Life in Water Flashcards

1
Q

life began in water

A

stable temp, buoyancy (less structure), viscosity, density (large animals can fly), solvent

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2
Q

what is the limiting resource

A

oxygen

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3
Q

freshwater comes in two kinds:

A

lentic (still) and lotic (moving)

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4
Q

physical factors

A

light, temperature, water movement, salinity, oxygen, pressure

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5
Q

light compensation point

A

depth where rate of oxygen production and use are the same (less light, less photosynthesis in deep)

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6
Q

thermocline

A

a layer of water through which temperature changes dramatically
layers: thermal stratification

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7
Q

water cycling facts

A

driven by solar energy - wind, evaporation, clouds etc.
97% - oceans
2% polar icecaps
1% freshwater

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8
Q

the hydrological cycle

A

reservoirs - lakes, ocean, atmosphere etc.
enterning water: precipitation or sub/surface flow
exits: evaporation, flow
cycle turn over is 9 days in atmosphere and 3100 in oceans

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9
Q

how are currents formed? what do currents do?

A

wind blows

moderate climate, move nutrients, gene flow

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10
Q

gyres

A

circulation systems that under Coriolis move right in NH and left in SH
- cold water from poles to equator
- warm water from equator to poles
this moderates climate

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11
Q

upwelling

A

deep water moved to surface

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12
Q

oceans as an environment

A

largest continuous environment

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13
Q

littoral/intertidal zone

A

shallow shoreline, influenced by tides rising and falling

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14
Q

neurotic zone

A

from coast to shelf (200m)

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15
Q

oceanic zone

A

beyond continental zone

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16
Q

epipelagic (photic) zone

A

surface to 200m

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17
Q

mesopelagic zone

18
Q

bathypelagic zone

19
Q

abyssal zone

20
Q

hadal zone

21
Q

benthic

A

habitants at bottom of aquatic environment

22
Q

pelagic

A

habitants above the bottom

23
Q

thermocline trends

A

permanent and drastic at tropics but weak at poles

24
Q

thermohaline circulation

A

at poles water freezes, leaving salt behind. water gets saltier and denser and sinks, pulling up less salty water = upwelling

  • threatened by freshwater melting (less salty)
  • cycles nutrients
25
salinity
varies with evaporation and precipitation
26
oxygen
highest at surface and bottom
27
comparison of oceans
tropical seas are physically and chemically stable temperature and high lat are more productive highest productivity at coastlines open ocean supports species and is important to O and CO2 budgets
28
fringing reef
shore of island or continent (shallow, photosynthesis, tropics and subtropics)
29
barrier reef
stands between open sea and lagoon (photosynthesis, shallow, tropics and subtropics)
30
atolls
dotting islands
31
kelp forests
photosynthesis, temperature regions
32
levels of intertidal zone | - oxygen
``` supra tidal (splash zone), high intertidal, middle intertidal, low intertidal, subtotal (always covered) - larger amount of oxygen ```
33
spring tides and neap tides
sun and moon pull together (big); sun and moon work opposite (small)
34
salt marshes, mangrove forests and estuaries
transition between freshwater and marine and marine and terrestrial salt marshes have salt plans (evaporated water) mangroves are tropical and subtropical estuaries are dynamic high productivity and many species in wetlands
35
rivers and streams - riparian zone - vertical divisions
O not limiting riparian zone: transition between water and terrestrial vertical divisions: water surface, water column, benthic zone, hypoheic zone (transition to ground water), phreatic zone
36
trees and turbidity on rivers and streams
limit light
37
flood pulse concept
periodic flooding brings nutrients to flood plains and wetlands
38
biochemical oxygen demand
some pollutants require a lot of oxygen to breakdown
39
zones of lakes
littoral (shore) and limnetic (open)
40
oligotrophic lake
well-mined, well oxygenated, low production
41
eutrophic lakes
high production, low oxygen