Abiotic Factors Are Determinants of Terrestrial Biome Distribution
Biome
- Large-scale groupings of ecosystems sharing similar abiotic factors (e.g., temperature, precipitation).
- Despite being geographically distant, biomes of the same type (e.g., deserts) share comparable abiotic conditions.
- Two primary abiotic factors, temperature and rainfall, govern the development of these distinct ecosystems.
1. Temperature: The Energy Factor
- Influence on Metabolism and Growth
- Warm regions (e.g., tropics) foster rapid plant growth and high biodiversity due to abundant energy.
- Cold regions (e.g., tundra) limit plant growth and species diversity because metabolic activities slow in low-temperature environments.
- Impact on Ecosystem Productivity
- Higher temperatures generally boost photosynthesis and nutrient cycling, resulting in lush vegetation.
- Lower temperatures restrict these processes, often yielding more sparse and specialized communities.
Temperature affects not only the survival of plants and animals but also their behavior and reproduction. For example, many species in colder biomes hibernate or migrate to cope with seasonal changes.
2. Rainfall: The Water Factor
- Essential Resource
- Water is vital for all living organisms; varying levels of rainfall create gradients of vegetation density.
- High rainfall supports tropical rainforests, while low rainfall leads to desert conditions.
- Seasonality
- The timing of rainfall influences growing seasons and the life cycles of organisms.
- Regions with unpredictable or seasonal rainfall patterns (e.g., savannas) exhibit adapted species that survive fluctuating water availability.
- Consider the stark differences between deserts and tropical rainforests.
- Deserts, with their high temperatures and very low rainfall, are home to drought-resistant plants like cacti and animals adapted to conserve water.
- On the other hand, tropical rainforests, characterized by high temperatures and abundant rainfall, support dense vegetation and a wide array of animal species.
Visualizing Biome Distribution: Temperature-Rainfall Graph
- Mean Annual Temperature (x-axis) vs. Mean Annual Precipitation (y-axis)
- Each biome occupies a distinct zone on this graph.
- Examples:
- Tropical Rainforests: High temperature, high rainfall.
- Deserts: High temperature, very low rainfall.
- Grasslands: Moderate temperature, moderate rainfall.
- Tundra: Low temperature, low to moderate rainfall.
- Convergent Evolution
- Similar abiotic pressures (e.g., low moisture) cause unrelated species to develop analogous traits.
- Explains why grasslands on different continents share ecosystem structures despite distinct species.
Key patterns on the graph
- Tropical Rainforests: Found in regions with high temperatures and high rainfall, these areas support dense vegetation and high biodiversity.
- Deserts: Located in areas with high temperatures and very low rainfall, deserts feature sparse vegetation and highly specialized organisms.
- Grasslands: Found in regions with moderate temperatures and medium rainfall, grasslands support grasses and herbivores but lack sufficient water for dense forests.
- Tundra: Found in regions with very low temperatures and low to moderate rainfall, tundras are characterized by limited vegetation, such as mosses and small shrubs.
- The boundaries between biomes on the temperature-rainfall graph are not fixed.
- They can shift due to changes in climate, human activity, or natural events.


