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

A

200-1000

18
Q

bathypelagic zone

A

1000-4000

19
Q

abyssal zone

A

4000-6000

20
Q

hadal zone

A

deepest

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
Q

salinity

A

varies with evaporation and precipitation

26
Q

oxygen

A

highest at surface and bottom

27
Q

comparison of oceans

A

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
Q

fringing reef

A

shore of island or continent (shallow, photosynthesis, tropics and subtropics)

29
Q

barrier reef

A

stands between open sea and lagoon (photosynthesis, shallow, tropics and subtropics)

30
Q

atolls

A

dotting islands

31
Q

kelp forests

A

photosynthesis, temperature regions

32
Q

levels of intertidal zone

- oxygen

A
supra tidal (splash zone), high intertidal, middle intertidal, low intertidal, subtotal (always covered)
- larger amount of oxygen
33
Q

spring tides and neap tides

A

sun and moon pull together (big); sun and moon work opposite (small)

34
Q

salt marshes, mangrove forests and estuaries

A

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
Q

rivers and streams

  • riparian zone
  • vertical divisions
A

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
Q

trees and turbidity on rivers and streams

A

limit light

37
Q

flood pulse concept

A

periodic flooding brings nutrients to flood plains and wetlands

38
Q

biochemical oxygen demand

A

some pollutants require a lot of oxygen to breakdown

39
Q

zones of lakes

A

littoral (shore) and limnetic (open)

40
Q

oligotrophic lake

A

well-mined, well oxygenated, low production

41
Q

eutrophic lakes

A

high production, low oxygen