Principles of Ecology

Principles of Ecology

The Biosphere

  • The biosphere is described as the zone of life on Earth.

  • Two primary categories of biomes:

    • Terrestrial Biomes

    • Aquatic Zones

Terrestrial Biomes

Key Concepts
3.1 Characterization of Terrestrial Biomes
  • Terrestrial biomes are characterized primarily by dominant vegetation forms.

    • Plants are categorized based on growth forms rather than taxonomic relationships.

Learning Objectives:
  • Explain why plant growth forms are used to categorize terrestrial biomes.

  • Describe how global patterns of precipitation and temperature influence the location of terrestrial biomes.

  • Evaluate the impact of human activities on the distribution of biomes.

  • Describe the nine major terrestrial biomes.

Human Activities and Biomes

  • Human activity can significantly impact the distribution and health of various biomes:

    • Logging, agriculture, and land conversion contribute to habitat loss.

    • Example: About 50% of tropical rainforest biome has been altered, which complicates recovery due to nutrient-poor soils.

    • Nutrients are locked in vegetation above ground, resulting in decreased soil fertility after deforestation.

Aquatic Ecosystems

3.2 Freshwater Ecosystems
  • Biological zones in freshwater ecosystems, such as rivers and lakes, depend on factors including:

    • Velocity

    • Depth

    • Temperature

    • Clarity

    • Chemistry

Learning Objectives:
  • Explain how these factors affect streams and rivers of different orders, and lakes.

3.3 Marine Biological Zones
  • Marine environments are determined by:

    • Ocean depth

    • Light availability

    • Bottom substrate stability

Learning Objectives:
  • Explain how depth and substrate types influence aquatic life.

  • Analyze how energy sources and food availability affect marine organism populations.

Growth Forms and Environmental Indicators
  • Vegetation (plants) serves as a long-lasting indicator of climatic conditions in specific areas.

  • Different growth forms reveal specific environmental adaptations:

    • For example, sclerophyllous shrubs grow in seasonally dry climates, demonstrating adaptations to water storage.

Examples of Plant Growth Forms

Figure 3.3 Plant Growth Forms (Part 1) and (Part 2)
  • Growth forms illustrate environments and characteristics:

    • Sclerophyllous Shrubs: Adapted to dry/moist, warm/cool environments.

    • Deciduous Trees: Shed leaves, indicating adaptation to seasonal changes.

    • Succulent Plants: Store water, critical for survival in arid conditions like cacti and euphorbs.

Major Terrestrial Biomes

  • Tropical Rainforests: Located near the equator, characterized by high biodiversity and annual precipitation exceeding 2000 mm.

    • Example: Yanganbi, Zaire 0°, 487 m with average annual temperature 24.6°C.

    • High biomass and species diversity; altered significantly by human practices.

  • Tropical Seasonal Forests and Savannas: Found between tropical regions around 10° to 23.5° N/S with dry seasons.

    • Comprise dry forests and savannas with grasses and scattered trees.

    • Example: Coxim, Brazil 18°S, 287 m with average annual temperature 24.5°C, total annual precipitation 1493 mm.

  • Hot Deserts: Characterized by high temperatures and low water availability.

    • Examples include Sonoran Desert, adapted plant species like cacti that store water.

  • Temperate Grasslands: Maintained by fires and large herbivores; high soil fertility but heavily impacted by agriculture.

    • Example: Denison, Nebraska, USA, with average annual temperature 9.1°C and total annual precipitation 727 mm.

  • Temperate Deciduous Forests: Significant for agriculture; species diversity lower than tropical forests but still notable (approx 3,000 species in North America).

    • Example: Wellsboro, Pennsylvania, USA, with average annual temperature 7.6°C and total annual precipitation 848 mm.

  • Boreal Forests (Taiga): Found mostly in Russia and Northern America; conifers dominant, limited decomposition due to cold and wet conditions.

    • Example: Fort Simpson, Northwest Territories, Canada, with average annual temperature -4.6°C and total annual precipitation 333 mm.

  • Tundra: Located above 65° latitude in Arctic conditions; characterized by permafrost, low-growing vegetation.

    • Example: Olenek, Russia, with average annual temperature -14.3°C and total annual precipitation 184 mm.

Mountain Biological Zones
  • On mountains, biomes are organized by elevation:

    • Higher elevation tends to mimic other biomes such as grasslands, tundra, and boreal forests.

    • Different temperature and precipitation conditions at various elevations lead to distinct zonation.

  • Example of elevation-related zones:

    • Alpine Zone: influenced heavily by temperature and elevation.

Understanding Stream Orders

Stream Characteristics
  • Streams and rivers are categorized as lotic systems, originating at high elevations with first-order streams.

    • First-order streams merge to form higher-order streams, leading to large rivers (6th-order streams).

  • Riparian Zones: Riparian vegetation provides essential organic matter and shade, critical for stream ecology.

Impact of Human Activities

Human Impacts on Ecosystems
  • Significant human impacts on aquatic ecosystems include:

    • Sedimentation from agricultural practices affecting coral reefs and stream habitats.

    • Sewage and industrial waste as pollutants.

    • Deforestation and land conversion leading to habitat loss.

Questions to Consider:
  • Are there associations between specific biomes and latitudinal gradients?

  • Which biomes are more impacted by human activities? Why?

  • Strategies for mitigating human impacts include improved land management practices, pollution reduction techniques, and habitat restoration initiatives.

Conclusion

  • Understanding the dynamics and interconnections of biomes is essential in forming strategies around conservation and sustainable resource management.

  • Addressing the complexities of human-environment interactions remains critical in preserving ecological integrity.