IL

Biodiversity and Conservation Bio-3/13/25

Ecosystems and Global Ecology

  • Biomass: flow of energy

  • Ecosystem: community of interacting species

  • Biosphere: thin zone of soil, water, and the atmosphere surrounding earth


Energy Flow

  • Primary producer/autotroph: make their own food

    • Via energy in sunlight into chemical energy

    • Exception: areas in deep sea of hydrothermal vent: use methane 

  • Primary production

    • Gross primary productivity: total amount of chemical energy produced 

    • Chemical energy can be used for: 

      • cellular respiration and 

      • anything else can be put into growth and reproduction (NPP)

        • NPP creates biomass

    • Fate of biomass

      • Consumers eat living organisms

        • Primary

        • Secondary

        • Tertiary

        • Decomposers

      • Trophic level: organisms that obtain energy from the same source occupy the same trophic level

      • Diagram on right: 

        • Black arrows get smaller going up to show energy given off as heat

    • Trophic Structure

      • Food chain: one possible pathway

        • Grazing food chain: composed of herbivores and organisms that eat them

        • Decomposer food chain: made up of species that eat detritus (primary decomposer)

        • Consumers can be part of multiple food chains

        • Consumers can feed on multiple trophic levels

        • Food web: sum of all trophic or feeding interactions in an ecosystem

    • Transfer of biomass

      • Productivity: biomass produced within an area over a period of time

      • Biomass declines as you move up trophic levels

      • 10% of biomass gets transferred up each trophic level

        • Reason: most consumed energy is used for cellular processes

        • Efficiency: amount of energy that moves from one trophic level to the next (in percent, about 10%)

          • Larger organisms: less surface area to volume so less heat lost

      • Biomagnification: the increase of a molecules at higher trophic levels

        • Common for molecules that don’t break down quickly 

        • Examples: mercury, organic pollutants

        • The greater the number of trophic levels, the higher the health impacts on top consumers

    • Nutrient Cycling

      • Cycling: energy transferred when one organism eats another

      • Nutrients that are essential to life are also transferred 

        • Carbon, nitrogen, phosphorus, sulfur, calcium

      • Biogeochemical cycle: the path an element takes as it moves from abiotic reservoirs to organisms and back again

      • Example: terrestrial cycling

        • Nutrient in the soil taken up into a plant

        • Plant transforms nutrients into organic form

        • When eaten, nutrients go to consumer

        • Waste and eventual death are taken up by decomposers

        • Decomposers convert into inorganic form

        • Ultimate source of nutrients for cycling comes from

        • the environment (can also be lost to it)

      • Nutrient loss examples

        • Co2 is released to the atmosphere during cellular respiration

        • An herbivore eating a plant and then leaving the ecosystem

        • Transport of the exosystem by flowing water or wind

        • Plant removals due to agriculture

      • Nutrient gain examples

        • Rocks being broken down or weathered

        • Transport into the ecosystem by flowing water or wind

        • Carbon is added when primary producers fix it during photosynthesis

      • Factors limiting nutrient cycling (3 factors)

        • Rate of nutrient decomposition

        • Abundance and diversity of detritivores

        • Quality of the detritus, some things are harder to breakdown than others

          • Detritus: waste or debris 

      • The Nitrogen cycle

        • Atmosphere is the largest nitrogen reservoir but is unavailable to plants

        • Nitrogen needs to be fixed before it is biologically usable

        • Can be fixed by 

          • Enzyme catalyzed reactions in bacteria

          • lighting -driven reactions in the atmosphere

      • The phosphorus cycle

        • Main reservoir is in earth’s crust

        • Available by the weather of rocks and deposition in soils

        • Humans mine phosphorus as a fertilizer and have increased its abundance in the global cycle by four times in the last 75 years

      • Carbon cycle

        • Largest reservoir is in the ocean

        • Atmosphere reservoir is not the largest but important because it can be cycled quickly from the atmosphere

        • Photosynthesis takes carbon out of atmosphere into tissues

        • Anthropogenic impacts: changes caused by human activities

          • Intensive agriculture, deforestation, etc

          • Burning fossil fuels

Climate change

  • Terminology

    • Weather: short term and variable

    • Climate: long-term pattern of regional and global weather

    • Global warming: increase in the average temperature of the planet

    • Global climate change: sum of all the changes in local temperature and precipitation patterns that result from global warming

  • Causes

    • The Greenhouse Effect

      • Solar radiation either reflects off the earth or is absorbed and warms it

      • Much of the heat reemitted gets trapped around the earth by the atmosphere, CO2 is really good at absorbing the heat

      • Increased CO2=Higher retention of heat around the earth

      • Biological effects

        • Range shifts: species moving towards poles as suitable habitat moves

        • Phenology shifts: changes in processes that happen on the seasonal cycle (ex. When organisms mate, migrate, etc.)

        • Evolutionary adaptation: climate change can impact allele frequencies by favoring certain traits over others (ex. Ladybugs with primarily black shield are selected against) 

        • Extinctions: rising temperatures can be too much for species and they cannot adapt or move quickly enough

        • Ocean acidification: increased CO2 in the atmosphere causes a lower pH in the ocean that can erode calcium carbonate shells

          • Co2 in atmosphere can be quickly brought into the carbon cycle


Biodiversity and Conservation

  • Biodiversity: biological diversity

  • Species richness and species diversity

    • Richness: # of species in the community

    • Diversity: richness and evenness both taken into account

  • Genetic diversity: can also be used to measure diversity

    • Can be used to measure the adaptive capacity of a community

  • Phylogenetic diversity: measure of diversity that is higher when species are more distantly related 

    • Measured by length of the branches in the phylogenetic tree

  • Functional diversity: variation in ecological traits

  • Ecosystem diversity: a measure of diversity that emphasized the complexity of species interactions 

  • Distribution of biodiversity

    • Global trends

      • Higher diversity closer to the equator 

      • Higher diversity of land than on sea

        • Possible reasons: insects

      • Higher diversity in areas with greater geographical variation 

    • Biodiversity in peril

      • Rates of extinction are increasing

    • Threats to biodiversity

      • Habitat loss: MOST IMPORTANT FACTOR

      • Harvest overexploitation

        • Marine species most susceptible to this

        • Ex. overfishing

      • Climate change

    • Benefits of biodiversity

      • Direct and indirect benefit to humans

      • Ecosystem services

        • Est. $125 trillion per year

    • Preserving biodiversity

      • Sustainability

      • Management plans

      • Ecosystem restoration

      • Wildlife corridors