3B Light Availability of Phytoplankton Flashcards
what are the main reasons light reaching the earth varies
latitude
season
time of day
day length
atmospheric conditions
how does latitude impact light reaching earth
poles receive less solar energy cus sun is on horizon, therefore larger impact patch
impact patch
solar rays hitting the earth
smaller impact patch means more solar energy per unit area (vice versa)
how does season impact light reaching earth
tilt of the earth causes size of impact patch to change
summer/winter solstice receives most solar energy at 23.5 degrees N/S
what is the is the tilt of the earth’s rotation axis
23.5 degrees
how does time of day impact light reaching earth
maximum solar energy occurs at noon when it is directly over head
function of time of day for the Equinox
how does day length impact light reaching earth
longer days get more sun; more solar energy
poles in summer have longer days and vice versa
what is one mole of photons called
Einstein (E)
what is photosynthesis dependent on
number of photons in the right wavelength reaching the chlorophyll
what is heating in the water column dependent on
light’s energy (short wavelength heats more)
what do we usually use to measure light
irradiance Watts (Joules/s)
watt is the conversion between Watt and Einsteins usually
1 Watt = 4.4 microE/s
what is low, optimal, and high light for a phytoplankton
< 100 microE/m^2 s
150-200 microE/m^2 s
2000 microE/m^2 s
how does atmospheric conditions affect amount of light reaching earth
clear sky lets more light in vice versa
scattering, absorption prevent light from reaching the surface
what percent of solar radiation reaches the surface on a clear day
80
what percent of solar radiation reaches the surface on a cloudy day
25
what is albedo
fraction of light reflected from a surface
average sinced different wavelengths reflect differently
large for light surfaces, vice versa
what does ocean water albedo depend on
surface roughness
sun light angle
sediment concentraion
chl concentration
do open ocean or coastal ocean have higher albedos
coastal oceans
what happens to light as it moves through water
phons scatter/ get absorbed
what is the attenuation coefficient
measure of how clear the water is
larger k is coastal water
what wavelengths does water absorb more
longer wavelengths
what kind of light is found in deeper water
blue
what is photosynthesis
fixation of CO2 into sugars
releases O2
what is respiration
suagrs being ‘burned’ with O2 to release energy (ATP) for cellular metabolism
CO2 and H2O are released
who uses respiration
all aerobic organisms
what percentage of carbon gets fixed annually by phytoplankton??
50%
how did the creation of phosynthesis change the earth’s evolution?
oxygen level increased from <1% to 20%
CO2 levels fell from >10% to 0.03%
how is phytoplankton biomass measured in the ocean?
hyperspectral radiometer- measures light reaching down the water column, temperature and salinity
clamps shut at a certain depth in the ocean
filter water to measure phytoplankton
primary production definition
stock/biomass of phytoplankton
measure of chl a or C over volume (mg chla/ml)
what is PAR
photosynthetically active radiation
400-700 nm wavelength
primary productivity definition
rate of fixation of organic carbon from inorganic carbon
photosynthesis
in mole CO2 comsumed/ml h or O2 produced/ml h or organic C produced/ml h
do phytoplankton use respiration or photosynthesis
both
respire all the time, photosynthesize in the day
Gross primary productivity definition
rate of PS without accounting for R (total C fixed)
net primary productivity
gross PP - rate of respiration
what can we determing from net PP
amount of C available for phytoplankton growth in higher trophic levels**
how can we measure net PP with a pure phytoplankton culture
bottle exposed to sunlight
how can we measure gross PP with a pure phytoplankton culture
use bottle kept in the dark to measure repiration, add that value to the value obtained from the light bottle measuring net PP
how come the light/dark bottle method doesn’t work for measuring phytoplankton net PP in situ?
because the respiration occuring is not only coming from phytoplankton, it also includes plankton respiration
how can we measure PP at sea?
adding radioactive carbon 14C to the bottle at a given ratio to C
phytoplankton become labelled with 14C