A terrestrial ecosystem is a land-based ecological system where biotic components (living organisms) interact with abiotic components (non-living physical and chemical factors).
Covers approximately 28–29% of Earth's surface (land area).
Organized into large ecological regions called biomes.
Distribution is mainly controlled by:
Temperature
Precipitation
Latitude
Altitude
Components
A. Biotic Components
Producers (Autotrophs)
Green plants and photosynthetic organisms.
Convert solar energy into chemical energy through photosynthesis.
Form the primary productivity base.
Consumers (Heterotrophs)
Primary consumers (herbivores)
Secondary/Tertiary consumers (carnivores, omnivores)
Decomposers (Detritivores & Saprotrophs)
Bacteria and fungi.
Responsible for nutrient cycling and mineralization.
B. Abiotic Components
Soil (edaphic factors)
Climate (temperature, precipitation, humidity)
Solar radiation
Topography
Wind patterns
These factors regulate primary productivity, species distribution, and ecosystem functioning.
3. Functional Processes
Energy flow (unidirectional)
Biogeochemical cycles (carbon, nitrogen, phosphorus cycles)
Carbon sequestration
Ecological succession
Trophic dynamics
Forest Ecosystems
A forest ecosystem is a terrestrial biome characterized by high tree density, vertical stratification, and high biomass.
Classification Basis:
Latitude
Climate (temperature + rainfall)
Vegetation type (leaf morphology)
A. Tropical Forests
Location:
Near the equator (0°–10° latitude).
Climate:
High temperature (25–30°C average)
Annual rainfall > 200 cm
No distinct winter
Key Features:
High Net Primary Productivity (NPP)
Multi-layered canopy structure:
Emergent layer
Canopy
Understory
Forest floor
Extremely high species richness and endemism
Rapid nutrient cycling but nutrient-poor soils
Ecological Importance:
Major global carbon sink
High biodiversity reservoir
B. Temperate Forests
Location:
Mid-latitudes (30°–50°).
Climate:
Moderate rainfall
Distinct seasons
Types:
Deciduous forests
Broad-leaved trees
Seasonal leaf shedding (adaptation to cold/drought)
Temperate coniferous forests
Needle-leaved evergreen trees
Soil:
Relatively fertile compared to tropical forests.
C. Boreal Forest (Taiga)
Location:
High latitudes (50°–70° N).
Climate:
Long, severe winters
Short growing season
Moderate precipitation (mostly snow)
Vegetation:
Coniferous species (needle-leaved)
Adapted to cold and low evaporation
Ecological Role:
Stores large amounts of carbon in biomass and soils
Lower species diversity but large geographic extent
Specialized Forest Types
1. Mediterranean Forests
Hot, dry summers
Sclerophyllous vegetation (thick leaves)
2. Montane Forests
Altitudinal zonation
Temperature decreases with elevation
3. Mangrove Forests
Coastal intertidal zones
Salt-tolerant (halophytic) vegetation
Shoreline stabilization and storm buffering
2. Grassland Ecosystems
Grasslands are terrestrial ecosystems dominated by grasses and herbaceous vegetation, with insufficient rainfall to support dense forests.
Coverage:
~20% of global land surface.
Climate Control:
Moderate to low precipitation
Seasonal rainfall
Periodic fires and grazing
A. Tropical Grasslands (Savanna)
Features:
Wet and dry seasons
Scattered trees
High grazing pressure
Ecological Traits:
Fire-adapted vegetation
Large herbivore populations
B. Temperate Grasslands
Climate:
Cold winters
Hot summers
Soil:
Deep, fertile chernozem soils
High organic matter
Examples:
Prairies
Steppes
Pampas
C. Montane Grasslands
Occur at high altitudes
Short growing season
Alpine meadows
D. Flooded Grasslands
Seasonally inundated
High productivity
Important wetlands
E. Desert/Xeric Grasslands
Transition zones between grassland and desert
Sparse vegetation
3. Desert Ecosystems
Deserts are terrestrial ecosystems characterized by extremely low precipitation (<25 cm annually) and high evapotranspiration rates.
Key Characteristics
Large diurnal temperature variation
Low primary productivity
Sandy or rocky soils
Low organic matter
Types of Deserts
Hot and dry
Semi-arid
Coastal
Cold deserts
Adaptations
Plants:
Xerophytes
Succulents
Reduced leaf surface area
CAM photosynthesis
Animals:
Nocturnal behavior
Water conservation mechanisms
4. Mountain Ecosystems
Mountain ecosystems are characterized by altitudinal zonation, where climate and vegetation change with elevation.
Key Concepts
Environmental lapse rate (temperature decreases with altitude)
"Water towers of the world" (source of rivers)
High endemism
Zonation
Foothill forests
Montane forests
Subalpine zone
Alpine tundra
Permanent snow
5. Tundra Ecosystems
Tundra is a treeless biome with extremely low temperatures and the presence of permafrost (permanently frozen subsoil).
Types
Arctic tundra (high latitude)
Alpine tundra (high altitude)
Characteristics
Short growing season (6–10 weeks)
Low precipitation (but low evaporation)
Poorly developed soil
Vegetation
Mosses
Lichens
Dwarf shrubs
Sedges
Faunal Adaptations
Thick fur/insulation
Migration
Hibernation
Comparative Analysis
| Feature | Desert | Tundra | Grassland | Forest |
|---|---|---|---|---|
| Water availability | Very low | Frozen water | Moderate seasonal | High (varies by type) |
| Biodiversity | Low | Low–moderate | Moderate | Very high (tropical) |
| Soil fertility | Poor | Poor | High (temperate) | Variable |
| Temperature | Extreme heat/cold | Persistently cold | Seasonal | Climate dependent |
Ecological Importance of Terrestrial Ecosystems
Carbon sequestration
Oxygen production
Climate regulation
Biodiversity conservation
Soil formation
Water cycle regulation
Provisioning services (food, timber, fiber)
Core Controlling Factors
Latitude
Altitude
Precipitation
Temperature
Soil type
Disturbance regimes (fire, grazing, storms)
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