2.4 Biomes, zonation and succession Flashcards
Biome
collections of ecosystems that share distinctive abiotic factors, species and climatic conditions
Types of biome
Terrestrial (forest, desert, grassland, tundra), marine and freshwater (aquatic)
Tricellular model of atmospheric circulation
explains differences in temp + precipitation and how they influence the structure and productivity of different biomes.
Latitude and atmospheric circulation
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
Formations
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)
Tropical rainforests
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
Temperate forest
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
Deserts
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
Tundra
→ 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
Effects of climate change on biome distribution
→ increases in CO2 and other GHG increases mean global temperature, affecting rainfall patterns
→ climate change alters biome distribution
Spatial and temporal changes in communities
→ 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
Zonation
→ the arrangement or pattern of communities in bands in response to a change in environmental factors over distance (eg. altitude, latitude, distance from shore)
Rock shores
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
Succession
→ 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)
Pioneers
first stage of ecological succession - species able to withstand difficult conditions