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55 Cards in this Set
- Front
- Back
North Pacific gyre
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clockwise with california current (eastern boundary current), to north equatorial current, into the western boundary current of kuroshio and then the north pacific current.
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South Pacific gyre
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counterclockwise with the south equatorial current into the australian current and then the peru/ humboldt (cold, broad water along the south america which enter the s. euatorial.)
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West wind drift
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encircles the globe, which merges the atlantic, pacific and indian oceans.
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south pacific
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islands between hawaii and australia. This is the riches and most diverse area for marine forms
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east pacific barrier
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open water from hawaiin islands to the coast of north,central and south america. Difficult physical barrier for many organisms
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North Pacific gyre
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clockwise with california current (eastern boundary current), to north equatorial current, into the western boundary current of kuroshio and then the north pacific current.
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South Pacific gyre
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counterclockwise with the south equatorial current into the australian current and then the peru/ humboldt (cold, broad water along the south america which enter the s. euatorial.)
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West wind drift
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encircles the globe, which merges the atlantic, pacific and indian oceans.
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south pacific
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islands between hawaii and australia. This is the riches and most diverse area for marine forms
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east pacific barrier
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open water from hawaiin islands to the coast of north,central and south america. Difficult physical barrier for many organisms
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Current
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river in a larger body of water (sea). Have surface currents which extend few hundreds of feet, wind-driven and promoted by the coriolis effect
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gyre
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created in the ocean basin, usually 4 currents. 2 boundary currents (north/south along the land). and 2 open-ocean (east/west)
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Sea
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open water. with poor nutrients, except for atlantic which contains sargassum weed
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conter current
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current flows against the surface current. equatorial counter curent(underneath the north-pacific and above the south-pacific) continually flowng but strength is determined by the season which is affected by the atmosphere.
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El nino
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1 every 7-10 years. Results in too much rain in some areas and drought in others. Occurs when the equatorial c.current is so strong that it pushes away the normal surface current and results in an opposite flow that last a year or more.
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Geostrophic flow
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creates a "hill" in the center of the basin because of the coriolis effect taking the surface water with the winds help to the center, but because of gravity and this effect the water rolls down and creates the premanent flow of the currents
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westward intensification
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western boundary currents flow faster(narrow) and deeper (warmer) than the slow,cold, shallow easter currents because of the hill which is off-center and the coriolis effect
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North-pacific gyre
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clockwise from the north pacific current to the california current into the equatorial current and then the western kuroshio current (japan).
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South-pacific gyre
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counter clockwise with the south equatorial current folowing the australian current than the peru current which comes from the west wind drift
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west wind drift
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clockwise aroung the globe around the antartic merges the waters of pacific, atlantic and indian occeans and also creates the peru/humboldt (cold water).
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southern oscillation
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oscillation of the surface pressure. the eastern pacific waters are warm (el nino)sea level pressure drops and rises in the west
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biogeographical distribution
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location of an organism based on both the physical factors of the environment and the biological needs or adaptions of the oraganism where the organism can successfully carry on their life processes.
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south pacific
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islands between hawaii and australia. Islands that are around the equator in north and south. Invertebrates are rich and diverse in this area
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invertebrate
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have no internal skeleton, like sponges, jellyfish, worms, snails, crabs, shrimp, sea urchins and starfish. (95%)
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east pacific barrier
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open water from hawaiin islands to coast of north,central and south america. physical barrier for many organisms to cross
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broadcast spawning
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a strategy of reproduction for invertebrates in producing thousands of eggs and sperm in the the water in hopes of achieving fertilization and surviving in larval stages. no investment of parents
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teleplanic larvae
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if fetilization occurs, the larvae stage is long-term, which aids in dispersal and can be either mero of holoplanktonic.
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Planktotrophic
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very long lived larvae who are predatory depending on the food source from the environment...most likely other larvae. a telplanic larvae
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Lecithtrophic
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a teleplanic larvae that are shorter tem and carry food supply around with them and when yolk is consumed they become adult forms as holoplankton of benthic form.
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stepping stones
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island or groups of islands which are like steps to dispersal for organisms. the closer the islands are the easier for dispersal
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Eddies
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flow of water between, around islands and between currents along coastlines, which prevent organisms from dispersing too far.
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Antitropical(bipolar) distribution
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there is a known pattern in both terrestrial and benthic marine forms of animal and in terrestrial and intertidal/subtidal forms of plant where their presnce is seen in temperate to subpolar latitudes in both the north and south hemisphere, but not in tropical region because its a barrier
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plankton gametic survival strategies
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large numbers released, able to maneuver in strong gloes , mover to areas with lots of individual sense the other eggs by chemicals, produce large eggs
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plankton larval survival strategies
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internal brooding by parents, large number release, move to favorable areas, extend larval life by physical environment (cold water to slow down metabolism), small, increase s.a by appendages and body extensions, large eyes, are transparent and gleatinous
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larvae goals
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find suitable site for settling to adult form, exist in larval stage for as long as possible, survive predation
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phytoplanton
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small microscopic forms of algae that drift of feebly swim in the water column, and can perform photosynthesis. account for 95% of all marine primary productivity
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productivity
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measure the reprodictive capacity of an organism, measure how much organic stuff is produced by an organism, amt of carbon produced as g c/M2/year and measure the rate at which enery is assimilated by an organism
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ionization of the ocean
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fertilize the cold antartic water with iron to enhance the bloom of the phytoplankton. so that their is more plant material to absorb all the CO2 we generate that is killing out planent.
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compensation depth
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depth in the water column where the organism rate of photosyntheis equals the rate of respiration. Above the depth there is trophogenic where there is a net amt of productivity and below is tropholytic hwere the organisms do not produc to give us any net gain.
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Phytoplanton as biological pump
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make organic matter from dissolved CO2, from the atmosphere and when they die and fall to the abyss, the carbon is removed from the atms for many years. they transport carbon to deep ocean.
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Phytoplankton
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form of algae that are unicellular, microscopic, and are able to move bu special appendages (flagella, cilia, oil droplets)
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nanoplankton
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80-90% of all phytoplankton, very small cells, very important base for food chain
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energy pyrmaid
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close to terrestrial,phytoplankton being mose efficient, then herbivores (zooplankton), carnivorees (nekton, fish), then more carnivores (seals), then top carnivores (sharks)
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biomass pyramid
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upside for marine environment because phytoplnkton can produce more for its size. whith higher level nekton, heaviest, than 1st level nekton, then zooplankton and then the lightest phytoplankton.
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biological pump of phytoplankton
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with the sunlight, carbon dioxide and wATER into carbohydrates and proteins-->the food of life.
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antitropic
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there are nutrients leaking out in the warmer areas, so the primary productivity (grams of carbon/meter square/year) is less than the other areas with antartica being the most
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Cyanophyta(monera)
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type of phytoplankton. blue algae,trichodesium which creates the red sea because of a red pigment
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Coccolithophores(plantae)
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are calcium carbonate cocco produce dimethyl sulfate which gives energy.plant kingdom because of photosynthesis,flagellated,
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diatom(plantae)
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create petridish with the outer shell, with cell in center and bottom smaller. have center diatom or pennate (oblong) with asexual reproduction. 3 forms: coscinodiscus (round, centric diatom); rhizosolenia (cylinder); chaetoceros (centric top, weird bottom with hair appendages); asterionella (upside down bell with centric top) and nitzschia (rectangle shape)
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Dinoflagellates (plantae)
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have two flagella and are either naked or armored. create red tide. use chlorophyll to photosynthesize. Ceratium (cyckomorphosis, temp can change shape,seasonally and tri-prong shape) Gonyaulax &Gymnodinium (red tide effect) Noctiluca (naked, predator, can see with naked eye, symbiotic zooxanthellae, live in tissue of other organisms.
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marine snow
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steady fall of organic remains from top of water column to bottom, held tpgether by mucus, carbon-rich nd many zooplankters live their.
mucus that traps sand, dust, particulates from atmosphere. |
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Zooplankton
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feeble swimmers, many bioluminscent, produce mucus, have gelatinous body for buoyancy,
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ubacteria and archbacteria-monera
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eat the oil
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protista-radiolarans
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cyclical base cell with glass like shell
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protista forenmeriferan
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calcium carbonate shell
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