1.2.6 Biogeochemical cycles
Helpful prior knowledge and learning objectives:
Helpful prior learning:
Section 1.1.1 The economy and you, which explains what an economy is and how it is relevant to students’ lives
Section 1.1.2 The embedded economy, which explains the relationship between the economy and society and Earth’s systems.
Section 1.1.3 Degenerative economies, which explain the problems for people and planet with the way our current economies operate.
Section 1.1.4 Regenerative economies, which explain the characteristics of economies that support and regenerate all life on Earth.
Section 1.2.2 Energy basics, which explains different forms and sources of energy.
Section 1.2.3 Impact of the fossil fuel energy pulse, which explains the role of fossil fuels in accelerating economic and population growth
Section 1.2.4 Matter in the economy, which explains the role of material extraction in our economies and the impact of that extraction and waste on ecosystems.
Section 1.2.5 Ecosystems: interactions, energy and stability, which explains the basic functions and interactions in ecosystems and the factors affecting ecosystem stability
Section S.1 Systems thinking, which explains what a system is and why systems thinking is useful. (coming soon)
Section S.x Stocks and flows, which explains a type of system with accumulations of energy, matter, information and other things that increase or decrease over time through inflows and outflows. (coming soon)
Section S.x Feedback loops and tipping points, which explains the roles of reinforcing and balancing feedback loops in amplifying or dampening change. (coming soon)
Learning objectives:
explain the roles of biogeochemical cycles (focusing mainly on water and carbon) in ecosystem function
explain how human economic activities disrupt biogeochemical cycles
Figure 1. The Whanganui River in New Zealand, the first river to be granted legal personhood (Activity at the end refers to this)
(Credit: James Shook CC BY 2.5)
The water in your body is just visiting.
It was a thunderstorm a week ago.
It will be the ocean soon enough.
Most of your cells come and go like morning dew.
We are more weather pattern than stone monument.
Sunlight on mist. Summer lightning.
Your choices outweigh your substance.
-- “Naming the River” from Field Guide to the Haunted Forest
by ©Jarod K. Anderson, with permission
Jarod Anderson’s poem beautifully highlights the connection between humans and nature. Like all living things, our bodies are about 70% water, which comes from and returns to our ecosystems, through vital biogeochemical cycles.
What are biogeochemical cycles?
Biogeochemical cycles move essential elements between abiotic (nonliving) and biotic (living) parts of ecosystems. Elements like water, carbon, oxygen, nitrogen and phosphorus cycle through the air, land, water, and organisms, link all Earth systems. However, human activities often disrupt these cycles, risking collapse of the Earth systems on which we depend.
This section explores the water and carbon cycles, showing their importance to Earth's life-support systems.
How does the water cycle work?
The water cycle, or hydrosphere, is the stocks and flows of all water on Earth. Stocks, or storages, of water include oceans, glaciers and ice caps, groundwater, surface water, the atmosphere and living organisms. Figure 2 shows that the salty oceans hold most water (97.2%), while a tiny fraction of freshwater exists mainly as ice in glaciers and ice sheets.
Water moves between stocks, driven by solar radiation and gravity. Water is transferred from one place to another, or it is transformed into different states.
Figure 2 shows these movements between water stocks.
Figure 3. The water cycle
(Credit: NASA)
evaporation, transpiration, and sublimation: water from oceans, rivers, lakes, soils, all living organisms, and glaciers and ice sheets is warmed by solar radiation, and rises into the atmosphere as water vapour
condensation: water vapour cools in the atmosphere forming water droplets and clouds
precipitation: when water droplets fall back to Earth as rain, snow, or hail
infiltration: some water flows into soils, collecting as groundwater
runoff: some water flows over land and collects into lakes, rivers, and oceans, and the cycle repeats.
Why is the water cycle important for life on Earth?
The water cycle is crucial for ecosystem function. It stabilises Earth's temperature, cooling areas through evaporation, transpiration and sublimation. Glaciers and ice sheets also reflect warming solar radiation back into the atmosphere. Oceans absorb carbon dioxide (CO2) from the atmosphere, reducing global warming. Ocean currents distribute heat globally. In addition to regulating temperature, the water cycle also distributes matter like nutrients vital for life and also supplies fresh water for organisms' survival.
How does human economic activity disrupt the water cycle?
Human economic activities disrupt the water cycle, including:
overextraction of water: we use too much surface water and groundwater for farming, industry and domestic use. The average T-shirt needs 2,700 litres of water to produce! Agriculture uses 70% of all freshwater withdrawals globally. This leaves less water available in parts of the water cycle for the ecosystems that rely on it. You can see this in the drying of the Aral Sea (Figure 4), once the world’s fourth largest lake due to diversion of river inflows for agriculture.
pollution: factories, farms, and homes pollute waterways with chemicals and organic waste. Pollution can hinder evaporation and poison organisms that rely on water from contaminated sources.
deforestation: humans cut down forests for farming, mining, and expanding the built environment. Removing trees reduces transpiration, with less water to condense into clouds and less precipitation. Deforestation in the Amazon Rainforest causes drought in the region, further harming the forest in a reinforcing feedback loop (Section S.x).
burning fossil fuels causing climate change: humans burn fossil fuels for energy to power the economy (Section 1.2.2). This warms the planet, which changes how much rain falls, where it falls, and how often. Heavier storms cause flooding and damage waterways, preventing water from infiltrating soils and reducing long-term groundwater storage needed by plants and humans. Droughts worsen the situation. Too much water evaporates from soils, making it harder for soil to absorb water when it rains. Climate change also melts glaciers and ice caps. This raises sea levels and changes heat-distributing ocean currents, and it reduces glacier ice storages and the summer ice melt that feeds rivers and streams that ecosystems and humans depend on in drier months.
Human disruptions to the water cycle damage the ecosystems on which we depend, and are depleting water stocks for human agricultural systems. Protecting and supporting the water cycle is critical to all life on Earth.
How does the carbon cycle work?
Carbon is an element found in all life forms, making up nearly 50% of organisms’ dry biomass. The carbon cycle is how carbon moves between Earth's atmosphere, hydrosphere, biosphere, and lithosphere. Carbon stocks include the atmosphere, oceans, living organisms, rocks and soil. Carbon is transferred and transformed between these stocks, shown in Figure 5.
photosynthesis: plants transform carbon dioxide and water into glucose and oxygen producing their own food, moving carbon from the atmosphere to plants (Section 1.2.5);
cellular respiration: living organisms transform glucose and oxygen into carbon dioxide and water, moving carbon from living things to the atmosphere;
feeding/consumption: animals eat plants, and animals eat other animals, transferring carbon along a food chain or in a food web (Section 1.2.5);
decomposition: microorganisms and other decomposers like beetles and millipedes transform dead plants and animals and animal faeces, moving carbon into soils or the sea bed, and releasing carbon dioxide into the atmosphere as they respire;
Figure 5. The carbon cycle
(Credit: Met Office)
oceanic gas exchange: carbon dioxide from the atmosphere dissolves in ocean water and is released back into the atmosphere;
fossilisation and sedimentation: under high pressure, high temperature and over long periods of time, decaying organic matter can transform into fossil fuels (coal, oil, natural gas);
extraction: humans transfer coal, oil, and natural gas stocks to energy production facilities such as refineries, power plants, and car engines (Section 1.2.4);
combustion: humans burn coal, oil, and natural gas, releasing carbon dioxide to the atmosphere (Section 1.2.2).
Why is the carbon cycle important for life on Earth?
The carbon cycle moves carbon from the atmosphere, hydrosphere and lithosphere to living organisms in the biosphere, which is essential for life and climate regulation. Carbon dioxide, a greenhouse gas, warms Earth which supports life. However, excessive carbon dioxide in the atmosphere causes overheating and acidifies oceans, both of which threaten life. Balanced carbon levels in Earth’s various stocks are crucial to functioning ecosystems on which humans depend.
How does human economic activity disrupt the carbon cycle?
Human economic activities significantly alter the carbon cycle:
combustion of fossil fuels: fossil fuels form over millions of years in the lithosphere. When humans burn coal, oil, and gas for energy (Section 1.2.3), we release carbon dioxide into the atmosphere, enhancing the greenhouse effect rapidly warming the planet.
land use for urbanisation and agriculture: deforestation to clear land for farming, mining, and expanding the built environment for urbanisation reduces the trees and other plants that sequester carbon dioxide from the atmosphere in biomass and soils;
soil disruption and livestock rearing for agriculture: ploughing fields can release carbon stored in the soil. Livestock produce methane, another greenhouse gas.
These activities increase atmospheric carbon dioxide (Figure 6) beyond the levels that natural processes can remove. As a result, Earth’s average temperature is increasing, causing climate change, higher sea levels, ocean acidification, and altered habitats for plants and animals.
Figure 6: Annual CO2 emissions
(Credit: Our World in Data)
Human agriculture and civilizations developed around 10,000 years ago under stable climates with less than 1°C temperature variation, a period called the Holocene. Currently, global temperatures are almost 1.5°C warmer than the pre-Industrial time period because burning fossil fuels has increased concentrations of carbon dioxide in the atmosphere. The climate is changing so rapidly that it will likely be difficult for our societies and economies to adapt.
Our current economies disrupt the carbon cycle and destabilise the conditions for human life on Earth. To restore balance in the carbon cycle, we must dramatically reduce our CO2 emissions and regenerate ecosystems.
Activity 1.2.6
Concept: Systems
Skills: Thinking skills (creative and critical thinking, transfer)
Time: Depends on the option - see below
Type: Individuals, pairs or group - depends on the option
Option 1 - Creative thinking
40+ minutes
Imagine that you are a water molecule or a carbon atom. From that perspective, write a short poem (story, or some other format) that reflects your experience in some part of the water or carbon cycle, or that reflects how human activities have disrupted your movement in the water or carbon cycle.
Option 2 - Discussion: Does it make sense to distinguish between living and nonliving parts of nature?
20-25 minutes
E rere kau mai te Āwanui, Mai i te Kāhui maunga ki Tangaroa. Kō au te Āwa, kō te Āwa kō au.
“The great river flows from the mountains to the sea. I am the river, the river is me.”
--Ngāti Hau, the indigenous communities along the Whanganui River, New Zealand
Questions to think about / discuss in small groups or as a class:
Is the distinction between biotic (living) and abiotic (nonliving) parts of ecosystems appropriate? Given what you have learned about the water and carbon cycles, why might it be more appropriate to consider all elements of nature living, as reflected in the Maori worldview?
If we would consider all elements of nature to be living, how might that change the way human economies engage with and impact the natural world?
Option 3 - Legal personhood for nature
40-50 minutes
Some countries and regions are giving legal personhood to abiotic parts of nature, like rivers, to increase their protection under the law. Alone or with some partners, do some quick research on legal personhood to find answers to these questions or others that come up:
What is legal personhood and why is it important?
For whom is it typically used in economic law?
How are countries and regions using legal personhood to protect nature? Are there examples of nature being protected this way in your region?
What are the barriers to using legal personhood to protect nature?
Discuss what you found out with a few other students or as a whole class.
Option 4 - Annotating diagrams
The illustrations in this section show the water and carbon cycles. However, the human disruptions to these cycles are only described in words. Make those disruptions visible by adding them to the cycle diagrams. You may want to work alone to test your understanding, or work with a partner to support each other’s understanding.
Sketch one (or both) cycles on a piece of paper (boxes for stocks, arrows for flows) and then annotate further with the human disruptions by hand. You may want to use a pencil so that you can edit your diagrams as you go. OR
Copy and paste the relevant illustration(s) into a digital document and annotate it from there.
Ideas for longer activities, deeper engagement, and projects are listed in Subtopic 1.5 Taking action
Further exploration
The River is Me, a short (17 min) documentary about how the Whanganui River in New Zealand has been granted legal personhood, in keeping with the Maori worldview that the river is a living entity. Difficulty level: easy.
IPCC Sixth Assessment Report Fact Sheets - A set of brief and clear fact sheets for different regions of the world and different industries to help people understand the impact of climate change. Select your region, or an industry you find interesting or important to learn more about the impact of climate change. Difficulty level: medium
A series of lectures from the Institute for New Economic Thinking on the climate crisis:
The Scope of the Climate Crisis - [ECO]NOMICS Part 1 - In this video lecture, Professor Juliet Schor reviews how economists have approached the climate change problem, arguing that their views and methods have been central to our failure to address the crisis. Difficulty level: medium
Political Economy of Climate Disruption - [ECO]NOMICS Part 2 - In this video lecture, Professor Juliet Schor discusses the political economy approach to climate change, which links action and inaction to economic and political interests. Who benefits and who bears the costs of continuing the emit greenhouse gases? Difficulty level: medium
Sources
Anderson, J. (2020, November 27). “Naming the River”. Field Guide to the Haunted Forest. Amazon Digital Services.
Daly, H., Farley, J. (2011). Ecological Economics (2nd ed.). Washington, D.C.: Island Press.
Encyclopedia Britannica (2024, January 24). Māori. https://www.britannica.com/topic/Maori.
Freid, D. (Director). (2018). The River is Me [Film].
Met Office (n.d.). Carbon cycle. https://www.metoffice.gov.uk/weather/climate/climate-explained/carbon-cycle.
NASA (n.d.). Classroom Activity: Modelling the Water BudgetJet Propulsion Laboratory, California Institute of Technology. https://www.jpl.nasa.gov/edu/teach/activity/modeling-the-water-budget/.
Rutherford, J., Williams, G. (2015). Environmental Systems and Societies. Oxford: Oxford University Press.
Terminology
Link to Quizlet interactive flashcards and terminology games for Section 1.2.6 Biogeochemical cycles
ecosystem: the interaction of groups of organisms with each other and their physical environment
biogeochemical cycle: Earth system cycles that move essential elements like water, carbon and nitrogen between living and nonliving parts of ecosystems
abiotic: nonliving
biotic: living
water cycle: the stocks and flows of all water on Earth
hydrosphere: all the waters on Earth
stock: an accumulation of something, such as energy, matter, information, or money
flow: movement of something such as energy, matter, information or money between stocks
glacier: a mass of dense ice that constantly moves under its own weight, found in high altitudes and at the poles
groundwater: water that collects underground in soil or in rock crevices and pores
surface water: water that collects on the surface of the ground, like lakes and rivers; also known as blue water
atmosphere: the gases surrounding the Earth
freshwater: a water body with very low or no salt content
solar radiation: energy emitted by the sun
gravity: the force that attracts a body towards the centre of the earth, or towards any other physical body having mass
transfer: to move something from one place to another
transform: a change in the state, energy or chemical nature of something
evaporation: the transformation of a substance like water from a liquid into a gas
transpiration: the transformation of water from a plant's leaves, stem, or flowers to a gas
sublimation: transformation of a substance like water from a solid to a gas without first becoming a liquid
water vapour: the gaseous state of water
condensation: the transformation of water vapour into water droplets and clouds due to cooling in the atmosphere
precipitation: the transfer of water from clouds to the Earth as rain, snow or hail
infiltration: the transfer of water through soils, collecting as groundwater
runoff: the draining away (transfer) of water and the substances carried in it from the surface of land, or structure
carbon dioxide (CO2): gas produced by burning carbon or organic compounds and through respiration, naturally present in the atmosphere and absorbed by plants in photosynthesis
ocean currents: the predictable movement of ocean water in a direction
overextraction: taking too much of something away from somewhere else, especially using effort or force
pollution: the presence of a substance that has harmful effects on the environment
organic waste: any material that easily breaks down in nature and comes from either a plant or an animal
deforestation: removing a wide area of trees, often for farming, mining, or urbanisation
reinforcing feedback: a situation where change in a system causes further changes that amplify the original change which can lead to tipping points in a system
fossil fuel: a non renewable energy source including coal, oil, and natural gas, formed over millions of years in the Earth's crust from decomposed plants and animals
climate change: a change in the temperature and precipitation patterns in an area, in recent times due to human economic activities
economy: all the human-made systems that transfer and transform energy and matter to meet human needs and wants
biomass: organic matter
carbon cycle: the movement of carbon between Earth's atmosphere, hydrosphere, biosphere, and lithosphere
biosphere: all the living organisms on Earth
lithosphere: the solid, outer part of Earth
photosynthesis: the process by which green plants and some other organisms use sunlight to transform carbon dioxide and water into food
cellular respiration: the transformation of food (carbohydrates) into energy within cells
consumption: using resources and products to meet needs, or in food chains, eating another organism
decomposition: breaking something into smaller parts, especially organic materials
oceanic gas exchange: the process where gases like CO2 move between the atmosphere and the oceans
fossilisation: the process that occurs when plant and animal remains are preserved in sedimentary rock
sedimentation: process in which rock is formed from small pieces of sand, stone, etc. that have been left by water, ice, or wind
extraction: taking something away from somewhere else, especially using effort or force
combustion: a chemical process in which a substance reacts rapidly with oxygen and gives off heat
greenhouse effect: a process that occurs when gases in Earth's atmosphere trap the Sun's heat
built environment: human-made structures or conditions in an area
urbanisation: the increase in the proportion of people living in towns and cities, along with the built environment
livestock: a population of animals kept by humans for their use
ocean acidification: a reduction in the pH of the ocean over time, caused primarily by absorption of carbon dioxide
habitat: the natural home or environment of an animal, plant, or other organism
Holocene: the current geological epoch, beginning approximately 11,700 years ago, noted for its stable climate
legal personhood: a legal concept where a person or a thing has legal rights and/or duties