topic 2 Flashcards

1
Q

definition; example

fundamental niche vs realised niche

A

definition:
-fundamental is the entire set of conditions a popoulation can SURVIVE and REPRODUE

-realised is set of conditions ACTUALLY used to SURVIVE and REPRODUCE due to biotic conditions

example:
in a forest, sparrows feed on berries growing on bushes
-fundamental: anywhere there is berries, including entire bush and forest floor; anywhere there is the resource

-realised niche: there is resources competition on the forest floor, so sparrows’ niche is only area on bushes

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2
Q

Predation example

A

Dingo, sheep

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3
Q

Herbivory example

A

Elephants grazing on shrubs

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4
Q

Parasitism example

A

Ticks on moose

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5
Q

Mutualism example

A

Bees pollinating flowering plants

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6
Q

Commensalism example

A

Barnacles on humpback whales

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7
Q

Named example of a food chain involving producers, consumers, decomposers

A

Grassland ecosystem foodchain: grass –> grasshopper –> rat –> snake –> fungi

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8
Q

2 examples

examples of bioaccumulation

A

-mercury building up in fish
-pesticides building up in small animals

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9
Q

2 examples

examples of biomagnification

A

-high concentration of heavy metals in apex predator fish such as tuna as a result of acccumulation along the food chain being magnified

-high concentration of DDTs in apex predator birds such as the bald eagle as a result of consuming prey (small fish) with DDTs

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10
Q

detailed example of how humans impact energy flows

A

deforestation
* trees play a role in the energy cycle, absorbing and converting sunlight
* when large areas deforested, energy that would have been absorbed/converted is instead REFLECTED, contributing to global warming

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11
Q

(4 points)

detailed example of impact of urbanisation on matter cycle (carbon)

A

-increases need for energy and thus increases use of fossil fuels, leading to increased combustion –> creates more matter (carbon) which cannot be adequately integrated into carbon cycle, leading to climate change

-decreased land covered by vegetation, reducing photosynthesis –> less matter can be cycled through vegetation for absorption and conversion, tldr global warming

-increases food requirements, leading to increased land use for agriculture

-increased requirement and transport of food leads to greater energy requirements and increased fossil fuel use –> creates more matter etc same as above

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12
Q

what human activities impact energy flows and matter cycling

A

-through large scale activities:
* deforestation
* pollution
* urbanisation
* overexplotation of resources

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13
Q

outline structure for how humans impact energy flows

A

-role thing plays in energy flow/system
-what would happen to the energy –>
-how [human activity] changes what happens to the energy
-impact

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14
Q

detailed example of agriculture’s impact on matter cycle (nitrogen)

A

-industrial agricultural techiniques of NITROGEN FIXATION –> significantly INCREASED the amount of GLOBAL NITROGEN FIXATION –> INCREASED amounts of useable nitrogen in fertilisers

-application of nitrate fertiliser to increase crop yield and save money in agriculture –> biologically available nitrogen in ecosystem INCREASES, runs off or leaches into bodies of water –> causes EUTROPHICATION and DISRUPTION to ecosystem –> eutrophophication leads to LOW OXYGEN LEVELS, changing food-web structure and resulting in habitat degradation

-nitrogen in crop biomass is transferred across locations –> this removes the matter from the cycle in one location and adds it to another –> this alters the nitrogen cycle and can cause DISRUPTION to ecosystems

-agricultural soils become waterlogged as a result of irrigation –> denitrifying bacteria INCREASES –> rate of nitrogen gas returning to the atmosphere INCREASES

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15
Q

4 main activities that impact carbon cycle matter cycling

A

-urbanisation
-deforestation
-agriculture
-fossil fuel use

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16
Q

outline structure for how humans impact matter cycling

A

human behaviour
impact
how that CHANGES CYCLING OF MATTER

17
Q

4 points

detailed example of impact of deforestation on matter cycle (carbon)

A

-trees are removed, leading to carbon storage reduction –> matter is then released back into the atmosphere en masse

-deforestation worsens soil erosion –> flow of carbon stored in soil into the rivers, which Doesn’t Happen Like That Usually

-deforestation reduces amount of photosynthesis occurring –> matter cycle is impacted as less matter can cycle from atmosphere into trees

-deforesttion increaes respiration from decomposers feeding on decaying forest residue –> increases the amount of matter being transferred from decomposers into atmosphere

18
Q

2 points

detailed example of impact of agriculture on matter cycle (carbon)

A

-land use is increased for agriculture and decreased for native ecosystems –> nature of carbon storage is altered

-agriculture results in the transportation of crops (a carbon storage) into new locations –> location of matter flow changes, altering carbon cycle on LOCAL and GLOBAL scale

19
Q

Detailed example of impact of fossil fuel use on matter cycling (carbon)

A

-involves the direct burning of a carbon store locked up for millions of years in carbon deposits

-MINING and BURNING fossil fuels reduces the available storages of non-renewable resoruces, and INCREASING storage carbon in atmosphere

-increased release of greenhouse gases (.e.g, co2) and thus warmer average gobal temperature

-INCREASED co2 levels in the atmosphere can LEAD to INCREASED VEGETATION GROWTH due to increased co2 available for photosyntheis, ALTERING THE CARBON CYCLING

20
Q

1

detailed example of impact of deforestation on matter cycling (nitrogen)

A

-trees are destroyed, leading to the loss of the nitrogen STORED in them as amino acids and protein

21
Q

Zonation case study

A

-Mount Kinabalu, Borneo
-showcases ALTITUDINAL ZONATION in the plant communities
-zonation is caused by TEMPERATURE changes
-ranges from TROPICAL RAINFOREST at LOW LEVELS (26 degrees celcius) to ALPINE COMMUNITIES near the SUMMIT (0 degrees celcius)

22
Q

what is needed to be known for zonation case study?

A

-location
-what kind of zonation
-what the zonation is caused by
-what this looks like along the gradient (looks like THIS at THIS FACTOR and THIS at THIS FACTOR)

23
Q

Primary succession example and general progression

A

-retreat of GLACIERS in ALASKA has caused PRIMARY SUCCESSION because ground is made bare

-EARLY PIONEER PLANTS such as mosses and lichens COLONISE the bare rock and create SOIL when they die

Arrival of PIONEER SPECIES that require soil to survive DISPLACING original pioneer species

PIONEER SPECEIES plant growth causes environmental change, and root growth enables soil to be RETAINED; NUTRIENTS and WATER in soil INCREASE

INTERMEDIATE NITROGEN-FIXING species arrive, adding nitrates to soil, increasing SOIL DEPTH and allowing SHRUBS AND TALLER PLANTS to arrive

seral stage: taller trees begin to replace others and initially grow quicker than the deciduous taking root; however the deciduous trees grow TALLER than the other sand SHADE THEM OUT

the CLIMAX COMMUNITY of decidious trees totally replace others after 100-200 years

24
Q

Secondary succession case study example

A

-regeneration of Australian bushland disturbed by fire, leaving empty but NOT destroyed soil

-PIONEER SPECIES grow back

-INTERMEDIATE SPECIES then LARGER TREES grow back

-CLIMAX COMMUNITY of large deciduous trees that outshade the later intermediate species dominate the ecosystem

25
Q

Compare and contrast 2 (named) r- and K-strategists

A

r-strategists (e.g., salmon) mature early, have a large number of offspring, and thrive in unstable environements
K-stragegist (.e.g, whales) have a late maturity, have few offspring, and thrive in stable environments

26
Q

Explain the distributions, climate, structure, biodiversity, and relative productivity of a pair of contasting biomes (#1)

desert and tundra

A

DESERT
distribution: in bands, lat=15-30 degrees north and south of equator
climate:
* low rainfall (under 250mm annually)
* high sunlight
* very hot in daytime and cold in night

structure:
* scarce vegetation, tall trees absent
* many XEROPHYTIC plants, e.g., cacti
* soil ERODES easily in wind, and has low water-holding capacity and fertility
* animals are adapted to desert conditions

relative productivity:
* very low

TUNDRA
distribution:
* high latitudes
* adjacent to ice margins

climate:
* low temps
* low precipitation
* seasonal sunlight
* short day length

structure:
* simple structure
* vegetation is low scrub and grasses, forms a single a layer
* tall trees absent
* producitivity LIMITED by frozen permafrost and soil

relative producitivty:
* low

where it is; how affects temperature; whatbiome Looks Like; productivity

27
Q

List five abiotic factors

A

-windspeed (TERRESTRIAL )
-temperature
-light
-wave action (MARINE)
-flow velocity (FRESHWATER)

28
Q

Windspeed (3 points)

A

-biome: terrestrial

-measurement tool: anemometer

-evaluative measure: gusty conditions can lead to large variations in data

29
Q

Temperature (3 points)

A

ecosystem type: terrestrial, freshwater, AND marine

measurement technique: thermometer

-evaluative measure: problems in data if temperatuer not taken from consistent depth

30
Q

Light (3 points)

A

ecosystem type: terrestrial, freshwater, AND marine

measurement technique: Lightmeter

evaluative measure: Cloud cover changes light intensity

31
Q

Wave action (3 points)

A

ecosystem type: marine

measurement technique: dynamometer

evaluative measure: changes in wave strength during a day and over a monthly period affect results

32
Q

flow velocity (3 points)

A

ecosystem type: freshwater

measurement technique: flowmeter

evaluative measure: readings must be taken from same depth; water flow can vary due to rainfall/ice melt