Lecture 6: Organisms: Convergence in fresh water & marine systems Flashcards

1
Q

the four types of freshwater aquatic systems

A
  1. flowing water - streams and rivers
  2. standing water - lakes and ponds
  3. wetlands
  4. estuaries
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2
Q

how do streams form

A

it forms whenever precipitation exceeds transpiration and evaporation

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3
Q

lotic systems

A

-rivers and streams
-very sensitive to changes in water flow

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4
Q

river continuum

A

The continuous combination and growth of streams, to rivers, to the river mouth, and the associated shifts in environments and ecosystems

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5
Q

Riparian zone

A

Distinct terrestrial vegetation that borders lotic systems and experiences seasonal flooding and an elevated water table

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6
Q

streams

A
  • within streams, riffles and pools represent distinct environments, but they are both low productivity
  • food webs are allochthonous
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7
Q

streams - what does it mean that food webs are allochthonous

A

-the organisms in streams depend on organic input at the base of the food web from outside the system to stay balanced
-this can include leaves and dead materials that fall into the stream

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8
Q

rivers

A

-becomes more autochthonous as it gets larger
-has a balanced food web, but silt and turbulent water currents can reduce productivity
-Downstream movement of nutrients and life must be balanced by upstream inputs and allochthonous material.

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9
Q

rivers - what does it mean for the river to be autochthonous

A

nutrients and sunlight support the algal growth from within the river

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10
Q

direct ecological consequences of dams

A

-Disruption to the nutrient flow to lower regions of the river.
-Habitat conversion/destruction of large upstream adjacent area (the reservoir)
-Nutrient buildup on the upstream side of the dam.
-Movement and dispersal disruption for aquatic life, especially fish migration and reproduction.

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11
Q

standing water - lakes and ponds

A

-found in glacier depressions, glacier melts and forms the standing water
-subdivided into 3 / 4 distinct ecological zones

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12
Q

lentic systems

A

-lakes and ponds

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13
Q

standing water - Littoral zone

A

shallow areas, with rooted vegetation

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14
Q

standing water - Limnetic zone

A

-open water with floating algae

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15
Q

standing water - Profundal zone

A

-very deep water with no light
-found only in deep lakes

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16
Q

standing water - Benthic zone

A

sediment with burrowing and microorganisms

17
Q

Thermal zone and circulation in temperate lakes

A

-in most temperate lakes there is thermal stratification
-the surface layer and the deeper layers both have seasonally different temperatures
-a thermocline is present
-most production of biomass occurs in the surface layer where light can pass through for photosynthesis and oxygen levels are high

18
Q

temperate lakes - what is thermal stratification

A

there are distinct temperature zones in the lakes

19
Q

temperate lakes - thermocline

A

-forms between the warming and circulating surface layer and the more static deeper layer
-this region of rapid temperature change further limits mixing

20
Q

spring in temperate lakes

A

winds drive a mixing of layers and distribution of nutrients

21
Q

spring -> summer in temperate lakes

A

-thermocline forms
-high production in surface layer
-nutrients become limited and production declines

22
Q

summer -> autumn in temperate lakes

A

-thermocline disappears with seasonal cooling
-nutrients mixed with by wind turbulence

23
Q

autumn -> winter in temperate lakes

A

winter refuge for organisms in deep water

24
Q

algal bloom and human impacts in temperate lakes

A

-summer water heating and fun-offs can lead to algal blooming
-as the algae keeps blooming, the water becomes more covered and vegetation dies
-the oxygen is then used off
-when those organisms die oxygen is released, but the decomposition process burns the oxygen down
-results in no oxygen left for that system

25
Q

temperate lakes - eutrophication

A

-the algal bloom happens do to humans adding an excess of nutrients into the lakes through runoff
-bc there is an abundance of nutrients, there is no limits on the algae blooming

26
Q

wetlands

A

-they are the direct interaction of aquatic and terrestrial systems
-land that is permanently saturated and supports vegetation adapted to these condition
-plants are adapted to low oxygen concentrations in the saturated soils

27
Q

how are estuaries formed

A

at the mouth of rivers, typically when the river mouth is surrounded by land

28
Q

what are estuaries

A

Aquatic environment with a unique mix of fresh and salt water

29
Q

estuary - nutrients

A

-it is well-supplied with nutrients and sediment from rivers that deliver fresh water
-rapid nutrient exchange between the sediment and shallow water allows for high productivity

30
Q

estuary - high sediment deposition

A

-this creates salt mashes and mangrove wetlands
-salt marshes are exceptionally productive due to nutrient levels
-estuaries always have wetlands surrounding them

31
Q

Distinct zones of marine systems

A
  1. Intertidal zones
  2. Coral reefs
  3. Neritic zone
  4. Oceanic zone
  5. Benthic zone
32
Q

marine systems - Intertidal zone

A

-this biome is found between the low to high tide
-the zonation of organisms is according to air exposure tolerance

33
Q

Marine systems - Coral reefs

A

-this biome found in warm, shallow marine waters
-Structural complexity and productivity of system supports high biodiversity
-this zone is defined by a narrow range of conditions
-sensitive to temperature and pH changes

34
Q

marine systems - Neritic zone

A

-Depths down to the continental shelf
-High productivity from sunlight and tidal nutrient turbulence
-subdivided into the upper photic zone and deeper aphotic zone
-deeper areas are still relatively nutrient rich because of overall productivity of the system

35
Q

marine systems - oceanic zone

A

-Nutrient availability and productivity are low
-subdivided into photic zone and aphotic zone

36
Q

marine systems - Benthic zone

A

Sediment for burrowing and micro organisms