Topic 1.2: Terrestrial Biomes Flashcards
Definition and Core Characteristics of Biomes
- Biomes are geographical areas characterized by a shared combination of average yearly temperature and precipitation patterns, which together define a region's climate.
- Climate refers specifically to the long-term trends and averages of annual temperature and precipitation in a given area.
- Temperature and precipitation ranges serve as the two primary defining characteristics of any biome:
- Tropical Rainforest: Defined by consistently warm temperatures and extremely high annual rainfall.
- Desert: Defined primarily by very low annual precipitation. Although deserts often experience high temperatures, the defining factor distinguishing them from tropical rainforests is the scarce rainfall.
- Tropical Seasonal Forest (Savannah): Annual precipitation ranges from approximately 60cm or 75cm up to 280cm, with average annual temperatures ranging from 18∘C to 29∘C.
Adaptations of Organisms to Biome Climates
- Plant and animal communities residing within a biome possess specialized biological adaptations essential for surviving its specific climatic conditions.
- Desert Adaptations:
- Camels: Store energy in the form of fat inside their humps, allowing them to endure extended periods without access to external food and energy sources.
- Cacti: Possess thick, waxy cuticles (outer coatings) that minimize water loss caused by evaporation in high-heat, low-moisture environments.
- Grassland Adaptations:
- Shrubs and Wildflowers: Develop long, deep root systems capable of storing substantial energy reserves underground. When periodic wildfires devastate the above-ground vegetation, these deep root energy stores allow the plants to rapidly regrow.
Geographic Distribution and Latitudinal Patterns of Biomes
- The worldwide spatial distribution of biomes follows predictable geographic patterns determined largely by latitude and distance from the Equator, which dictate light intensity and temperature:
- Cold and Dry Biomes (Tundra and Boreal Forest):
- Located far from the Equator, concentrated around 60∘ latitude and further north.
- Characterized by low annual precipitation and low average temperatures.
- Temperate Biomes (Temperate Grassland and Temperate Seasonal Forest):
- Concentrated in the middle latitudes between 30∘ and 60∘ latitude.
- Experience moderate annual rainfall and moderate temperatures year-round, featuring warm summers and cool winter seasons.
- Tropical Biomes (Tropical Rainforest and Tropical Seasonal Forest / Savannah):
- Concentrated around the Equator (0∘ latitude).
- Characterized by direct solar radiation year-round, resulting in consistently warm temperatures and high annual precipitation.
Nutrient Availability Across Biomes
- Soil nutrient availability is a crucial biome characteristic that dictates which plant species—and how many species—can survive in an ecosystem.
- Tundra:
- The soil remains permanently frozen year-round as permafrost, except for a thin surface layer known as the active layer that thaws annually to support plant growth.
- Permanently frozen soil severely restricts the decomposition of organic matter by decomposers, preventing the recycling of essential soil nutrients.
- Frozen conditions result in low soil nutrient levels and low liquid water availability, limiting survival to very few plant species, which subsequently limits animal diversity.
- Tropical Rainforest:
- Possesses surprisingly nutrient-poor soil despite high plant density and high biomass production.
- Rapid nutrient uptake occurs because dense plant populations compete intensely for resources, immediately absorbing soil nutrients as soon as organic matter decomposes.
- Boreal Forest (Taiga):
- Characterized by cold temperatures and dominated by coniferous trees such as pine, spruce, and aspen.
- Features nutrient-poor soils because low temperatures throughout much of the year restrict the activity of decomposers (such as earthworms and fungi), slowing the decomposition of dead organic matter and nutrient cycling.
- Temperate Seasonal Forest:
- Found extensively in areas such as West Michigan and across much of the United States.
- Features high soil nutrient levels due to the abundance of broadleaf deciduous trees (such as oaks and maples) that shed their leaves every autumn.
- Accumulation of leaf litter on the forest floor, combined with moderate temperatures, promotes rapid decomposition and continuous nutrient replenishment in the soil.
Climate Change and Shifts in Biome Distribution
- Biome boundaries are dynamic and shift geographically in response to global climate changes driven by human activities.
- Mechanisms of Biome Shifts:
- Rising global temperatures cause previously frozen northern soils to thaw, expanding the suitable growing habitat for large tree species further north.
- Warm temperatures cause biomes to lose their southern geographic ranges, as southern regions become too warm for cold-adapted native tree species.
- Boreal Forest and Aspen Distribution Shifts:
- Historical range baseline for aspen trees was documented from 1971 to 2000.
- Climate modeling predicts a substantial northward shift in aspen range between 2071 and 2100.
- Regions in the northern United States and southern Canada are projected to become too warm to support characteristic boreal tree species like aspen and spruce.
- Direct Observational Evidence:
- Comparative photographs taken of the exact same Arctic plot of land in 1962 and 2004 document tree lines and boreal forest vegetation creeping steadily northward into previously frozen terrain.
Concept Explanation Skill Application
- Skill Practice Exercise:
- Task: Identify one characteristic of a biome and explain how that characteristic determines the community of organisms found in that biome.
- Operational Philosophy:
- "Think like a mountain, write like a scholar."