🌊 APES Topic 1.3: Aquatic Biomes

1. Key Characteristics / Environmental Factors

These are the main abiotic (non-living) factors that determine what aquatic biomes look like, which species can survive there, and how productive they

Factor

What it means / how it works

Effects on Organisms & Biome

Flow

How much water movement there is (rivers, currents, waves, etc.)

Affects oxygen mixing; influences what sorts of plants & animals can anchor themselves or move; transports nutrients & sediments.

Salinity

How much salt is in the water (freshwater vs. brackish vs. marine)

Determines which species can live there (many are salt-tolerant or not), osmoregulation challenges, etc.

Temperature

How warm (or cold) the water is; also seasonal variation

Warmer water holds less dissolved oxygen => fewer organisms; influences metabolic rates, species distributions.

Depth / Light Penetration

How deep the water is; whether sunlight can reach the bottom or not

Determines where photosynthesis can happen; which plants or algae can be rooted; where producers are.

Dissolved Oxygen (DO)

How much oxygen is dissolved in water

Critical for aerobic aquatic organisms; higher flow or turbulence helps increase DO; warm, stagnant water tends to have less DO.

2. Types of Aquatic Biomes & Their Zones / Examples

Here are the main aquatic biomes discussed, plus the internal zones/components, and important features / species adaptations.

A. Freshwater Biomes
  • Rivers and Streams

    • Flowing water; good mixing of water and air, leading to often high dissolved oxygen.

    • Carry sediments and nutrients downstream, contributing to fertile floodplains.

  • Lakes

    • Divided into zones:

    • Littoral zone: Shallow water near the shore, supporting emergent plants.

    • Limnetic zone: Open water where light reaches and photosynthesis occurs; often rich in algae & phytoplankton.

    • Profundal zone: Deeper water, too dark for photosynthesis.

    • Benthic zone: Bottom sediments where invertebrates (bugs, etc.) live in nutrient-rich material.

  • Wetlands

    • Areas where soil is saturated or submerged for part of the year; shallow enough for plants to grow with roots in water.

    • Plant types: Cattails, reeds, lily pads, and other emergent vegetation, all adapted to waterlogged soils.

    • Ecosystem services / benefits: Provide flood buffering, water purification, and high productivity thanks to nutrient and organic matter accumulation in sediments.

B. Estuaries & Brackish Biomes
  • Occur where freshwater mixes with saltwater (e.g., where a river meets the ocean).

  • Examples: Includes mangrove swamps (in tropical climates) and salt marshes (in temperate climates).

  • Adaptations: Organisms must tolerate changing salinity; plants like mangroves have special root systems (often stilt-roots) to cope with salt and waterlogging.

  • Productivity: Very productive due to nutrient input from sediments, sufficient light in shallow areas, and mixing encouraging growth.

C. Marine / Oceanic Biomes
  • Coral Reefs

    • Found in warm, shallow, clear waters beyond the shoreline.

    • Known for very high biodiversity.

    • A key mutualistic relationship exists between coral animals and photosynthetic algae (zooxanthellae).

    • Corals build calcium carbonate skeletons, providing structure and habitat; algae supply sugars via photosynthesis.

  • Intertidal Zones

    • The narrow band of coastline between high tide and low tide.

    • Organisms must tolerate significant fluctuations: waves, exposure to air (heat, desiccation), and changing salinity.

    • Examples: Barnacles, crabs, sea stars, and other organisms that can cling to rocks or seal themselves off.

  • Open Ocean (Pelagic Zones)

    • A very large biome; much of the ocean is low in nutrients and productivity per area, especially in deeper zones.

    • Zones:

    • Photic Zone: Where sunlight penetrates, allowing for photosynthesis.

    • Aphotic Zone: No sunlight; organisms rely on detritus, chemosynthesis, or predation.

    • Although productivity per area can be low, the ocean's immense size means its total contribution to global oxygen & carbon cycling is large, primarily through phytoplankton and algae.

3. Adaptations & Special Features
  • Salinity Tolerance: Many aquatic organisms are adapted to varying salinity, particularly in estuaries.

  • Root Adaptations: Some plants, such as mangroves, have roots specifically adapted to deal with salt and water movement.

  • Intertidal Adaptations: Organisms in intertidal zones often possess strong anchoring mechanisms (to rocks), shells, or coverings to resist drying and wave action.

  • Depth / Light Adaptations: Organisms in deep water typically do not rely on sunlight for energy, whereas those near the surface have adaptations for photosynthesis.

4. Ecosystem Services & Importance
  • Wetlands: Provide crucial flood control, water filtration, and nutrient cycling.

  • Estuaries & Coastal Zones: Serve as critical breeding grounds for fish & shellfish.

  • Coral Reefs: Protect coastlines, support high biodiversity, and contribute to tourism & fisheries.