2.4 Biomes, zonation and succession Flashcards

1
Q

Biome

A

collections of ecosystems that share distinctive abiotic factors, species and climatic conditions

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2
Q

Types of biome

A

Terrestrial (forest, desert, grassland, tundra), marine and freshwater (aquatic)

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3
Q

Tricellular model of atmospheric circulation

A

explains differences in temp + precipitation and how they influence the structure and productivity of different biomes.

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4
Q

Latitude and atmospheric circulation

A

are the primary factors affecting insolation, temp, and precip.
→ the higher the latitude, the colder the temperatures
→ areas around equator receive the most insolation / unit area of earth
→ polar areas have more atmosphere to pass through, = more loss of energy and cooler temps

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5
Q

Formations

A

Hot air heated at equator, rises to form Hadley cell.
→ as air rises, it cools and condenses, forming tropical storms (explains tropical rainforest at equator)

→ cooled air spreads and descends - descending creates high pressure and dry areas at 30° (explains desert biome)

→ air travels towards pole as warm winds, when met with cooler polar air at 60° it rises, condenses and forms precipitation (explains temperate forest biome)

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6
Q

Tropical rainforests

A

distribution: band around equator, within tropics of cancer and capricorn
→ temperature: high and consistent yearly (~26°C)
→ precipitation: high
→ insolation: high, little to no seasonal variation. Provides year round growing season.
→ productivity: comprises ~ 40% of NPP for terrestrial ecosystems. High photosynthesis and NPP caused by low latitude and ample direct sunlight.
→ biodiversity: high, up to estimated half of world’s species in rainforest canopy. High diversity due to high climate factors year round.
→ structure: stratified tree canopy, many niches. Only ~1% of light on canopy reaches forest floor, canopy has highest NPP.
→ soil low in nutrients, majority stored in trees. High rates of decay maintain rates of growth.
→ heavy rains can result in nutrients being washed away, which limits PP.
→ canopy usually protects soils from rainfall, but logging causes soils to be eroded rapidly

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7
Q

Temperate forest

A

distribution: between 40° - 60°N of equator
→ temperature: cold winters, warm summers
→ precipitation:determines whether temperate forests or grasslands develop
→ insolation: varies according to tilt of Earth, limits growing season
→ productivity: lower compared to rainforests due to power temps and rainfall. Second highest NPP in all biomes.
→ biodiversity: lower than rainforests, forests usually dominated by one species
→ structure: less stratification and layering, less dense canopy, reduces species diversity and complexity of niches
→ two types of trees (evergreen, deciduous - deciduous lose their leaves in winter)
→ forest floor leaf layer increases insulation and nutrients when it decays in warm temperatures

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8
Q

Deserts

A

distribution: 30° N and S
→ temperature: high during day (45-49°C), low at night (10-0°C)
→ precipitation: low - often very uneven
→ insolation: high (air is dry after leaving tropics)
→ productivity: lack of water limits photosynthesis and NPP, results in sparse vegetation
→ biodiversity: xerophytic species (adapted to fluctuations in temp and scarcity of water), reptiles most common vertebrates due to cold-blooded metabolism, cacti reduce surface area for transpiration via spines
→ structure: soil can be rich in nutrients as there is no leaching, decomposition is low due to lack of water

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9
Q

Tundra

A

→ distribution: high altitudes, the north polar region
→ temperature: low for majority of year, -50°C, warmer during 6 week period.
→ precipitation: low, water mainly stored in ice
→ insolation: short days, limited sunlight; almost 24h of sunlight during summer. Life increases during summer.
→ productivity: very low due to variable light intensity, rainfall and temperatures affecting race of photosynthesis
→ biodiversity: low, very few species adapted to cold conditions - large animals to reduce heat loss
→ structure: low temperatures lead to low cycling of minerals → peat bogs form in carbon sinks

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10
Q

Effects of climate change on biome distribution

A

→ increases in CO2 and other GHG increases mean global temperature, affecting rainfall patterns
→ climate change alters biome distribution

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11
Q

Spatial and temporal changes in communities

A

→ spatial changes occur along environmental gradients due to changes in altitude, latitude, distance from sea
→ temporal changes occur as a community develops from early to later stages

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12
Q

Zonation

A

→ the arrangement or pattern of communities in bands in response to a change in environmental factors over distance (eg. altitude, latitude, distance from shore)

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13
Q

Rock shores

A

organisms high on shore exposed to air for long periods of time, have adapted to withstand changes in salt concentration and temperature
→ organisms low on shore are covered by seawater, experience less variation in temperature and salt concentration, with greater wave stress

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14
Q

Succession

A

→ change over time in an ecosystem involving pioneer / intermediate / climax communities
→ each distinct community in the succession is a seral stage
→ succession explains how ecosystems develop from a bare substrate over time
→ lithosere (bare rock)
→ fresh water (hydrosere)
→ dry habitat (xerosere)

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15
Q

Pioneers

A

first stage of ecological succession - species able to withstand difficult conditions

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16
Q

Climax community

A

final stage of succession, more stable than earlier stages, in equilibrium

17
Q

Primary succession

A

occurs on previously uncolonised substrate (eg. rock)

18
Q

Secondary succession

A

occurs in places where a previous community has been destroyed. Faster than primary succession due to soil and seed bank.

19
Q

Primary succession on shingle ridge

A

→ lichens and mosses pioneer species that photosynthesise and trap water on nutrient-poor shingle
→ pioneer species trap particles blowing by and weather the rock
→ decomposition of pioneers results in a thin layer of soil
→ red fescue colonise area, roots trap soil and prevent erosion, pioneers begin to be outcompeted
→ xerophytic plants eg. sea kale prevent water loss, nitrogen-fixing plants eg. rest harrow increase soil nutrients
→ decomposition continues and allows growth of larger plants eg. shrub community of bramble
→ climax community of temperate forest (oak/sycamore) develops, shrubs are replaced by shade-adapted species like ferns

20
Q

Secondary succession in yellowstone

A

Fires in Yellowstone National Park wiped out many aspects of the park’s forest - some fires burned soil and ground biomass, some burned the canopy. Fires burned for several months.
→ recovery began almost immediately with herbaceous fireweed as a pioneer species
→ lodgepole pines, though a climax species, are serotinous, allowing fast regeneration in burned areas
→ comprising 80% of park’s forests, they only release seeds when high temperatures eg. fires create favourable open canopies for seedling establishment
→ aspen, wildflowers had an increase in productivity as nutrients were released from forest litter during burning
→ soil depth only charred to 14mm, leaving diverse root systems unharmed
→ minimal overall loss of wildlife from fires, only browsers eg. moose populations declining
→ other k-strategists eg. elk, bison, deer rebounded due to rapid plant growth, birds able to find ants and worms easily in newly uncovered soil

21
Q

changes through succession

A

GPP → pioneer communities have low GPP because of the low density in producers. Climax communities have high GPP as there is an increased consumer community.
NPP → high in pioneer communities as community respiration is low (low # organisms). High NPP means biomass is continuing to accumulate. Approaches zero in climax community as GPP is balanced by increased respiration

22
Q

Climax communities

A

community of organisms that is in steady-state equilibrium with natural environmental conditions. It is the endpoint of ecological succession.
→ greater biomass, high species, habitat and genetic diversity
→ favourable soil conditions and structure (deeper, greater water retention/aeration)
→ more k-strategist organisms (taller plants etc)
→ greater community complexity, resilience and stability

23
Q

R strategists

A

Colonisers
Highly adaptable
Rapid growth/development
Short lifespans
Small size, many offspring
Early, high reproduction
Type III survivorship
Suited to pioneer communities
Continuous J-curve population

24
Q

K strategist

A

Dominant species
Specialist, susceptible to change
Slow growth/development
Long lifespans
Large size, few offspring
Delayed reproduction
Type I or II survivorship
Suited to climax communities
S-population curve

25
Q

Human impact on succession

A

Human disturbance halts process of succession and divert it so a different stable state other than a climax community is reached.
→ activity modifies the ecosystem (eg. use of fire, grazing, agriculture, deforestation, overfishing); depending on the resilience of an ecosystem changes may be more or less permanent.
Eg. deforestation of tropical rainforest biome
→ increased demand for meat demands land for cattle ranching and agriculture, 90% of the reason why land is deforested in the Amazon. Results in habitat destruction and loss of climax community.
→ replacement with agricultural system affects global biodiversity, weather, sedimentation patterns
→ CO2 released returns to atmosphere