Chapter 5 Notes: Ecosystems to Biomes
Ecosystems
Ecosystems participate in core processes: photosynthesis, respiration, energy flow, and nutrient cycling.
Humans rely on ecosystems and assign value to ecosystem goods and services.
Ecosystems contain communities of interacting species and their abiotic factors.
Range of tolerance and limiting factors control species distribution.
Predictable patterns of ecosystem distribution around the world.
Biomes
Biomes are ecosystems having similar vegetation and climactic conditions.
Trophic levels
In photosynthesis, plants use light energy, CO₂, and H₂O to produce organic molecules (sugar).
Compounds and nutrients move up trophic levels (feeding levels) to other organisms.
Trophic level: feeding level defined by primary source of energy.
Trophic levels show the movement of energy and materials through the food web.
Food chains and Food webs
Food chain: describes where energy and nutrients move with respect to one organism to another; energy moves upward along the chain.
Not all energy and nutrients reach higher trophic levels.
Food web: interconnection of food chains forming a complex feeding network; usually prominent in aquatic systems.
Aquatic food webs (example components)
Base/primary producers: phytoplankton, diatoms (ice biota).
Primary consumers: herbivorous zooplankton, small fish.
Secondary consumers: carnivorous zooplankton, Arctic cod, carnivorous invertebrates.
Higher-level consumers: arctic cod, bearded seal, ringed seal, bowhead whale, beluga whale, polar bear, Arctic fox, Arctic terns, loon, sea ducks.
Key connections: diatoms/phytoplankton → zooplankton → small fish → larger fish/predators; top predators include mammals and seabirds.
Autotrophs, heterotrophs, and functional groups
Autotrophs: produce organic matter (OM) from inorganic matter using an external energy source.
Producers: green plants; photosynthetic and chemotrophic bacteria.
Heterotrophs: consume OM to obtain energy.
Consumers: eat living prey.
Decomposers: scavengers, detritus feeders, and chemical decomposers that eat dead OM.
Producers
Photosynthesis captures light energy to convert CO₂ and H₂O to OM.
Chlorophyll: green pigment in plant leaves responsible for absorbing light energy.
Chemosynthesis: bacteria use energy in inorganic chemicals (e.g., H₂S, NH₃) to synthesize OM.
Primary production: production of OM through photosynthesis and associated growth of organisms/biomass; also termed primary productivity.
Global primary productivity (terrestrial)
Net Primary Production (NPP): classification of new plant biomass in tons per hectare per year of total dry organic matter (above- and below-ground).
Categories (approximate): None, Low (1), High (≈15) (illustrative categories used in the slide).
Consumers (by diet)
Primary consumers (herbivores): eat producers.
Secondary consumers (carnivores): feed on primary consumers.
Tertiary consumers and beyond: feed on other consumers.
Carnivores: secondary or higher-order meat eaters.
Omnivores: feed on both plants and animals.
Grassland food chain (structure)
Producers → First-level (primary) consumers → Second-level consumers → Third-level (tertiary) consumers.
Decomposers and detritus
Decomposers: organisms whose feeding results in decay of OM.
Detritus: dead plant material, waste, and dead bodies; high in potential energy.
Energy from detritus is used by:
Scavengers (e.g., vultures): break down large pieces of matter.
Detritus feeders (earthworms): eat partly decomposed matter.
Chemical decomposers (fungi and bacteria): break down molecule-sized matter.
Specialized decomposers
Some decomposers digest wood (cellulose): termites.
Termites maintain mutualistic relationships with gut microorganisms to digest cellulose.
Cellulose: material in plant cell walls; indigestible by humans; excreted as waste.
Anaerobic respiration: occurs in absence of oxygen in sediments, lakes, marshes, swamps, and animal guts.
Fermentation: modified form of cellular respiration used by some decomposers; breaks down glucose without oxygen; produces ethyl alcohol, methane, acetic acid.
Trophic categories (summary)
Autotrophs: make their own organic matter from inorganic nutrients using environmental energy sources.
Heterotrophs: must feed on organic matter for energy.
Producers:
Photosynthetic green plants: use chlorophyll to absorb light energy.
Photosynthetic bacteria: use light energy.
Chemosynthetic bacteria: use high-energy inorganic chemicals (e.g., H₂S).
Consumers:
Primary consumers/herbivores: feed exclusively on plants.
Omnivores: feed on both plants and animals.
Secondary consumers/carnivores: feed on primary consumers.
Higher-order carnivores: feed on other carnivores.
Parasites: feed on another plant or animal over an extended period.
Decomposers, scavengers, detritus feeders, chemical decomposers (fungi/bacteria).
Limits on trophic levels
Terrestrial ecosystems typically have 3–4 trophic levels; marine systems can have up to 5.
Biomass = total combined (net dry) weight of organisms.
Rule of thumb: each higher trophic level has about 90% less biomass than the level below it.
Example (grassland):
Grass biomass (producers) ≈ 100 (units)
Herbivores (first-level consumers) ≈ 10
Primary carnivores (second-level consumers) ≈ 1
Higher carnivores (third-level consumers) ≈ 0.1
Biomass pyramid: segments show relative biomass at each trophic level.
Biomass pyramid (illustration from slide)
Producers: 100
First-level consumers: 10
Second-level consumers: 1
Third-level consumers: 0.1
Note: The pyramid demonstrates the dramatic drop in biomass at higher trophic levels.
Flow of energy in terrestrial ecosystems
Standing-crop biomass: biomass of primary producers in an ecosystem at a given time (above-ground biomass is often highlighted).
Biomass and primary production vary greatly by ecosystem type and climate:
Forests have large biomass.
Grasslands have high primary production.
Sunlight is the primary energy source for most ecosystems.
Primary production uses only about 2\% of available solar energy, yielding approximately 120\ \text{gigatons of OM/year}.
Fate of food energy
About 60-90\% of ingested energy is oxidized for energy needs.
About 10-40\% is converted to body tissues for growth, repair, and maintenance.
Undigested food is excreted as waste.
Excretions include carbon dioxide, nitrogen, phosphorus, and water (via urine).
Energy flow inefficiency and secondary production
Energy flow between trophic levels is inefficient; only a small percentage is transferred to the next level.
Much biomass is not consumed by herbivores.
Some energy is used for cellular metabolism.
Some is not digested and excreted as waste.
Secondary production: rate of growth of consumers over time; incorporation of matter and energy from a lower trophic level into a consumer's body (tissue formation/growth).
Trophic inefficiency and bioaccumulation
Higher trophic levels require more energy for the same amount of tissue.
More energy, time, water, and resources are needed to produce a consumer than a producer.
Some materials (heavy metals, pesticides) are hard to degrade and can be excreted slowly; they bioaccumulate within individuals and biomagnify up the food chain.
Aquatic systems: key differences from terrestrial systems
Aquatic systems follow similar energy flow with two major differences:
1) More energy is available at each level; energy transfer is more efficient; cold-blooded animals require less energy.
2) Aquatic systems have a reversed biomass pyramid: smaller biomass of algae and greater biomass of larger fish at higher trophic levels.Implications: food chains can be longer; bottom-dwelling organisms (algae/phytoplankton) have shorter lifespans with rapid turnover, while upper-level organisms live longer and may have more biomass per individual.
From ecosystems to biomes
Ecosystem patterns show predictable populations of organisms under particular conditions.
Distinct biotic communities characterize different regions.
Biomes are large geographical terrestrial biotic communities controlled by climate.
Biomes are often named after dominant vegetation and do not have strict boundaries.
Climate and its effects on biomes
Climate = average temperature and precipitation (weather) of a region; varies widely.
Equatorial regions: warm, high rainfall, little seasonality.
Temperate zones: seasonal temperatures.
Polar regions: longer and colder winters.
Average temperature varies with latitude and altitude.
Latitude, altitude, and microclimates
Latitude increases away from the equator; altitude increases away from sea level.
Microclimate: environmental conditions in a localized area can differ from regional climate.
Microclimates create variations of ecosystems within a biome.
Precipitation and species distribution
Precipitation varies from nearly 0 to over 100 inches per year.
Distribution can be even or seasonal.
Climate supports species within their range of tolerance; highest densities occur where conditions are optimal; species are excluded where any condition exceeds their tolerance.
Temperature delineated biomes
Tropical rainforest: cannot tolerate freezing.
Deciduous forest: trees drop leaves and go dormant during freezing temperatures.
Coniferous forests: tolerate harsh winters and short summers (northern regions).
Permafrost: permanently frozen subsoil, roots cannot penetrate; limits tree growth.
Tundra: ecosystem of organisms that can live where permafrost persists.
Distribution of terrestrial biomes
Global map shows latitudinal and altitudinal distribution of biomes (examples include tundra, boreal forests, temperate forests, savannas, deserts, tropical forests).
Aquatic systems: depth, salinity, and permanence
Aquatic and wetland ecosystems are determined by depth, salinity, and permanence of water.
Freshwater systems include lakes, marshes, streams, and rivers.
Mixed gradients exist (estuarine environments) between freshwater and marine systems.
Marine systems include oceans and coastal regions.
Productivity across biomes
Biomes differ in primary productivity; tropical rainforests are among the most productive.
Open oceans contribute a large share of global productivity but individual site productivity is often limited by nutrient availability.
Estuaries and upwelling zones are particularly productive due to nutrient inputs.
Productivity: examples and rankings (illustrative)
Open Ocean: relatively high region-wide productivity but low per-area rates in many zones; productivity often limited by nutrients.
Upwelling zones: among the highest productive marine areas.
Estuaries: extremely productive due to mixing and nutrient influx.
Freshwater lakes/streams: substantial productivity, supporting diverse communities.
Terrestrial productivity varies: dense productivity in tropical rainforests; moderate in temperate forests and grasslands; lower in deserts.
Notable terrestrial productivity examples (order roughly from high to lower): Estuaries, Upwelling zones, Temperate forests, Tropical rainforests, Grasslands, Deserts, Tundra.
Productivity data (selected examples from the slide)
Average annual net primary productivity (g m^{-2} yr^{-1}) and % of global surface area (for context):
Estuary: approximately $1300$ g m^{-2} yr^{-1}$ (high productivity) and substantial local area.
Open Ocean: approximately $125$ g m^{-2} yr^{-1}$ (lower per-area productivity compared with estuaries but vast area).
Upwelling zones: around $500$ g m^{-2} yr^{-1}$ (high productivity).
Continental shelf: around $360$ g m^{-2} yr^{-1}$.
Lake and stream: around $250$ g m^{-2} yr^{-1}$.
Boreal forest / temperate forests: several g m^{-2} yr^{-1} (typical values lower than large open-water zones per unit area but extensive).
Tropical rainforest: among the higher rainforest biomes in total productivity due to year-round warmth and moisture.
Desert and semidesert scrub: around $90$ g m^{-2} yr^{-1}$ (low per-area productivity).
Tundra: around $140$ g m^{-2} yr^{-1}$ (low but not negligible in nutrient-poor conditions).
Note: values vary by source; the slide presents a comparative table with multiple biomes and involves both productivity and area metrics to illustrate global patterns.
Ecosystem disturbance and resilience
Disturbance: natural or human-induced event that interrupts ecological succession and creates new conditions on-site (e.g., volcanoes, fires, human activities).
Different ecosystems have different capacities to respond to disturbances (resilience).
Disturbances can kill or displace many community members and alter energy flow and nutrient cycling.
Resilience
Resilience: ability of a system to absorb, adapt to, or recover from disturbances while maintaining ecosystem services, structure, and biodiversity.
Mechanisms include:
1) Resistance: ability to withstand stress or disturbance without significant change (e.g., mature temperate forests with high biodiversity and complex structure).
2) Recovery: speed and extent to which an ecosystem returns to its pre-disturbance state and re-establishes equilibrium.
Succession
Ecological succession: transition from one biotic community to another after a disturbance.
Pioneer species: first colonizers of a newly opened area.
Facilitation: early species modify conditions to aid subsequent species, driving succession forward.
Succession is not infinite; a climax ecosystem is the final stage but can change with new species introductions or removals.
Adjoining ecosystems in the same environment can be at different successional stages.
Primary and secondary succession
Primary succession: occurs in areas lacking plants and soil (e.g., retreating glacier).
Secondary succession: occurs after a disturbance in areas with pre-existing soil (e.g., fire, floods, human clearing).
Process: recolonization by plants and animals from surrounding areas; starts with soil.
Aquatic succession
Lakes and ponds undergo aquatic succession: soil from land erodes and settles in water; lake gradually fills in; terrestrial species move in as the lake fills; aquatic species move toward the center and eventually the lake disappears.
Disturbance and resilience in ecosystems
All stages of succession are present in landscapes; disturbances create gaps or patches and biodiversity is enhanced by disturbance.
Natural succession can be blocked or modified if key species are eliminated.
Fire and succession
Fire is a major disturbance in many ecosystems.
Tolerance to fire varies by species:
Grasses and pines tolerate fire.
Broad-leaved trees are more damaged by fire.
Fires release nutrients from dead matter and some plants require fire to germinate (fire-adapted ecosystems).
Fire-climax ecosystems: ecosystems that depend on periodic fire to maintain their existence (e.g., certain grasslands and pine forests).
Resilience mechanisms and limits
Resilience mechanisms help restore ecosystem function after disturbance (energy flow and nutrient cycling).
Limits exist: a severely degraded ecosystem may not recover its original functions, leading to a new, less productive ecosystem.
Ecosystem capital and human welfare
Ecosystems provide valuable services to humans and other species (flood control, soil maintenance, CO₂ absorption, nutrient cycling).
Goods and services are not fully captured by markets; ecosystem capital underpins many economic and social systems.
Economic valuation of ecosystem services
Incremental value of services: economic value of how changes in quantity/quality of services affect human welfare.
Example: converting forest to palm plantations may yield short-term revenue ($1,000–$2,000 per hectare per year) but incur larger losses in ecosystem services (~$5,000–$10,000 per hectare per year).
Estimates suggest roughly $44 trillion per year in ecosystem goods and services across major services, contributing to more than half of global GDP when aggregated across sectors.
Ecosystem restoration
There is capacity to restore ecosystems, though some sites require intensive restoration work.
Global demand for ecosystem goods and services (e.g., agriculture, infrastructure) creates pressure to convert ecosystems.
Alternatives can be pursued when:
Society recognizes how essential ecosystems are.
Ecosystem sustainability is promoted.
Alternatives are economically viable.
Managing ecosystems
Effective ecosystem management relies on understanding:
How ecosystems function.
How they respond to disturbances.
What goods and services they provide.
U.S. agencies involved in ecosystem management include:
Forest Service
Department of Wildlife and Fisheries
National Park Service
Environmental Protection Agency (EPA)
National Oceanic and Atmospheric Administration (NOAA)
Equations and key quantitative references (LaTeX)
Primary production uses only a small fraction of available solar energy:
\text{Primary production} \approx 0.02 \times (\text{total solar energy input})Energy yield from primary production (example):
120\ \text{gigatons of organic matter per year}Biomass ratio across trophic levels (typical approximate rule of thumb):
\text{Producer biomass} : \text{First-level consumer biomass} : \text{Second-level consumer biomass} : \text{Third-level consumer biomass} \approx 100 : 10 : 1 : 0.1Energy fate: energy costs and tissue formation ranges:
Energy used for metabolism, growth, and maintenance typically: 60\% \le E_{metabolism} \le 90\% of ingested energy.
Energy converted to tissue: 10\% \le E_{tissue} \le 40\% of ingested energy.
Energy transfer efficiency between trophic levels is low; a common conceptual statement is that only a small percentage is transferred to the next level (no single universal percentage, but the 1/10 rule is often cited in teaching).
Ecosystem services valuation: a large-scale estimate cited is approximately 44\times 10^{12}\$ (\$44 trillion)\per\year in ecosystem goods and services contributing to human welfare; this reflects global significance beyond market transactions.
// End of notes on Chapter 5: From Ecosystems to Biomes