Ecosystem
Components, productivity, energy flow, nutrient cycles.
Food chains and webs
Trophic levels, ecological pyramids.
An ecosystem is a community of organisms interacting with each other and with their physical environment.
Components:
Abiotic (non-living):
- Climatic: light, temperature, water, wind.
- Edaphic: soil pH, mineral nutrients.
Biotic (living):
- Producers (autotrophs): plants, algae, cyanobacteria. Fix energy from sunlight (photosynthesis) or chemicals (chemosynthesis).
- Consumers (heterotrophs):
- Primary (herbivores): cow, grasshopper.
- Secondary (carnivores feeding on herbivores): frog.
- Tertiary (top carnivores): tiger, eagle.
- Decomposers / detritivores: bacteria, fungi, earthworms. Break down dead organic matter, recycling nutrients.
FOOD CHAINS
Linear sequence of organisms where each is eaten by the next. Energy flows in one direction (sunlight → producers → consumers → decomposers).
Two types:
1. Grazing food chain (GFC). Starts with living plants.
Example: grass → grasshopper → frog → snake → eagle.
2. Detritus food chain (DFC). Starts with dead organic matter.
Example: dead leaves → fungi → earthworm → bird.
Food web: interconnected food chains. Real ecosystems are webs, not chains.
TROPHIC LEVELS
Each step in a food chain.
- T1: producers
- T2: primary consumers
- T3: secondary consumers
- T4: tertiary consumers
- T5: quaternary consumers (rare — energy too low)
10% rule (Lindeman): only ~10% of energy at one trophic level passes to the next. The rest is lost as heat (respiration), waste, or in undigested form.
This is why:
- Food chains rarely have more than 4-5 trophic levels.
- Top carnivores are few in number (energy bottleneck).
- A vegetarian diet is more "efficient" — eat closer to producers.
ECOLOGICAL PYRAMIDS
Graphical representation of trophic levels.
Pyramid of numbers:
- Usually upright (lots of grass, fewer cows, fewer humans).
- Inverted in tree ecosystems (one tree feeds many insects).
Pyramid of biomass:
- Usually upright (mass of producers > consumers).
- Inverted in aquatic ecosystems (low biomass of phytoplankton at any moment, but high turnover supports many zooplankton).
Pyramid of energy: ALWAYS upright. Energy decreases at each level due to the 10% rule.
ECOSYSTEM PRODUCTIVITY
GPP (Gross Primary Productivity): total organic matter produced by photosynthesis per unit area per unit time.
NPP (Net Primary Productivity): GPP minus respiration loss by plants. This is what's available to consumers.
Earth's annual NPP: ~170 billion tonnes (dry weight). Oceans contribute ~55 billion despite covering 70% of surface — surprisingly low because phytoplankton turnover is fast.
NUTRIENT CYCLES (biogeochemical cycles)
Unlike energy, matter (nutrients) is recycled.
Carbon cycle:
- Atmospheric CO₂ → photosynthesis → organic carbon in producers → consumers/respiration → CO₂ back.
- Long-term: fossil fuels, sedimentary rocks, oceans.
- Anthropogenic disturbance: burning fossil fuels released ancient carbon → climate change.
Nitrogen cycle:
- N₂ in atmosphere (~78%) is unusable by most organisms.
- Nitrogen fixation by Rhizobium (legume nodules), Azotobacter (free-living), cyanobacteria (Anabaena, Nostoc), lightning.
- N₂ → NH₃ → NH₄⁺ (ammonification by decomposers).
- Nitrification: NH₃ → NO₂⁻ (by Nitrosomonas) → NO₃⁻ (by Nitrobacter).
- Plants absorb NO₃⁻; build amino acids/proteins.
- Denitrification: NO₃⁻ → N₂ by Pseudomonas. Returns to atmosphere.
Phosphorus cycle: sedimentary (no atmospheric phase). Phosphate rock → weathering → soil/water → plants → animals → decomposition → soil.
Water cycle: evaporation, condensation, precipitation, runoff, infiltration.
ECOLOGICAL SUCCESSION
Predictable progression of communities over time at a site.
- Primary succession: starts from bare rock or fresh substrate (e.g., after a volcano). First colonizers: lichens.
- Secondary succession: after a disturbance (fire, agriculture abandonment). Faster than primary because soil is intact.
Stages: pioneer → seral communities → climax community (stable, in equilibrium with climate).
Hydrarch succession: in water → ends in forest. Xerarch: in dry/rocky area → ends in forest.
Energy flow and productivity
10% rule, GPP, NPP, secondary productivity.
An ecosystem is a community of organisms interacting with each other and with their physical environment.
Components:
Abiotic (non-living):
- Climatic: light, temperature, water, wind.
- Edaphic: soil pH, mineral nutrients.
Biotic (living):
- Producers (autotrophs): plants, algae, cyanobacteria. Fix energy from sunlight (photosynthesis) or chemicals (chemosynthesis).
- Consumers (heterotrophs):
- Primary (herbivores): cow, grasshopper.
- Secondary (carnivores feeding on herbivores): frog.
- Tertiary (top carnivores): tiger, eagle.
- Decomposers / detritivores: bacteria, fungi, earthworms. Break down dead organic matter, recycling nutrients.
FOOD CHAINS
Linear sequence of organisms where each is eaten by the next. Energy flows in one direction (sunlight → producers → consumers → decomposers).
Two types:
1. Grazing food chain (GFC). Starts with living plants.
Example: grass → grasshopper → frog → snake → eagle.
2. Detritus food chain (DFC). Starts with dead organic matter.
Example: dead leaves → fungi → earthworm → bird.
Food web: interconnected food chains. Real ecosystems are webs, not chains.
TROPHIC LEVELS
Each step in a food chain.
- T1: producers
- T2: primary consumers
- T3: secondary consumers
- T4: tertiary consumers
- T5: quaternary consumers (rare — energy too low)
10% rule (Lindeman): only ~10% of energy at one trophic level passes to the next. The rest is lost as heat (respiration), waste, or in undigested form.
This is why:
- Food chains rarely have more than 4-5 trophic levels.
- Top carnivores are few in number (energy bottleneck).
- A vegetarian diet is more "efficient" — eat closer to producers.
ECOLOGICAL PYRAMIDS
Graphical representation of trophic levels.
Pyramid of numbers:
- Usually upright (lots of grass, fewer cows, fewer humans).
- Inverted in tree ecosystems (one tree feeds many insects).
Pyramid of biomass:
- Usually upright (mass of producers > consumers).
- Inverted in aquatic ecosystems (low biomass of phytoplankton at any moment, but high turnover supports many zooplankton).
Pyramid of energy: ALWAYS upright. Energy decreases at each level due to the 10% rule.
ECOSYSTEM PRODUCTIVITY
GPP (Gross Primary Productivity): total organic matter produced by photosynthesis per unit area per unit time.
NPP (Net Primary Productivity): GPP minus respiration loss by plants. This is what's available to consumers.
Earth's annual NPP: ~170 billion tonnes (dry weight). Oceans contribute ~55 billion despite covering 70% of surface — surprisingly low because phytoplankton turnover is fast.
NUTRIENT CYCLES (biogeochemical cycles)
Unlike energy, matter (nutrients) is recycled.
Carbon cycle:
- Atmospheric CO₂ → photosynthesis → organic carbon in producers → consumers/respiration → CO₂ back.
- Long-term: fossil fuels, sedimentary rocks, oceans.
- Anthropogenic disturbance: burning fossil fuels released ancient carbon → climate change.
Nitrogen cycle:
- N₂ in atmosphere (~78%) is unusable by most organisms.
- Nitrogen fixation by Rhizobium (legume nodules), Azotobacter (free-living), cyanobacteria (Anabaena, Nostoc), lightning.
- N₂ → NH₃ → NH₄⁺ (ammonification by decomposers).
- Nitrification: NH₃ → NO₂⁻ (by Nitrosomonas) → NO₃⁻ (by Nitrobacter).
- Plants absorb NO₃⁻; build amino acids/proteins.
- Denitrification: NO₃⁻ → N₂ by Pseudomonas. Returns to atmosphere.
Phosphorus cycle: sedimentary (no atmospheric phase). Phosphate rock → weathering → soil/water → plants → animals → decomposition → soil.
Water cycle: evaporation, condensation, precipitation, runoff, infiltration.
ECOLOGICAL SUCCESSION
Predictable progression of communities over time at a site.
- Primary succession: starts from bare rock or fresh substrate (e.g., after a volcano). First colonizers: lichens.
- Secondary succession: after a disturbance (fire, agriculture abandonment). Faster than primary because soil is intact.
Stages: pioneer → seral communities → climax community (stable, in equilibrium with climate).
Hydrarch succession: in water → ends in forest. Xerarch: in dry/rocky area → ends in forest.
Biogeochemical cycles
Carbon, nitrogen, phosphorus, water cycles.
An ecosystem is a community of organisms interacting with each other and with their physical environment.
Components:
Abiotic (non-living):
- Climatic: light, temperature, water, wind.
- Edaphic: soil pH, mineral nutrients.
Biotic (living):
- Producers (autotrophs): plants, algae, cyanobacteria. Fix energy from sunlight (photosynthesis) or chemicals (chemosynthesis).
- Consumers (heterotrophs):
- Primary (herbivores): cow, grasshopper.
- Secondary (carnivores feeding on herbivores): frog.
- Tertiary (top carnivores): tiger, eagle.
- Decomposers / detritivores: bacteria, fungi, earthworms. Break down dead organic matter, recycling nutrients.
FOOD CHAINS
Linear sequence of organisms where each is eaten by the next. Energy flows in one direction (sunlight → producers → consumers → decomposers).
Two types:
1. Grazing food chain (GFC). Starts with living plants.
Example: grass → grasshopper → frog → snake → eagle.
2. Detritus food chain (DFC). Starts with dead organic matter.
Example: dead leaves → fungi → earthworm → bird.
Food web: interconnected food chains. Real ecosystems are webs, not chains.
TROPHIC LEVELS
Each step in a food chain.
- T1: producers
- T2: primary consumers
- T3: secondary consumers
- T4: tertiary consumers
- T5: quaternary consumers (rare — energy too low)
10% rule (Lindeman): only ~10% of energy at one trophic level passes to the next. The rest is lost as heat (respiration), waste, or in undigested form.
This is why:
- Food chains rarely have more than 4-5 trophic levels.
- Top carnivores are few in number (energy bottleneck).
- A vegetarian diet is more "efficient" — eat closer to producers.
ECOLOGICAL PYRAMIDS
Graphical representation of trophic levels.
Pyramid of numbers:
- Usually upright (lots of grass, fewer cows, fewer humans).
- Inverted in tree ecosystems (one tree feeds many insects).
Pyramid of biomass:
- Usually upright (mass of producers > consumers).
- Inverted in aquatic ecosystems (low biomass of phytoplankton at any moment, but high turnover supports many zooplankton).
Pyramid of energy: ALWAYS upright. Energy decreases at each level due to the 10% rule.
ECOSYSTEM PRODUCTIVITY
GPP (Gross Primary Productivity): total organic matter produced by photosynthesis per unit area per unit time.
NPP (Net Primary Productivity): GPP minus respiration loss by plants. This is what's available to consumers.
Earth's annual NPP: ~170 billion tonnes (dry weight). Oceans contribute ~55 billion despite covering 70% of surface — surprisingly low because phytoplankton turnover is fast.
NUTRIENT CYCLES (biogeochemical cycles)
Unlike energy, matter (nutrients) is recycled.
Carbon cycle:
- Atmospheric CO₂ → photosynthesis → organic carbon in producers → consumers/respiration → CO₂ back.
- Long-term: fossil fuels, sedimentary rocks, oceans.
- Anthropogenic disturbance: burning fossil fuels released ancient carbon → climate change.
Nitrogen cycle:
- N₂ in atmosphere (~78%) is unusable by most organisms.
- Nitrogen fixation by Rhizobium (legume nodules), Azotobacter (free-living), cyanobacteria (Anabaena, Nostoc), lightning.
- N₂ → NH₃ → NH₄⁺ (ammonification by decomposers).
- Nitrification: NH₃ → NO₂⁻ (by Nitrosomonas) → NO₃⁻ (by Nitrobacter).
- Plants absorb NO₃⁻; build amino acids/proteins.
- Denitrification: NO₃⁻ → N₂ by Pseudomonas. Returns to atmosphere.
Phosphorus cycle: sedimentary (no atmospheric phase). Phosphate rock → weathering → soil/water → plants → animals → decomposition → soil.
Water cycle: evaporation, condensation, precipitation, runoff, infiltration.
ECOLOGICAL SUCCESSION
Predictable progression of communities over time at a site.
- Primary succession: starts from bare rock or fresh substrate (e.g., after a volcano). First colonizers: lichens.
- Secondary succession: after a disturbance (fire, agriculture abandonment). Faster than primary because soil is intact.
Stages: pioneer → seral communities → climax community (stable, in equilibrium with climate).
Hydrarch succession: in water → ends in forest. Xerarch: in dry/rocky area → ends in forest.