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_% of global photosynthesis takes place in the ocean
50
Plankton
small organisms that drift with the ocean currents
Types of phytoplankton
diatoms (require silica)
flagellates: motile so they avoid sinking in calm waters
Photosynthetic bacteria: can grow at very low nutrient concentrations
NPP
difference between amount of CO2 taken into cell by photosynthesis and the amount of CO2 exported from the cell by respiration
Compensation light level
light intensity whereby CO2 gained by photosynthesis just compensates for CO2 lost by respiration (NPP = 0)
At high light levels, phytoplankton are
photoinhibited
Main source of iron to surface ocean
dust blowing off of continents
Shift from __ limitation to _ in North pacific Subtropical gyre
nitrogen; phsophate
Warm, nutrient poor water in subtropics is due to
surface convergence of the ekman layer
Subtropical gyre productivity is characterized by
low primary productivity per square meter and low seasonal variation
Tidal mixing
occurs in shallow continental shelf regions, seasonally steady, occurs as tide wave motion accelerates horizontally and is squeezed on the shallow shelf
Coastal upwelling from ekman transport features
seasonally variable, greatly enhances upward movement of deep water that is rich in nutrients
Critical depth
Depth at which mixing occurs where phytoplankton lose the same amount of carbon they gain in one day (mixing below this depth means loss>gain)
Spring phytoplankton bloom progression in westerly winds region
Winter: light limited, nutrient abundant
Spring: light abundant, nutrients abundant
Summer: light abundant, nutrient limited
Fall: light modest, nutrients modest
Oceanic NPP is _% of global NPP
46
_% of annual global ocean primary production is coastal
26
_ most often limits the growth of phytoplankton in the ocean, but and limit growth in certain important regions
nitrogen, iron, phosphate
hawaii is _ limited
phosphate
the southern ocean is _ limited
iron
Nekton
able to swim against ocean currents
Holoplankton
organisms that live their entire lives as plankton (copepods, some shrimp, arrow worms, some jellyfish)
Meroplankton
organisms that spend only part of their life as plankton (crabs, barnacles, oysters, fish larvae)
Exploitation efficiency
the efficiency w which a consumer population is able to find, capture, and ingest all of the potential prey present in their environment
Gross production efficiency
physiological/biochemical efficiency of converting ingested prey into consumer biomass
Trophic transfer efficiency
EE x GPE
Big phytoplankton means
short, efficient food chains
Bacteria make up more than _% of the living biomass in the ocean
50
Oligotrophic
naturally low plant nutrient concentrations (subtropical gyres)
Eutrophic
pelagic environment that has naturally high plant nutrient concentrations (coastal upwelling zones)
As a general rule, preferred prey size is _% of the consumer’s size
10
Study methods for plankton
transmission light microscopy and culture-plate colony counts
Epifluorescent microscopy
allows study of bacterial abundance and distinction between autotrophic and heterotrophic flagellate cells
Source of carbon and energy for heterotrophic bacterial growth
grow on DOM released from phytoplankton by natural leakage, cell senescence, or sloppy feeding by large zooplankton
The microbial loop
describes the role microbes play in the marine carbon cycle
Prochlorococcus
very abundant bacteria in the ocean, autotrophic with chlorophyll. Single handedly contributes more than 25% of ocean primary production, growth is expected to decline due to global warming
Heterotrophic bacteria are/are not highly abundant in all ocean environments
are
Most of living biomass in open-ocean is in the form of
bacteria
When phytoplankton are small…
grazers are small and fecal material is small, so it cannot easily sink and the carbon decomposes and is respired back to CO2 - inefficient biological pump
Vertical zonation
communities are divided into distinct bands [zones’ that are at characteristic heights in the intertidal
What sets the upper limit to species distributions in the intertidal?
Physical stresses such as desiccation, sunlight, temperature, and emersion
What sets the lower limit to species distributions in the intertidal?
Biological interactions such as competition for space and predation
Vibrio pectenicida
bacterial pathogen responsible for die-off of sunflower starfish
Corals receive -% of energy from zooxanthellae
60 - 90
Optimal temperature for corals
26-28
Restricted temperature range for corals
18-36Â
Sunlight limits coral growth to a depth range extending from the ocean surface down to maximum of about _
25 m
_% of corals were exposed to bleaching
84
Pakicetus
hoofed mammal that is often classified as the earliest whale. lived about 53 mya, wolfish appearance.
How do we know pakicetus is an ancestor of whales?
ear region shape in skull
Modern whales
odonticeti and mysticeti
Baleen
used for gulp, skim (surface) feeding, and bottom plowing
First mysticeti appeared about _ mya due to..
35; a change in foodchain structure
Pacific humpback migration
summer feeding at high latitudes
winter calving at low latitudes
odontocetes
produce rapid bursts of clicks and whistles, used for echolocation and communication
Mysticetes
vocalizations primarily used in sexual selection, some echolocation (but only for depth/barriers, not prey)
Spectrograms
used to visualize vocalizations
Sources of anthropogenic sound in the ocean
naval operations
commercial shipping
oil exploration
half of orcas might be loss within to years due to
30 to 50; PCB accumulation
Treaty of Neah Bay
gave makah tribe right to hunt whales in exchange for land
International Convention for the Regulation of Whaling
agreement to set quota levels based on findings from scientific committtee
Latent heat of fusion
amount of heat to change from solid to liquidL
latent heat of vaporization
heat to convert 1 gram of water to water vapor
Specific heat capacity of water
amount of heat to raise 1 gram of water by one degree C
_% of excess heat energy accumulated in the earth system is taken up by the ocean
93
During condensation, latent heat is
released to the atmosphere
During evaporation, latent heat is
removed from the ocean
Hydrogen bonds below 100C
are strong enough to allow some individual water molecules to temporarily bind with others to form liquid water
Amount of salt in the ocean fluctuates T/F
F
input and export of salt in oceans through:
weathering
calcification and deposition into sediments
Conservative constituents
only varied by physical exchange processes at the surface (salinity, temperature, inert gas concentration)
non-conservative constituents
altered by chemical or biological processes that occur in the water column (biological uptake, phytoplankton nutrients)
Dissolved plant nutrients are low/high in surface waters because of…
low; uptake by phytoplankton
atlantic ocean is low in
phosphatepa
pacific ocean is high in
phosphate
old water is low/high in phosphate because…
high; it has had more time to accumulate biological matter (debris)
There has been a _% of oxygen in the ocean since the 60s
2
Global warming will increase/decrease the strength of the thermocline, lowering/raising oxygen content of the oxygen minimum zone
increase; lowering
Flux of CO2 across air-sea interface
deep ocean water rich in CO2 flixes CO2 out of ocean, overall there is a net flux of CO2 into oceanO
Ocean has uptaken _% of all CO2 emitted since industrialization
30
Ocean acidity has increased by _% since industrialization
26
Ability of ocean to uptake CO2 will increase/decrease due to…
decrease; increasing acidity and temperature
which region will acifify fastest?
polar regions and coastal upwelling regions
Pteropod
a type of zooplankton at the base of the marine food web that has a protective shell
Ocean acidity will increase by _% by the end of the century
170
Ocean acidification is irreversible on timescales of at least _ of years
tens of thousands