Biomes: Terrestrial and Aquatic - Study Notes

Key Concepts and Definitions

  • Biome: an area that shares a combination of average yearly temperature and precipitation (climate).

    • Example: camels & cacti have water-preserving traits suited to desert conditions; shrubs & wildflowers store energy in roots to recover quickly after fire in grasslands.

  • Nutrient availability shapes which plants can grow in a biome:

    • Tropical rainforest: nutrient-poor soil due to rapid nutrient uptake and heavy rainfall.

    • Boreal forest: nutrient-poor soil due to cold temps and slow decomposition.

    • Temperate forest: nutrient-rich soil due to abundant litter and favorable decomposition.

    • Tundra: low soil nutrients because frozen soils prevent decomposition of dead organic matter.

  • Shifting Biomes: as climate changes, biome locations shift (e.g., boreal forests moving north as tundra permafrost melts and lower latitudes warm).

Biome Distribution: Latitude, Altitude, and Climate

  • Latitude (distance from equator) determines typical temperature and precipitation patterns, leading to predictable global biome patterns.

  • Latitudinal zones:

    • Tundra & Boreal: higher latitudes (6060^\circ+).

    • Temperate: mid-latitudes (3030^\circ6060^\circ).

    • Tropical: closer to the equator (near 00^\circ).

  • Altitude can mimic latitude: mountains host distinct biomes at different elevations.

  • A climograph (Page 7) combines monthly temperature and precipitation:

    • Temperature: line graph

    • Precipitation: bar graph

    • A regional climate profile helps predict which biomes occur where.

The Earth's Major Terrestrial Biomes

  • Tropical rainforest

  • Tropical seasonal forest / savanna

  • Subtropical desert

  • Woodland / shrubland

  • Temperate grassland / cold desert

  • Temperate seasonal forest

  • Temperate rainforest

  • Boreal forest (taiga)

  • Tundra

  • Polar ice cap

Deserts: Types and Characteristics

  • (Sub)tropical deserts: found at the equator.

  • Temperate deserts: found at mid latitudes.

  • Cold deserts: found in polar regions.

Desert Adaptations (Plants and Animals)

  • Plant adaptations:

    • Shallow root systems or very deep taproots to access water.

    • Large water-storage vesicles.

    • Waxy leaves or reduced leaf surface area; some have leaves absent.

    • Thorns or spines to reduce water loss and deter herbivores.

    • CAM-like water-use strategies: Uptake CO₂ at night to minimize water loss.

  • Animal adaptations:

    • Small body size, long limbs, efficient water use.

    • Nocturnal behavior to avoid daytime heat.

    • Burrowing to escape heat and conserve moisture.

  • Ecological context:

    • Fragile ecosystems with slow plant growth and slow nutrient recycling.

    • Low species diversity and low water availability limit plant survival.

Grasslands and Savannas

  • Clump-forming trees in some savannas; grazing animals common.

  • Fire regimes select for fire-adapted species and rapid regrowth.

Tundra and Alpine Environments

  • Arctic tundra: permafrost; low nutrients; slow plant growth.

  • Alpine tundra: high elevation with cold temps and more sunlight than arctic tundra.

  • Plant adaptations: shallow, networked root systems; seeds germinate after fire events.

  • Animal adaptations: being fast, grazing specialists, camouflage; long limbs/velocity help in open landscapes.

Forest Biomes: Tropical, Temperate, Boreal

  • Tropical (Rainforest):

    • High temperature and moisture.

    • Stratification of niches and rapid nutrient cycling despite poor soils.

    • Nutrients largely stored in the canopy.

  • Temperate (Seasonal/Deciduous):

    • Moderate temperature and moisture.

    • Broadleaf trees; rapid decomposition; rich soil.

    • Notable undergrowth diversity in temperate forests.

  • Cold (Coniferous/Boreal/Taiga):

    • Evergreen leaves; waxy, needle-like leaves minimize water loss.

    • Nutrient-poor, acidic soils limit undergrowth.

Tropical RF Adaptations (Vegetation & Animals)

  • Vegetation:

    • Poor soils; most nutrients stored in tree canopies.

    • Broadleaf evergreen leaves.

    • Extreme diversity of niches; sunlight is a limiting factor.

    • Stratification within canopy supports coexistence.

  • Animals:

    • Major pollinators: bees, butterflies, birds, bats.

    • Stratified niches and specialized diets.

Temperate and Boreal Forest Adaptations

  • Deciduous Forest Vegetation:

    • Broadleaf deciduous trees.

    • More ground-level diversity and undergrowth; varied habitats for animals.

  • Boreal Forest Vegetation:

    • Evergreen leaves; waxy needles.

    • Acidic soils hinder undergrowth.

Mountains: Ecological Roles

  • Harbors a majority of the world's forests.

  • Home to many endemic species.

  • Help regulate Earth's climate and influence sea levels.

  • Major storehouses of water; important in hydrologic cycle.

Key Characteristics of Aquatic Biomes

  • Depth: influences how much sunlight reaches plants for photosynthesis.

  • Temperature: warmer water holds less dissolved O₂, limiting the number of organisms that can be supported.

  • Salinity: determines species viability and usage as drinking water (Freshwater vs. estuary vs. ocean).

  • Flow: affects which plants/organisms can survive and how much O₂ can dissolve in water.

Freshwater: Rivers & Lakes

  • Rivers: high O₂ due to continuous mixing with air; transport nutrient-rich sediments; deltas and floodplains are fertile.

  • Lakes: standing bodies of freshwater; important drinking water sources.

    • Littoral zone: shallow water with emergent plants.

    • Limnetic zone: light penetrates; photosynthesis occurs; mainly phytoplankton; no rooted plants.

    • Profundal zone: too deep for sunlight; no photosynthesis.

    • Benthic zone: muddy bottom with invertebrates; nutrient-rich sediments.

Freshwater: Wetlands

  • Wetland: soil submerged/saturated for at least part of the year, shallow enough for emergent plants.

  • Plants adapted to roots submerged in standing water (e.g., cattails, lily pads, reeds).

  • Benefits of wetlands:

    • Stores excess water during storms, reducing floods.

    • Recharges groundwater by absorbing rainfall into soil.

    • Roots filter pollutants from water draining through.

    • High plant productivity due to abundant water and nutrients in sediments.

Wetland Types (Visual Cues)

  • Swamp, Marsh, Reeds & cattails, Cyprus tree (wetland components shown in diagrams on the source).

Estuaries and Mangroves

  • Estuaries: areas where rivers meet the ocean; mix of fresh and salt water; high productivity due to nutrient-rich sediments deposited by rivers.

  • Salt Marshes: coastal estuary habitats in temperate climates; breeding grounds for many fish and shellfish.

  • Mangrove Swamps: mangrove trees with stilt roots stabilize shorelines and provide habitat for many species of fish and shellfish; estuary habitats along tropical coasts.

Coral Reefs

  • Warm, shallow waters beyond the shoreline; most diverse marine biome on Earth.

  • Mutualistic relationship between coral (animals) and algae (plants).

  • Coral sequesters CO₂ to build calcium carbonate exoskeletons; algae provide energy to coral via photosynthesis.

  • Interdependence: coral cannot survive without algae and algae rely on the habitat and CO₂ from coral.

Intertidal Zones

  • Narrow band of coastline between high and low tide.

  • Organisms adapt to crashing waves and direct sun exposure during low tide.

  • Examples: barnacles, sea stars, crabs that attach to rocks.

  • Adaptations like shells and tough outer layers prevent desiccation during low tides.

  • Different zones host different species (e.g., spiral wrack secretes mucus to retain water during low tide).

Open Ocean

  • Low productivity per unit area; primarily algae and phytoplankton support most life.

  • Photic zone: region where sunlight can reach and enable photosynthesis.

  • Aphotic zone (abyssal): too deep for sunlight.

  • Overall, oceanal photosynthesis and respiration contribute substantially to Earth's O₂ and CO₂ exchange.

Key Concepts and Definitions
  • Biome: Area defined by average yearly temperature and precipitation (climate).

    • Example: Camels & cacti adapted to desert; shrubs & wildflowers to grassland fires.

  • Nutrient availability influences plant growth:

    • Tropical rainforest: Poor soil (rapid uptake, heavy rain).

    • Boreal forest: Poor soil (cold, slow decomposition).

    • Temperate forest: Rich soil (abundant litter, good decomposition).

    • Tundra: Low soil nutrients (frozen soils, no decomposition).

  • Shifting Biomes: Climate change causes biome locations to shift.

Biome Distribution: Latitude, Altitude, and Climate
  • Latitude determines temperature, precipitation, and global biome patterns.

  • Latitudinal zones:

    • Tundra & Boreal: Higher latitudes (6060^\circ+).

    • Temperate: Mid-latitudes (3030^\circ6060^\circ).

    • Tropical: Near the equator (near 00^\circ).

  • Altitude mimics latitude: Mountains host diverse biomes at different elevations.

  • A climograph (Page 7) shows monthly temperature (line) and precipitation (bar) to predict biome occurrence.

The Earth's Major Terrestrial Biomes
  • Tropical rainforest

  • Tropical seasonal forest / savanna

  • Subtropical desert

  • Woodland / shrubland

  • Temperate grassland / cold desert

  • Temperate seasonal forest

  • Temperate rainforest

  • Boreal forest (taiga)

  • Tundra

  • Polar ice cap

Deserts: Types and Characteristics
  • (Sub)tropical deserts: Equator.

  • Temperate deserts: Mid-latitudes.

  • Cold deserts: Polar regions.

Desert Adaptations (Plants and Animals)
  • Plant adaptations:

    • Shallow or deep taproots.

    • Large water-storage vesicles.

    • Waxy/reduced/absent leaves; thorns/spines.

    • CAM water-use: CO₂ uptake at night.

  • Animal adaptations:

    • Small, long limbs, efficient water use.

    • Nocturnal.

    • Burrowing.

  • Ecological context:

    • Fragile ecosystems: slow growth, slow nutrient recycling.

    • Low diversity; low water limits plant survival.

Grasslands and Savannas
  • Clump-forming trees in some savannas; common grazing animals.

  • Fire regimes select for fire-adapted species and rapid regrowth.

Tundra and Alpine Environments
  • Arctic tundra: Permafrost, low nutrients, slow plant growth.

  • Alpine tundra: High elevation, cold, more sunlight than arctic tundra.

  • Plant adaptations: Shallow, networked roots; seeds germinate after fire.

  • Animal adaptations: Fast, grazing specialists, camouflage; long limbs aid movement.

Forest Biomes: Tropical, Temperate, Boreal
  • Tropical (Rainforest):

    • High temperature and moisture.

    • Niche stratification, rapid nutrient cycling despite poor soils.

    • Nutrients mainly in canopy.

  • Temperate (Seasonal/Deciduous):

    • Moderate temperature and moisture.

    • Broadleaf trees; rapid decomposition; rich soil.

    • Diverse undergrowth.

  • Cold (Coniferous/Boreal/Taiga):

    • Evergreen, waxy, needle-like leaves (minimize water loss).

    • Nutrient-poor, acidic soils limit undergrowth.

Tropical RF Adaptations (Vegetation & Animals)
  • Vegetation:

    • Poor soils; most nutrients in tree canopies.

    • Broadleaf evergreen leaves.

    • Extreme niche diversity; sunlight is limiting.

    • Canopy stratification supports coexistence.

  • Animals:

    • Major pollinators: bees, butterflies, birds, bats.

    • Stratified niches, specialized diets.

Temperate and Boreal Forest Adaptations
  • Deciduous Forest Vegetation:

    • Broadleaf deciduous trees.

    • More ground-level diversity and undergrowth; varied animal habitats.

  • Boreal Forest Vegetation:

    • Evergreen, waxy needles.

    • Acidic soils hinder undergrowth.

Mountains: Ecological Roles
  • Harbors most of the world's forests.

  • Home to many endemic species.

  • Regulate Earth's climate and influence sea levels.

  • Major water storehouses; important in hydrologic cycle.

Key Characteristics of Aquatic Biomes
  • Depth: Influences sunlight for photosynthesis.

  • Temperature: Warmer water holds less dissolved O₂.

  • Salinity: Determines species viability and drinking water use.

  • Flow: Affects organism survival and O₂ dissolution.

Freshwater: Rivers & Lakes
  • Rivers: High O₂ (mixing with air); transport nutrient-rich sediments; fertile deltas/floodplains.

  • Lakes: Standing freshwater, important drinking water sources.

    • Littoral zone: Shallow, emergent plants.

    • Limnetic zone: Light penetrates, photosynthesis; phytoplankton; no rooted plants.

    • Profundal zone: Too deep for sunlight; no photosynthesis.

    • Benthic zone: Muddy bottom, invertebrates; nutrient-rich sediments.

Freshwater: Wetlands
  • Wetland: Soil submerged/saturated part of year, shallow enough for emergent plants.

  • Plants adapted to submerged roots (e.g., cattails, lily pads, reeds).

  • Benefits:

    • Stores excess water during storms, reduces floods.

    • Recharges groundwater by absorbing rainfall.

    • Roots filter pollutants.

    • High plant productivity (water, nutrients).

Wetland Types (Visual Cues)
  • Swamp, Marsh, Reeds & cattails, Cyprus tree (visual cues from diagrams).

Estuaries and Mangroves
  • Estuaries: Rivers meet ocean; fresh/salt mix; high productivity (river sediments).

  • Salt Marshes: Coastal estuary, temperate; breeding grounds for fish/shellfish.

  • Mangrove Swamps: Mangrove trees with stilt roots; stabilize shorelines, habitat; tropical coasts.

Coral Reefs
  • Warm, shallow waters; most diverse marine biome.

  • Mutualism: coral (animals) and algae (plants).

  • Coral sequesters CO₂ to build CaCO₃ exoskeletons; algae provide energy via photosynthesis.

  • Interdependence: Coral relies on algae, algae on coral habitat/CO₂.

Intertidal Zones
  • Narrow coastline band between high/low tide.

  • Organisms adapt to crashing waves and sun exposure at low tide.

  • Examples: barnacles, sea stars, crabs attached to rocks.

  • Adaptations (shells, tough layers) prevent desiccation.

  • Different zones host different species (e.g., spiral wrack secretes mucus to retain water).

Open Ocean
  • Low productivity per unit area; primary life from algae/phytoplankton.

  • Photic zone: Sunlight reaches for photosynthesis.

  • Aphotic zone (abyssal): Too deep for sunlight.

  • Ocean photosynthesis/respiration significantly contributes to Earth's O₂/CO₂ exchange.