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Ecology and sustainability · Ecosystem dynamics

Matter cycles

The carbon in your breath today may once, millions of years ago, have been part of a dinosaur, or of a fern in a swamp that is now a Texas oil field. Unlike energy, which is dissipated as heat and does not come back, the atoms of matter are not destroyed: they pass from living things to the atmosphere, the water or the rocks, and return again and again. These journeys are called biogeochemical cycles.

Reservoirs, fluxes and types of cycle

A mature forest in the Pacific Northwest stores tons of carbon in its trunks, but when the wood burns or decomposes, that mass disappears from view even though the atoms have not been destroyed. Where is the planet's matter stored, and by what mechanisms does it travel from one place to another?

Landscape with atmosphere, forest, soil, ocean and rocks: blue arrows show the gaseous flow of carbon and nitrogen through the atmosphere and green arrows show the sedimentary flow of phosphorus through soil, water and sediments. living things atmosphere N₂ CO₂ gaseous · C, N soil flux ocean rocks and sediments sedimentary · P zones: reservoirs · arrows: fluxes
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Explain the difference between a gaseous and a sedimentary biogeochemical cycle, and classify the carbon, nitrogen, and phosphorus cycles into one of the two types,…

Explain the difference between a gaseous and a sedimentary biogeochemical cycle, and classify the carbon, nitrogen, and phosphorus cycles into one of the two types, justifying your choice.

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Define reservoir and flow in a biogeochemical cycle, and identify a specific reservoir and a specific flow in the carbon cycle, explaining which process maintains that…

Define reservoir and flow in a biogeochemical cycle, and identify a specific reservoir and a specific flow in the carbon cycle, explaining which process maintains that flow.

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The carbon cycle

Diagram of the carbon cycle: producers take CO₂ from the atmosphere by photosynthesis and return it by respiration; the carbon passes to consumers through feeding and, from both, to the soil and the decomposers. atmosphere (CO₂) producers consumers soil and decomposers photosynthesis respiration feeding

Decomposition, the ocean, and methane

Decomposition is the breakdown of dead organic matter by decomposers (bacteria and fungi) and detritivores (earthworms, millipedes). They release $\text{CO}_2$ by respiration and return ammonium and phosphate to the soil. Without them, nutrients would stay locked in dead material and producers would run out of raw materials.

Phytoplankton carry out photosynthesis in the surface ocean. $\text{CO}_2$ also dissolves directly in seawater, so the oceans act as a sponge for atmospheric $\text{CO}_2$. Some carbon sinks as dead organisms and ends up in sediments.

Methane ($\text{CH}_4$) is made by methanogens, archaea that live without oxygen (in the stomachs of cattle, in wetlands, in landfills). It is part of the carbon cycle. Per molecule, $\text{CH}_4$ traps far more heat than $\text{CO}_2$ (a much higher global warming potential), so a small amount matters.

Reading a carbon cycle diagram

In exam diagrams, arrows are often marked with letters or a question mark. Identify the reservoirs at each end of the arrow, then decide which process moves carbon between them.

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Write the overall chemical equations for photosynthesis and aerobic cellular respiration, and explain the role both processes play, in opposite directions, within the…

Write the overall chemical equations for photosynthesis and aerobic cellular respiration, and explain the role both processes play, in opposite directions, within the carbon cycle.

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Explain what the decomposition of organic matter is, which groups of organisms carry it out, and why the cycles of matter would come to a halt without them even if…

Explain what the decomposition of organic matter is, which groups of organisms carry it out, and why the cycles of matter would come to a halt without them even if producers were still present.

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Explain the role phytoplankton plays in the oceanic carbon cycle and why the oceans are said to act as a sponge for atmospheric $\text{CO}2$.

Explain the role phytoplankton plays in the oceanic carbon cycle and why the oceans are said to act as a sponge for atmospheric $\text{CO}_2$.

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Gasoline combustion and cellular respiration both release $\text{CO}2$. Explain what the two processes have in common chemically, how they differ, and why only one of…

Gasoline combustion and cellular respiration both release $\text{CO}_2$. Explain what the two processes have in common chemically, how they differ, and why only one of them has been part of the natural carbon cycle for millions of years.

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The diagram represents the main reservoirs and fluxes of the carbon cycle. Name the processes marked with the letters a, b, and c, indicate which process corresponds to…

The diagram represents the main reservoirs and fluxes of the carbon cycle. Name the processes marked with the letters a, b, and c, indicate which process corresponds to the arrow marked with '?', and explain how this flux alters the balance of the cycle.

ATMOSPHERE (CO₂) PRODUCERS CONSUMERS SOIL AND DECOMPOSERS FOSSIL FUELS a b c ?
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Describe the possible journey of a carbon atom from being part of atmospheric $\text{CO}2$ to becoming incorporated into a muscle in your body and then returning to the…

Describe the possible journey of a carbon atom from being part of atmospheric $\text{CO}_2$ to becoming incorporated into a muscle in your body and then returning to the atmosphere, naming the biological process behind each step (photosynthesis, feeding, respiration...).

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A mature forest fixes $10\ \text{t}$ of $\text{CO}2$ per hectare per year, but its trees and decomposers release $9.5\ \text{t}$ through respiration over the same…

A mature forest fixes $10\ \text{t}$ of $\text{CO}_2$ per hectare per year, but its trees and decomposers release $9.5\ \text{t}$ through respiration over the same period. Calculate the forest's net annual carbon sequestration and explain why a young, growing forest sequesters much more than a mature one even though it fixes less $\text{CO}_2$ in total.

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Explain how the deforestation of a tropical basin disrupts both the carbon cycle and the water cycle at the same time: what happens to the carbon stored in the biomass,…

Explain how the deforestation of a tropical basin disrupts both the carbon cycle and the water cycle at the same time: what happens to the carbon stored in the biomass, to evapotranspiration, to the region's rainfall and to runoff.

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Cattle emit methane ($\text{CH}4$) during digestion. Explain which anaerobic process produces it, which cycle of matter it belongs to, and why its emission is a concern…

Cattle emit methane ($\text{CH}_4$) during digestion. Explain which anaerobic process produces it, which cycle of matter it belongs to, and why its emission is a concern even though it is much smaller in quantity than that of $\text{CO}_2$ (compare their global warming potentials).

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A science skeptic posts the following message: "The atmosphere contains about $850\text{ Gt}$ of carbon and the oceans more than $38\,000\text{ Gt}$. Our annual…

A science skeptic posts the following message: "The atmosphere contains about $850\text{ Gt}$ of carbon and the oceans more than $38\,000\text{ Gt}$. Our annual emissions from burning fossil fuels are barely around $10\text{ Gt}$. Since the planet's total carbon is constant and anthropogenic emissions are less than $0.03\,\%$ of the marine reservoir, it is absurd to claim that we can alter the global carbon cycle."

  1. a) Refute their argument by distinguishing between the dynamics of the biological (fast) cycle and the geological (slow) cycle: use the concepts of flux, residence time, and dynamic equilibrium to justify why $10\text{ Gt/year}$ destabilizes the global climate.
  2. b) If natural sinks (biosphere and ocean surface) absorb on average $45\,\%$ of the anthropogenic carbon emitted each year, calculate how many ppm of $\text{CO}_2$ accumulate annually in the atmosphere, knowing that $1\text{ ppm} \approx 2.13\text{ Gt}$ of atmospheric carbon.
  3. c) Predict what will happen to the ocean's capacity to continue acting as a chemical sink for $\text{CO}_2$ as surface water temperature increases and its pH decreases, justifying through the chemical equilibrium of carbonic acid and carbonates.
Solve

The nitrogen cycle

Although the air you breathe contains $78\%$ nitrogen and plants are immersed in it, many Iowa corn fields turn yellow and stop growing if fertilizer is not added to the soil. Why does an element that is so abundant in the atmosphere turn out to be unavailable to plants, and how do they manage to take it in?

Diagram of the nitrogen cycle: N₂ from the air becomes ammonium by fixation, nitrate by nitrification and organic matter by uptake; organic matter returns ammonium by ammonification and nitrate returns to the air as N₂ by denitrification. N₂ (air) ammonium NH₄⁺ nitrate NO₃⁻ organic matter fixation nitrification uptake denitrification ammonification
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Describe the role of nitrogen-fixing bacteria and nitrifying bacteria, indicating which chemical transformation each group performs and why they are essential for plant…

Describe the role of nitrogen-fixing bacteria and nitrifying bacteria, indicating which chemical transformation each group performs and why they are essential for plant nutrition.

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Name the main chemical forms nitrogen adopts throughout its cycle (atmospheric $\text{N}2$, ammonium, nitrite, nitrate and organic matter) and explain why most plants…

Name the main chemical forms nitrogen adopts throughout its cycle (atmospheric $\text{N}_2$, ammonium, nitrite, nitrate and organic matter) and explain why most plants cannot directly use the $\text{N}_2$ in the air.

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Order the following stages of the nitrogen cycle as they occur in an ecosystem and briefly describe what each consists of: nitrification, fixation, denitrification, and…

Order the following stages of the nitrogen cycle as they occur in an ecosystem and briefly describe what each consists of: nitrification, fixation, denitrification, and ammonification.

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The roots of legumes host nodules containing bacteria of the genus Rhizobium. Explain what the plant and the bacterium exchange in this symbiosis, which process of the…

The roots of legumes host nodules containing bacteria of the genus Rhizobium. Explain what the plant and the bacterium exchange in this symbiosis, which process of the nitrogen cycle the bacterium performs, and what agricultural advantage there is in including legumes in crop rotation.

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The phosphorus cycle and other sedimentary cycles

Diagram of the sedimentary phosphorus cycle showing the slow weathering of phosphate rocks and their transport to the soil and bodies of water without passing through the atmosphere. phosphate rock erosion very slow soil rivers/sea no passage through the atmosphere
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Phosphorus is often the limiting nutrient in terrestrial ecosystems. Explain what it means for a nutrient to be "limiting," why the phosphorus cycle is so slow, and what…

Phosphorus is often the limiting nutrient in terrestrial ecosystems. Explain what it means for a nutrient to be "limiting," why the phosphorus cycle is so slow, and what consequence its lack of a gaseous phase has.

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Eutrophication: when the cycles become unbalanced

After the neighboring fields have been heavily fertilized, a pond of clear water becomes covered within a few days by a dense, opaque green layer, and soon afterwards dead fish appear floating at the edge. How can a massive input of nutrients, which stimulates the primary producers, end up wiping out the aquatic fauna?

Cross-section of a eutrophic lagoon: at the top, fertilizer from a field reaches the water and algae cover the surface and block the light; at the bottom, the algae die and sink, the decomposers use up the oxygen at the bottom and the fish die. 1 Excess N and P no light O₂ 2 Algal bloom days later O₂ O₂ decomposers 3 Algae die 4 Anoxia → mortality

This is the same process behind the Gulf of Mexico "dead zone," fed by fertilizer runoff down the Mississippi River, and the algal blooms in the Chesapeake Bay.

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An environmental monitoring team studies a coastal lagoon after an agricultural runoff discharge and records the following data: Day 5: Surface reactive phosphorus…

An environmental monitoring team studies a coastal lagoon after an agricultural runoff discharge and records the following data:

  • Day 5: Surface reactive phosphorus concentration of $0.8\text{ mg/L}$ and chlorophyll $a$ of $65\ \mu\text{g/L}$; dissolved $\text{O}_2$ saturation of $145\,\%$ at noon in the top $40\text{ cm}$ of depth.

  • Day 20: Surface $\text{O}_2$ saturation of $35\,\%$ at dawn; extreme turbidity ($40\text{ NTU}$); dissolved $\text{O}_2$ at the bottom ($3\text{ m}$) at $0.3\text{ mg/L}$, with the release of hydrogen sulfide ($\text{H}_2\text{S}$) and benthic fauna die-off.

A city technician states: "It is impossible for fish to die of asphyxiation if algae produce plenty of oxygen through photosynthesis; the cause must be direct chemical toxicity from nitrate."

  1. a) Refute the technician's claim using biogeochemical arguments: justify why a massive autotrophic bloom inevitably leads to hypolimnetic and nocturnal anoxia.
  2. b) Explain which trophic group proliferates from day 15 onwards and which anaerobic metabolic pathways account for the presence of $\text{H}_2\text{S}$ at the bottom.
  3. c) Predict what immediate ecological consequences treating the lagoon with a chemical algaecide to eradicate phytoplankton would have on the matter cycle.
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The sulfur cycle

Sulfur is part of amino acids such as cysteine and methionine. Plants take up sulfate from the soil and the sulfur passes to consumers through feeding; decomposition returns it to the environment. Microorganisms transform reduced and oxidized compounds: in anoxic environments sulfide can be produced, and oxidizing bacteria convert it into sulfate.

Sulfur cycle: sulfate in the soil passes to plants and animals and returns through decomposition; volcanoes and combustion emit sulfur gases that are deposited with the rain; rocks and sulfide-oxidizing bacteria supply sulfate. sulfur gases deposition volcano combustion producer consumer decomposers sulfate rocks and sediments sulfide anoxic environment oxidizing bacteria

Back to the beginning: The carbon atom you breathe out today could have belonged to a dinosaur because, after the reptile died and decomposed, that carbon passed into the atmosphere as $\text{CO}_2$ or was trapped in sedimentary rocks; millions of years later, a plant fixed it again by photosynthesis and it reached you through the food chain.

Summary

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