Ch2 Flashcards

1
Q

Turnover

A

time for water reservoir to renew

  • atmosphere 9days
  • river 12-20 days
  • lake - days-centuries
  • oceans 3100 years
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2
Q

Life in water

A

Density higher = structure for soft bodied organisms

Buoyancy higher = organisms use lipids/air sacs to stay under pressure

Viscosity higher = more energy to move

Light lower = photosynthesis restricted

Heat conduction higher = difficult to maintain body temp above surrounding temp

Specific heat higher = more stable

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3
Q

Littoral zone

A

Littoral zone = intertidal shallow zone

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4
Q

Ocean Zone

A
  • epipelagic = 0:200m
  • mesophelagic = 200-1000m
  • bathypelagic = 1000-4000m
  • abyssal = 4000-6000m
  • hadal = 6000m (O2 levels higher, fewer organisms)
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5
Q

Benthic

A

Habitat on bottom of ocean

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6
Q

Pelagic

A

Habitat off bottom of ocean

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7
Q

Ocean Light

A

80% absorbed in first 10m

  • very little penetrates past 600m
  • leaves 3400m deep = black water
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8
Q

Neritic zone

A

Neritic zone = coast margin of continental shelf (200m deep)

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9
Q

Ocean Temp

A

increases velocity of molecules so density decreases with warm water on top and cool water below

  • thermocline: rapid temperature change with depth causing thermal stratification
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10
Q

Ocean water movement

A
  • always mpving
  • deep water current make upwellings
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11
Q

Ocean Salinity

A

Decreases close to the equator due to precipitation>Evaporation

  • increases in subtropics
  • uniform proportions of major ions (Ca2+, Mg2+)
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12
Q

Ocean oxygen

A

increase near surface, decrease to 1000m

increase past 1000m (sometime)

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13
Q

Ocean Biology

A

Photosynthetic organisms are epipelagic (on top layer)
i. photoplankton/zooplankton
ii. 1/4 of total photosynthesis globally

When no light present organisms will chemosynthesize

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14
Q

Human influences on oceans

A
  • overharvesting
  • dumping
  • plastic
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15
Q

Coral reefs

A

in shallow marine waters
- fringing reef = corals growing around young islands from a fringing reef

  • barrier reef = as island subsides. corals continue to grow upward and outward towards the sea forming a barrier
  • atoll = as island subsides, coral growth will from an atoll on top of island when it has subdivided completely below sea level
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16
Q

Reefs and kelp beds

A
  • sufficient light
  • limited by temp
  • currents bring o2 and nutrients and remove waste = flushing
17
Q

Waves and ties of marine shores/intertidal

A

waves and tides most important

  • semidiurnal = 2 high tides and 2 low tides
  • diurnal = 1 high tide and 1 low tide
18
Q

Marine shores/Intertidal

A
  • where amphibious life adapted
  • tolerance to air exposure causes zonation
  • accessibility increasing = exploitation inceases
19
Q

Estuaries

A

river to sea

20
Q

salt marshes/mangroves

A

low costs

salt marsh located in northern regions

mangroves located in tropical/subtropical southern regions

21
Q

Estuaries/salt marshes/mangroves characteristics

A
  • tides and river
  • organisms, nutrients, O2
  • remove waste
  • vulnerable
22
Q

Salt marshes and mangroves fluctuations

A

fluctuations strong and complex for:
- light, temp, O2
- salinity gradient (fresh water will sit on top of salt water until it mixes)
- tides
- primary production

23
Q

Endemic species

A

native and only found in one particular area

24
Q

River and stream - light, water movement, temp

A

Light
- surface
- water column
Water movement
- cause erosion and suspended sediments
Temperature
- similar to water temp

25
Q

River and stream - salinity and O2

A

Salinity
- leaching in the basin
Oxygen
- inversely correlated with temp
- not limiting

26
Q

Lentic waters

A

= lakes/water that doesn’t move

Surface water:
- great lakes = 20%
- lake baikal = 20%
- rift lakes of Africa = 20%

27
Q

Lake structure

A
  • Littoral zone
  • Limnetic zone
  • Epilimnion: warm surface layer
  • Metalimnion zone: temp changes with depth; prevents nutrient exchange with hypolimnion
  • Hypolimnion: cold dark waters
28
Q

Lakes - light, temp water movement

A

Light
- colour: light absorbtion and biological activity

Temp
- thermal stratification w/ warming
- seasonal temp changes

Summer = stratification seperated by metalimnion

Fall = overturn (circulation of water temps)

Winter = ice on top, 4C on bottom with little circulation

Spring = overturn

Water movement
- caused by wind

29
Q

Lakes - salinity and O2

A

Salinity
- more variable than ocean, mean = 0.120ppt-200ppt

Oxygen
- Oligotrophic: production decreases and oxygen increases (poor in food)
- eutrophic: production increases, and oxygen decreases (lots of food)

30
Q

Wetlands

A

Land that is saturated with water

  • to promote wetland/aquatic processes there must be poorly drained soil
  • hydrophytic vegetation (can cause various biological activity)
  1. Bogs
  2. Fen
  3. Swamp
  4. Marsh
  5. Shallow water wetland
31
Q

Bogs/fens

A

40cm water + peat
- located mainly in northern hemisphere
- no salinity
- anerobic and acidity inhibit decomp
bogs = precipitation only, very acidic (<4.5)
fens = precipitation and GW/SW, alkaline but variable (4.5-9.0)

32
Q

Peatland

A
  • no salinity
  • pH