Skip to topic
    ← Back to course topics

    Carbon stores in different biomes — Eduqas A-Level Geography

    Test yourself on Carbon stores in different biomes with EDUQAS A-Level practice questions.

    Start free

    7 days Premium · Then free forever · No card, no charge

    Carbon stores in different biomes explained

    This topic examines the carbon stores within tropical rainforest and temperate grassland biomes, the factors influencing their size (temperature, precipitation, light), and the impact of human activities such as land-use change (deforestation, afforestation, and agricultural activity) on these stores.

    What to demonstrate

    1. Identification of carbon stores in tropical rainforests and temperate grasslands
    2. Explanation of how temperature, precipitation, and light influence the size of carbon stores in these biomes
    3. Analysis of how human activities (deforestation, afforestation, agricultural activity) alter carbon store sizes
    Show all 4 objectives
    1. Understanding of the concept of mass balance in relation to carbon stores

    Carbon stores in different biomes exam tips

    Topic Overview

    This topic delves into the fascinating world of how carbon is stored across Earth's diverse biomes. You'll explore the various forms carbon takes – from living biomass (plants and animals) to dead organic matter in soils and sediments – and understand why these stores differ significantly depending on the biome's unique climatic conditions, vegetation types, and ecological processes. Understanding these carbon reservoirs is fundamental to grasping the global carbon cycle and its intricate links to climate regulation.

    The significance of carbon stores in different biomes extends far beyond academic interest; it's central to comprehending global environmental challenges, particularly climate change. Biomes act as crucial carbon sinks, absorbing carbon dioxide from the atmosphere, thereby mitigating the greenhouse effect. However, human activities like deforestation, land-use change, and agricultural practices can transform these sinks into carbon sources, releasing stored carbon back into the atmosphere and accelerating global warming. This topic therefore highlights the delicate balance within natural systems and the profound impact of human intervention.

    Within the broader WJEC A-Level Geography curriculum, 'Carbon stores in different biomes' forms a vital component of the 'Global Systems' unit. It builds upon your knowledge of the global carbon cycle and links directly to 'Climate Change: Causes and Consequences' by illustrating how changes in biome carbon storage affect atmospheric CO2 levels. Furthermore, it integrates with 'Ecosystems' by demonstrating the ecological processes (e.g., photosynthesis, respiration, decomposition) that govern carbon flux and storage, providing a holistic understanding of Earth's interconnected systems.

    Key Concepts
    • →Biomass Carbon: Carbon stored in living organisms, primarily plants (trees, grasses) and, to a lesser extent, animals. This is particularly significant in highly productive biomes like tropical rainforests.
    • →Soil Carbon: Carbon stored in organic matter within the soil, derived from dead plant and animal material. This store can be substantial, especially in biomes with slow decomposition rates like tundra or grasslands.
    • →Carbon Sequestration: The natural process by which carbon dioxide is removed from the atmosphere and stored in carbon sinks (e.g., forests, oceans, soils).
    • →Carbon Sinks vs. Sources: A carbon sink absorbs more carbon than it releases, while a carbon source releases more carbon than it absorbs. Biomes can act as either, depending on natural processes and human impacts.
    • →Factors Influencing Carbon Storage: Climate (temperature, precipitation), vegetation type, soil characteristics, decomposition rates, and human activities all dictate the size and stability of carbon stores within a biome.
    Marking Points
    • Identification of carbon stores in tropical rainforests and temperate grasslands
    • Explanation of how temperature, precipitation, and light influence the size of carbon stores in these biomes
    • Analysis of how human activities (deforestation, afforestation, agricultural activity) alter carbon store sizes
    • Understanding of the concept of mass balance in relation to carbon stores
    Examiner Tips
    • 💡Ensure you can explicitly link climate variables (temperature, precipitation, light) to the biological processes (photosynthesis, decomposition) that determine carbon storage in these specific biomes
    • 💡Use specific examples of land-use change to illustrate the shift in carbon stores
    • 💡Be prepared to apply the concept of mass balance to explain why a store might increase or decrease
    • 💡Use Specific Biome Examples: Don't just say 'forests'; specify 'tropical rainforests' or 'boreal forests' and explain *why* their carbon stores differ. For instance, tropical rainforests have high biomass carbon due to rapid growth, while boreal forests have significant soil carbon due to slow decomposition.
    • 💡Quantify and Compare: Where possible, use approximate figures or comparative terms (e.g., 'vast amounts,' 'significant proportion') to demonstrate depth of knowledge. Compare the relative importance of biomass vs. soil carbon in different biomes.
    • 💡Link to Processes and Impacts: Always explain the underlying ecological processes (photosynthesis, respiration, decomposition) that govern carbon storage. Crucially, connect this to human impacts (deforestation, agriculture) and their consequences for the global carbon cycle and climate change.
    Common Mistakes
    • Confusing the factors influencing store size (e.g., attributing light as a primary driver for soil carbon rather than biomass)
    • Failing to distinguish between the impacts of different land-use changes (e.g., equating afforestation with deforestation)
    • Neglecting the role of temperature and precipitation in regulating decomposition rates and thus carbon storage
    • Misconception: All biomes store carbon primarily in living biomass. Correction: While biomass is crucial in some biomes (e.g., tropical rainforests), others, like grasslands and tundra, store a significant, often larger, proportion of their carbon in the soil due to factors like slow decomposition or extensive root systems.
    • Misconception: The carbon cycle within a biome is a static process. Correction: The carbon cycle is highly dynamic. Carbon continuously moves between biomass, soil, and the atmosphere through processes like photosynthesis, respiration, and decomposition. Disturbances (e.g., fires, deforestation) can rapidly alter these fluxes.
    • Misconception: Only terrestrial biomes are relevant for carbon storage. Correction: Oceanic biomes are immense carbon stores, holding far more carbon than terrestrial biomes. They absorb atmospheric CO2 through physical and biological pumps, storing it in surface waters, marine life, and deep ocean currents and sediments.
    Revision Plan
    1. 1Week 1 - Step 1: Review the global carbon cycle and the definition of different biomes. Create a table listing the major biomes and their key climatic characteristics (temperature, precipitation).
    2. 2Week 1 - Step 2: For each major biome, research and note down the primary forms of carbon storage (biomass, soil, dead organic matter) and the relative importance of each. Focus on *why* these differences exist, linking to climate and vegetation.
    3. 3Week 2 - Step 3: Deep dive into the ecological processes. Understand how photosynthesis, respiration, and decomposition rates vary across biomes and how these affect carbon sequestration and release. Consider the role of permafrost in tundra.
    4. 4Week 2 - Step 4: Analyse human impacts. Investigate how activities like deforestation (tropical rainforests), agricultural expansion (grasslands), and permafrost melt (tundra) affect carbon stores, turning sinks into sources.
    5. 5Week 2 - Step 5: Practice exam questions, focusing on data interpretation (e.g., graphs showing carbon density) and essay questions that require you to compare and contrast carbon stores across multiple biomes and evaluate their significance for the global carbon cycle.
    Exam Question Types
    • 📋Short Answer/Explanation Questions (e.g., 'Explain how carbon is stored in a tropical rainforest biome.'): These require you to identify the main stores (biomass, soil) and briefly explain the processes involved (photosynthesis, rapid growth, rapid decomposition). Ensure you use specific biome characteristics.
    • 📋Data Response Questions (e.g., 'Analyse the provided data showing carbon stores in different biomes and discuss its implications for climate change.'): You'll need to interpret graphs, tables, or maps, identify trends, compare biomes, and link the data to the broader context of the carbon cycle and human impact.
    • 📋Essay Questions (e.g., 'Evaluate the relative importance of different terrestrial biomes as carbon stores and their vulnerability to human activity.'): These demand a structured argument, comparing multiple biomes, discussing both biomass and soil carbon, and critically assessing the threats and management strategies. Use specific examples and detailed explanations.
    • 📋Synoptic Questions (e.g., 'To what extent can the protection of specific biomes contribute to mitigating climate change?'): These questions require you to draw on knowledge from across the curriculum, linking carbon storage in biomes to climate change policies, international agreements, and sustainable development goals.
    Frequently Asked Questions
    Why are tropical rainforests considered such important carbon stores?
    Tropical rainforests are vital carbon stores due to their exceptionally high net primary productivity (NPP) and rapid growth rates, leading to massive amounts of carbon stored in their living biomass (trees and other vegetation). Although decomposition is also rapid, the sheer volume of organic matter means a significant carbon pool is maintained. They continuously absorb vast quantities of atmospheric CO2 through photosynthesis, acting as a crucial global carbon sink and playing a key role in regulating the Earth's climate.
    How does temperature affect carbon storage in different biomes?
    Temperature significantly influences carbon storage by affecting both photosynthetic rates and decomposition rates. In warmer biomes like tropical rainforests, high temperatures promote rapid plant growth (more carbon uptake) but also accelerate decomposition, meaning less carbon accumulates in the soil. Conversely, in colder biomes such as tundra, low temperatures inhibit both plant growth and, crucially, microbial decomposition. This leads to slow carbon uptake but allows large amounts of organic carbon to accumulate and be stored in the soil, often locked in permafrost.
    What's the main difference between biomass carbon and soil carbon, and where is each most important?
    Biomass carbon refers to carbon stored in living organisms, primarily plants, through photosynthesis. It's most dominant in highly productive biomes with dense vegetation, like tropical rainforests. Soil carbon, on the other hand, is carbon stored in dead organic matter (humus, detritus) within the soil. It becomes particularly important in biomes where decomposition is slow due to cold or waterlogged conditions, such as boreal forests, grasslands, and tundra, where it can represent a much larger store than the living biomass.
    Are oceans considered biomes in terms of carbon storage, and how do they store carbon?
    Yes, oceans are immense carbon stores, often considered the largest active carbon reservoir on Earth. They store carbon through both physical and biological processes. The 'physical pump' involves CO2 dissolving directly into surface waters and then being transported to the deep ocean via currents. The 'biological pump' involves marine organisms taking up dissolved CO2 for photosynthesis (phytoplankton), which then gets transferred through the food web and eventually sinks to the seabed as dead organic matter, locking carbon away for centuries or millennia.
    How do human activities impact carbon stores in biomes?
    Human activities profoundly impact biome carbon stores, often turning natural sinks into sources. Deforestation, particularly in tropical rainforests, releases vast amounts of stored biomass carbon through burning and decomposition. Agricultural practices, such as ploughing and overgrazing, can deplete soil organic carbon. The melting of permafrost due to global warming, exacerbated by human emissions, releases ancient carbon stores from tundra biomes. These activities collectively contribute significantly to increased atmospheric CO2 levels and accelerate climate change.
    Which terrestrial biome stores the least carbon and why?
    Deserts generally store the least amount of carbon among terrestrial biomes. This is primarily due to extremely low precipitation and high temperatures, which severely limit plant growth and thus biomass. The sparse vegetation means very little carbon is sequestered from the atmosphere. While some carbon can be stored in the soil, the lack of organic matter input and rapid decomposition in dry conditions means these stores are also minimal compared to other biomes.