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