Ecosystem

Components, productivity, energy flow, nutrient cycles.

Food chains and webs

Trophic levels, ecological pyramids.

Ecosystem — components, food chains, energy flow, nutrient cycles
Notes

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.

Ecosystem — components, food chains, energy flow, nutrient cycles
Notes

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.

Ecosystem — components, food chains, energy flow, nutrient cycles
Notes

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.