• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/55

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

55 Cards in this Set

  • Front
  • Back
North Pacific gyre
clockwise with california current (eastern boundary current), to north equatorial current, into the western boundary current of kuroshio and then the north pacific current.
South Pacific gyre
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.)
West wind drift
encircles the globe, which merges the atlantic, pacific and indian oceans.
south pacific
islands between hawaii and australia. This is the riches and most diverse area for marine forms
east pacific barrier
open water from hawaiin islands to the coast of north,central and south america. Difficult physical barrier for many organisms
North Pacific gyre
clockwise with california current (eastern boundary current), to north equatorial current, into the western boundary current of kuroshio and then the north pacific current.
South Pacific gyre
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.)
West wind drift
encircles the globe, which merges the atlantic, pacific and indian oceans.
south pacific
islands between hawaii and australia. This is the riches and most diverse area for marine forms
east pacific barrier
open water from hawaiin islands to the coast of north,central and south america. Difficult physical barrier for many organisms
Current
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
gyre
created in the ocean basin, usually 4 currents. 2 boundary currents (north/south along the land). and 2 open-ocean (east/west)
Sea
open water. with poor nutrients, except for atlantic which contains sargassum weed
conter current
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.
El nino
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.
Geostrophic flow
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
westward intensification
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
North-pacific gyre
clockwise from the north pacific current to the california current into the equatorial current and then the western kuroshio current (japan).
South-pacific gyre
counter clockwise with the south equatorial current folowing the australian current than the peru current which comes from the west wind drift
west wind drift
clockwise aroung the globe around the antartic merges the waters of pacific, atlantic and indian occeans and also creates the peru/humboldt (cold water).
southern oscillation
oscillation of the surface pressure. the eastern pacific waters are warm (el nino)sea level pressure drops and rises in the west
biogeographical distribution
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.
south pacific
islands between hawaii and australia. Islands that are around the equator in north and south. Invertebrates are rich and diverse in this area
invertebrate
have no internal skeleton, like sponges, jellyfish, worms, snails, crabs, shrimp, sea urchins and starfish. (95%)
east pacific barrier
open water from hawaiin islands to coast of north,central and south america. physical barrier for many organisms to cross
broadcast spawning
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
teleplanic larvae
if fetilization occurs, the larvae stage is long-term, which aids in dispersal and can be either mero of holoplanktonic.
Planktotrophic
very long lived larvae who are predatory depending on the food source from the environment...most likely other larvae. a telplanic larvae
Lecithtrophic
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.
stepping stones
island or groups of islands which are like steps to dispersal for organisms. the closer the islands are the easier for dispersal
Eddies
flow of water between, around islands and between currents along coastlines, which prevent organisms from dispersing too far.
Antitropical(bipolar) distribution
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
plankton gametic survival strategies
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
plankton larval survival strategies
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
larvae goals
find suitable site for settling to adult form, exist in larval stage for as long as possible, survive predation
phytoplanton
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
productivity
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
ionization of the ocean
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.
compensation depth
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.
Phytoplanton as biological pump
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.
Phytoplankton
form of algae that are unicellular, microscopic, and are able to move bu special appendages (flagella, cilia, oil droplets)
nanoplankton
80-90% of all phytoplankton, very small cells, very important base for food chain
energy pyrmaid
close to terrestrial,phytoplankton being mose efficient, then herbivores (zooplankton), carnivorees (nekton, fish), then more carnivores (seals), then top carnivores (sharks)
biomass pyramid
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.
biological pump of phytoplankton
with the sunlight, carbon dioxide and wATER into carbohydrates and proteins-->the food of life.
antitropic
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
Cyanophyta(monera)
type of phytoplankton. blue algae,trichodesium which creates the red sea because of a red pigment
Coccolithophores(plantae)
are calcium carbonate cocco produce dimethyl sulfate which gives energy.plant kingdom because of photosynthesis,flagellated,
diatom(plantae)
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)
Dinoflagellates (plantae)
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.
marine snow
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.
Zooplankton
feeble swimmers, many bioluminscent, produce mucus, have gelatinous body for buoyancy,
ubacteria and archbacteria-monera
eat the oil
protista-radiolarans
cyclical base cell with glass like shell
protista forenmeriferan
calcium carbonate shell