rocks and
tide pools
10:00 - Travel to
HMSC
10:30
- HMSC
Visitor Center
12:00 - Lunch on
HMSC grass (bring
your own)
12:30ish - Return
to Corvallis
Back by ~2:00
Required Field Trip Guide
dusk.geo.orst.edu/oceans/field.html
Answers to bolded questions in guide
–Turn assignment in to your TA
–Due by 5:00 p.m., June 8th
–This constitutes LAB 9