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95 Cards in this Set

  • Front
  • Back
Properties of Water
-Denser than air
-Density Changes with temperature
-Viscosity
-Surface Tension
-High heat of vaporization (evaporates slowly)
-High Heat Capacity (absorbs heat)
-High heat of fusion (change in state --> gas, liquid, etc.)
-Universal solvent (polar)
Viscosity
-increases with a decrease in temperature or an increase in salinity
-relatively low for a iquid
-allows organisms to move through water with paddle like structure (ex. copepods)
Organism Adaptations for High Heat Capacity of Water
-organisms mostly cold blooded
-if warm blooded --> insulated with fur, feathers, or fat
How do marine organisms get oxygen?
they pump it over gills or other respiratory structures
Salinity of Seawater
-35 g salt/1000 g water = 35 practical salinity units
Major Elements of Seawater
-Chloride (55%)
-Sodium (31%)
-Sulfate (8%)
-Magnesium (4%)
-Calcium (1%)
-Potassium (1%)
Minor Elements of Seawater
-Bicarbonate (0.41%)
-Bromide (0.19%)
-Boric Acid (0.07%)
-Strontium (0.04%)
Trace Elements of Seawater
-phosphate
-nitrate
-silicon dioxide
Density of Water
determined by: (in order)
1)temperature
2)salinity
3)pressure
-maximum density for pure water occurs at 4 degrees C
Pressure
-increases 1 atm ever 10 meters down
Plates
-Atlantic Plate
-India-Australian Plate
-South American Plate
-Pacific Plate
-Antarctic Plate
-Eurasian Plate
-Iran Plate
-Nazca Plate
-Cocos Plate
-Philippine Plate
Seas
-Baltic Sea
-Bering Sea
-Mediterranean Sea
-Black Sea
-Caribbean Sea
-China Sea
-North Sea
-Coral Sea
-Red Sea
-Arabian Sea
-Sea of Japan
Oceans
-Constitute 60% of N. Hemisphere & 80% of S. Hemisphere
-Pacific Ocean
-Atlantic Ocean
-Indian Ocean
-Arctic Ocean
Continental Shelf
Shore to Edge of Slope (200m deep)
Continental Slope
3000 meters deep
Continental Rise
4000 meters deep
Abyssal Plain
6000 meters deep
Oceanic Trench
about 10,000 meters deep
Thermal Stratification
1)Epilimnion
2)Thermocline
3)Hypolimnion
-Oxygen Deprivation on bottom when there is uneven mixing
Tropical Conditions
-thermal stratification is continuous
-low primary productivity
Temperate Climate
-overturn most of the year with stratification in summer
Minimum Oxygen
-oxygen decreases from surface to about 500 meters (minimum)
-after 500 meters, oxygen concentration begins increasing again
Currents
-flow clockwise in N. Hemisphere
-flow counterclockwise in S. Hemisphere
Ridge
Shallow areas/rises in ocean where there is high volcanic activity
Subduction Zone
-one plate is being pushed below another
-creates oceanic trenches
Tsunamis
-occur when pressure between plates is released causing massive waves
-also can occur is there is an underwater landslide
-clear sign of a tsunami when water moves away from shoreline
Photic Zone
-Enough light for photosynthesis
-Extends to the depth where the amount of carbon being used equals the amount being synthesized (no net change)
Neritic Zone
-encompasses the water mass that overlies the continental shelf
-goes down to depth of 200 m
Epipelagic Zone
-photic region of the pelagic zone (over open ocean)
-goes down to depth of 200 m
Aphotic Zone
-permanently dark water below the photic zone
-depth below 200 m and beyond
Mesopelagic Zone
-uppermost aphotic zone (700-1000 m)
-Water is about 10 degrees C
Bathylpelagic Zone
-Depth from 1000-4000 m
-Water is about 4 - 10 degrees C
Abyssalpelagic Zone
-Depth from 4000 - 6000 m
Hadalpelagic Zone
-open ocean water of the deep trenches
-depth between 6000 - 12000 m
Plankton
-limited swimming power
-travel at will of currents
-separated from organisms that are strong enough to swim against currents
Phytoplankton
-photosynthetic organisms that generate chemical energy from light
-generally algae & bacteria
Zooplankton
-free floating animals/organisms
-omnivores & carnivores
Bacterioplankton
-autotrophs & heterotrophs
Megaplankton
-above 20 cm
Macroplankton
-between 2-20 cm
-cniderians, snails
Mesoplankton
0.2-2 cm
-arthropods
Microplankton
0.02-0.2 cm
Nanoplankton
20-200 micrometers
Virtually Everything in the Marine system has...
a plankton stage of life
Meroplankton
only plankton for one stage of their life
Holoplankton
always in plankton stage
Diatoms
-dominant phytoplankton in polar and temperate regions
-Coccolithophores
-Have silicon dioxide box over body
Dinoflagellates
-symbiotic with other organisms
-have two flagella
-armored with plates of carbohydrate cellulose
-fairly common
Haptophytes
-found in tropical areas
-have calcium carbonate plates on sides
Prochlorophytes
-in tropical areas
-most numerically abundant
Cyanobacteria
-typically on shorelines
-blue-green algae
Phytoplankton
-Diatoms
-Dinoflagellates
-Prochlorophytes
-Haptophytes
-Cyanobacteria
Zooplankton
-Copepods
-Protista
-Radiolarians
-Ciliophora
-Cnidaria
Copepods
-swim with antennae
-use legs to gather diatoms
Protista
-grazers
Radiolarians
-may have symbiotic algae
-have silicon dioxide shell
Ciliophora
-major grazers of the nanophytoplankton
Cnidarian
-various jellyfish of the classes Hydrozoa & Scyphozoa
-eat fish
Ctenophora
-voracious carnivores
-capture food w/ tentacles
-some use lights to attract prey
Heteropods
-carnivores with transparent jellylike bodies
Pteropods
-carnivores
-shelled pteropods have fragile shells
-swim using winglike foot
Ostracoda
-hard to identify
-studied by few people
-plentiful in fresh & salt water
Chordata
-notochord
-hollow dorsal nerve chord
-gills
Salps
-class of Chordata
-filter feeders
Larvacea
-class of Chordata
-feed on algae
-shed "house" after it is filled up
-filter feeders
Primary Productivity
rate of formation of energy-rich organic compounds from inorganic materials
-phytoplankton are primary producers
Gross Primary Production
total amount of organic energy produced
Net Primary Production
gross primary production - energy needed for plant respiration
Net Primary Production (calculation)
-easiest way to measure this is by using oxygen
1)light/dark bottle method: two bottles, one clear, one dark, measure oxygen content in clear bottle - oxygen content from dark bottle
oxygen gain - oxygen loss = net primary productivity

2) C14 uptake method
-add radioactive C14 to bottle of seawater with phytoplankton
-after incubation period, poured onto filter paper
-measure amount of radioactivity on filter paper (proportional to rate of primary production)
-to correct for possible nonphotosynthetic uptake, same thing is run in a dark bottle

C uptake = (C14 on filter x available inorganic carbon x 1.05)/ total C14 added
What effects primary productivity?
1)Light
-much is reflected off surface (greater the angle = greater reflection)
-light is absorbed as it enters the water (infrared & ultraviolet light absorbed within first few meters)
-light scattered by particles in water

2)Nutrients
-more production where nutrients enter water from soil
Heaviest carbon fixation
-in tropical rainforests (about 31% light)
-oceans about 7% light --> much lower production
Differences in productivity based on season
-North Atlantic --> copepods eat diatoms after bloom
-Pacific --> copepods come to surface in last juvenile stage & eat diatoms --> no bloom
-Tropics dominated by Coccolithophore diatoms all year
Plankton (importance)
-plankton is the base of the food chain & all marine life depends on it
-if it is effected by chemicals, whether, etc., then all life is effected
Reptiles
1) loggerhead turtles
-long migration
-humans cause them great distress --> bubble butt (air in back parts that cause them to float to surface)
-bubble butt caused by stress
-humans also eat them

2) Sea Snakes
-Near Australia
-related to coras

3) Salt Water Crocodiles
-live near shore

4) Salt Water Iguanas
-Live in Galapagos
-Dive into cold water for 15-20mins to hunt
Birds
1)Penguins
-some live in Galapagos
-most familiar with ones in Antarctica
-warm blooded
-fish eaters

2)Albatross
-fish eaters

3)Cormorants
-dive down 100m to catch fish
Nekton
all organisms capable of sustained locomotion against the motion of the water
Holoepipelagic
fish that spend their entire lives in the epipelagic zone
Meroepipelagic
these fish spend only part of their life cycle in epipelagic waters
Buoyancy
1)most fish have gas bladders
2)mammals use lungs & fat deposits for buoyancy (whales have 2-3 feet of blubber)
3)birds use lungs & have hollow bones
-they can also trap air near body using their wings
4)sharks have lots of fat & heterocircle tail
Physostome
-open duct between gas bladder & esophagus
-can fill gas bladder by gulping at surface air or using rete mirabile
Physoclist
-no duct connected to gas bladder
Locomotion
1)Fish --> alternate contractions on opposite sides of body
2)Mammals --> spring forward using back muscles (this creates and up & down movement through the water)

-Flipper or Fins = slow movement
Body Shape
1)Frictional Resistance --> dependent on exposed surface area (a circle = least surface area)
2)Form Resistance --> drag is proportional to the cross sectional area of the object in contact with the water
-least resistance for large volume if ration between the largest diameter & length is about 0.22
3)Induced Drag --> turbulence due to change in speed & direction of flow
4)Laminar Flow --> smooth flow around small animals or large slow animals

-To reduce friction, genitalia are inside internal cavities, hair is gone, & mammary glands are reduced
Defense & Camouflage
1)Cryptic Coloration
-Upper Water --> dominated by blue & green colors
-Ventral Side --> white or silvery to match illumination source
2)Transparent --> some animals are transparent
Sensory Systems
1)Lateral Lines --> Pressure receptors; feel pressure changes around the animal
2)Ampullae of Larenzine -->sensitive to minute electric currents (sharks & rays)
3)Geomagnetic Fields --> long distance navigation (whales & loggerhead turtles)
Echolocation
-similar to sonar
-sounds travel faster in water
-Melon of sperm whale sends out sound waves that bounce off objects and are received by area in lower jaw
Eyes
-eyes on sides of head give wide range
-no binocular vision or great focus
Reproduction
-Holonektonic Fish --> large spawns of eggs, but few survive
-Pelagic Sharks --> have embryos; give live birth
-Birds & Reptiles --> give birth on land
-Whales --> give birth in warm water so offspring don't lose too much heat; offspring gain weight quickly
Special Adaptations for Warm Blooded Animals
-large body size --> reduces surface to volume ratio
-large amounts of blubber
Circulatory Systems
1)Counter-Current System
-core temperature kept high by arteries bringing warm blood to extremities & veins being warmed by running along arteries as they return
-kidneys --> loop of henle is an example a a counter current system
Diving Capabilities
-whales dive deep & hold breath for 80 mins
-seals about 40 mins
-collapse lungs without problems
-don't get bends because they don't breathe
-much larger blood volume --> stores more oxygen
Extreme Exercise
-cuts off blood flow to kidneys, digestive organs, and other organs that are not needed at the time
-same thing happens with diving animals
-they also slow their heart rate
(bottle-nosed dolphin goes from about 90 bpm --> 20 bpm when diving) --> aka bradycardia
Efficient Kidneys
-get rid of excess salt
-birds have salt glands to secrete salt through eyes
Birds have good smell
birds can smell DMS (Dimethyl Sulfide) gas produced by krill (zooplankton)
Review Food Web Chart
Both in the book & Dr. Savitz's sheet