Ch. 24 Ecology

Ecology: Study of Organisms in Relation to Their Environment

  • Ecology is defined as the study of organisms in relation to their environment.

  • Population: A group of organisms living in the same area at the same time.

  • Species: A group of organisms that can interbreed and produce fertile, viable offspring.

  • Community: Multiple populations (e.g., humans, coyotes, palm trees, butterflies) living in the same area at the same time.

  • Ecosystem: The interaction between biotic (living community) and abiotic (non-living components like soil, temperature, water) factors.

  • Habitat: The place where a species lives.

Biotic and Abiotic Factors

  • Biotic factors: Living factors such as organisms themselves, diseases (e.g., avian flu), and interspecific interactions (predation, commensalism, herbivory).

  • Abiotic factors: Non-living factors such as climate, temperature, water, salinity, and pH.

  • Example of pH affecting organisms: Hydrangeas change flower color based on soil pH (acidic = blue, alkaline = reddish).

  • Edaphic: Relating to soil.

Biomes

  • Biomes are major ecosystems spread over wide geographic areas with similar climatic conditions and similar flora and fauna.

  • Includes terrestrial and aquatic types.

  • Desert biomes share similar characteristics of temperature, precipitation, and weather patterns worldwide.

  • Climate determines the biome, and climate is determined by temperature and precipitation.

  • Climber graphs illustrate the distribution of biomes based on temperature and precipitation.

Roger Weteger’s Biome Distribution

  • Based on the relationship between temperature and precipitation.

  • X-axis represents a negative scale.

    • Tropical rainforest: High temperatures and high precipitation.

    • Tundra: Extremely low temperatures and low precipitation.

Factors Affecting Temperature

  • Tropics receive sunlight at 90 degrees, resulting in higher temperatures.

  • Temperate regions and poles receive sunlight at higher angles, resulting in lower temperatures.

Seasons

  • Determined by the permanent tilt of the Earth (23.5 degrees).

  • Northern Hemisphere summer: Tilted towards the sun, while Southern Hemisphere experiences winter.

  • Revolution of the Earth around the sun causes seasons.

  • Aquatic biomes are shaped by ocean currents and water salinity.

  • Estuary: Junction between a river and a sea/ocean with mixing of fresh and saline water.

Niche

  • The ecological role or profession of a species (e.g., an oak tree).

  • Ecological services provided: photosynthesis (producing oxygen), providing shade, acorns for squirrels, habitat for animals, and preventing soil erosion.

  • No two species can have the same niche; otherwise, competition occurs, and one species may outcompete the other.

Flow of Energy and Chemicals

  • Energy flows through an ecosystem and is lost.

  • Chemicals (nutrients) are recycled through biogeochemical cycles.

Nutrient Cycles

  • Water cycle, nitrogen cycle, carbon cycle, and phosphorus cycle (phosphorus cycle lacks an atmospheric component).

Water Cycle
  • Water is lost from terrestrial ecosystems through transpiration (loss of water from aerial parts of plants).

  • Water flows into rivers and streams via runoff.

  • Evaporation transforms liquid water into a gaseous state.

  • Condensation: As air rises, temperature drops, causing water vapor to become water droplets.

  • Precipitation: Water falls back to Earth as rain.

Biogeochemical Cycles
  • Involve both biotic and abiotic components, including abiotic reservoirs such as rivers, streams, rocks, and the atmosphere.

Nitrogen Cycle
  • Nitrogen is a vital component for living organisms, abundant in the atmosphere (79%).

  • Essential for plant growth, proteins, and DNA.

Stages of the Nitrogen Cycle

  • Nitrogen fixation: Atmospheric nitrogen converted to ammonium.

    • Acetobacter: Free-living bacteria in soil.

    • Rhizobium: Resides in root nodules of leguminous plants.

    • Cyanobacteria: Blue-green bacteria.

    • Lightning.

    • Haber process: Industrial process combining nitrogen and hydrogen to produce ammonia.

  • Nitrification: Ammonium converted to nitrite (NO2), then to nitrate (NO3).

    • Nitrosomonas: Converts ammonium to nitrite.

    • Nitrobacter: Converts nitrite to nitrate.

    • Nitrate is the form usable by plants (assimilation).

  • Assimilation: Nitrogen gets incorporated into plant parts.

  • Denitrification: Nitrate converted back to nitrogen.

    • Pseudomonas denitrificans bacteria facilitate this conversion.

Human Disruption of Nitrogen Cycle
  • Causes: Eutrophication, acid rain, and photochemical smogs.

  • Eutrophication: Excess nutrients (N, P, K) from fertilizers cause algal bloom in bodies of water.

    • Algae die, aerobic bacteria decompose them, oxygen levels drop, leading to fish death.

    • Natural eutrophication occurs over centuries, while cultural (anthropogenic) eutrophication is accelerated and occurs in decades.

  • Acid Rain: Sulfur dioxide and nitrogen oxides react with water to form sulfuric and nitric acids.

    • Damages forests, decays leaves, corrodes marble statues.

  • Photochemical Smog: Oxides in the atmosphere react in the presence of light.

  • Thermal Inversion: Pollutants trapped between two layers of cold air, preventing dispersion.

    • Usually, warm air rises, but cold air gets trapped in thermal inversion scenarios.

    • Thermal inversion ceases when sunlight heats up the Earth’s surface.

Greenhouse Gases

  • Greenhouse gases include carbon dioxide, methane, oxides of nitrogen, chlorofluorocarbons, sulfur dioxide, and water vapor.

Greenhouse Effect

  • Greenhouse gases trap incoming Earth's rays, warming the surface.

  • Without greenhouse gases, Earth would be frigid.

  • Incoming high-energy rays (e.g., UV) are converted to infrared upon striking the Earth’s surface.

  • Greenhouse gases reflect infrared radiation back to Earth. Excessive amounts of this reflection cause global warming.

  • Ozone shields the Earth and chlorofluorocarbons erode the ozone layer by colliding against it through chain reactions over many years.

Consequences of Global Warming

  • Ice caps are shrinking.

  • Weather patterns are changing.

  • Ocean pH decreases, harming mollusks.

  • Permafrost melts, damaging infrastructure.

  • Disease-carrying insects migrate from tropics to temperate regions.

Food Chains and Food Webs

  • Inedible parts (hooves, nails, claws, fur) and feces lead to carbon loss.

  • 10% Rule: Only 10% of energy is transferred from one trophic level to the next, due to entropy and the laws of thermodynamics.

  • Energy can neither be created nor destroyed.

Feeding Relationships

  • Autotrophs: Inorganic carbon source (carbon dioxide).

    • Producers making their own food.

    • Photoautotrophs use light as their energy source.

    • Chemoautotrophs use chemicals as their energy source.

  • Heterotrophs: Organic carbon source.

    • Rely on autotrophs.

    • Consumers (primary, secondary) eat producers or other consumers.

    • Decomposers rely on dead organic matter.

      • Detritivores (e.g., earthworms) ingest dead organic matter.

      • Saprotrophs (bacteria, fungi) secrete enzymes, break down polymers into monomers, and absorb them.

Trophic Level
  • Position of an organism in a food chain.

  • Food chain: Linear sequence of energy transfer between trophic levels.

    • Arrows denote the flow of energy, not who eats whom.

  • Food web: Interconnected food chains.

Ecological Pyramids
  • Graphical representation of relationships between trophic levels.

    • Pyramid of numbers: Represents the number of organisms.

    • Pyramid of biomass: Shows the flow of energy over time in terms of energy.

    • Pyramid of energy: Illustrates the flow of energy between trophic levels.

Limitations of Food Chain Size
  • Limited due to the 10% rule; energy available diminishes at higher trophic levels, limiting chain length.

Activists

  • Greta Thunberg is a notable environmental activist. Look her up.