Ecosystems and Tropical Rainforests
Ecosystem Function
- An ecosystem is a community of plants, animals, and their environment.
- Plants are producers, obtaining energy from the sun through photosynthesis to create food (leaves, seeds, fruits).
- Consumers (caterpillars, insects, birds, mice) eat the plants.
- Energy is recycled via nutrient cycling.
Nutrient Cycle
- Dead leaves and branches fall.
- Beetles and earthworms break down the leaves.
- Decomposers (bacteria and fungi) release nutrients into the soil.
- Water dissolves the nutrients.
- Plants absorb water and nutrients through their roots.
- Weathering breaks down rocks, releasing nutrients into the soil.
- Rapid nutrient cycles occur in hot climates due to high temperatures and abundant water, encouraging rotting and bacterial activity.
- Slow nutrient cycles occur in cold climates due to little heat and water, discouraging rotting and bacterial activity.
Tropical Rainforest Biome
- Located between 5 degrees north and 5 degrees south of the equator.
- Examples: Amazon Basin (Brazil), West Africa (Southern Nigeria, Congo, Ghana), Southeast Asia (Indonesia, Thailand, Northeastern Australia).
- Climate is hot due to the sun being directly overhead, concentrating solar rays.
Global Patterns of Ecosystems
- Climate influences natural vegetation and wildlife; large-scale ecosystems match climate zones.
- Large ecosystems are known as biomes (e.g., tropical rainforest, savanna, tundra).
- Latitude affects heat energy: at the Arctic Circle, solar energy strikes at a low angle and is spread over a large area; at 0 degrees latitude, solar energy strikes at almost a right angle, concentrating energy.
Climate of the Tropical Rainforest
- Hot throughout the year with high annual rainfall.
- Average temperature: 27∘C
- Rapid plant growth, trees can reach heights of 40m or more.
- Plant growth is controlled by sunlight, warmth, and water.
Rainforest Water Cycle
- Plant roots take up water.
- Rain is intercepted at the canopy level.
- Water evaporates and forms clouds, leading to convectional rainfall.
Rainforest Nutrient Cycle
- Rapid due to hot, damp conditions on the forest floor, allowing for rapid decomposition of dead plant material.
- Provides plentiful nutrients that are easily absorbed by plant roots.
- Nutrients are quickly absorbed by fast-growing plants and do not remain in the soil for long, staying close to the surface.
Nutrient Cycle in the Rainforest (Detailed Breakdown)
- Soil: Heat and high humidity allow rapid chemical weathering of bedrock, adding nutrients to the soil.
- Biomass: The number of plants and continual growing season results in high nutrient uptake from the soil to the biomass.
- Litter: Some leaves drop during the year; hot, humid conditions allow rapid decomposition, returning lots of nutrients quickly to the soil (leaves can rot in 6 weeks).
- High levels of runoff wash nutrients from the system.
- High precipitation causes leaching of nutrients from the soil.
- High precipitation adds nutrients to the system.
- Plants are always growing, with no dormant season, so a large amount of nutrients are stored in the biomass.