AQA A-Level Geography Paper 1, June 2025: Question 6
48 marks · Hard difficulty · Extended Response
Assess ecological concepts and human impacts on ecosystems, covering climatic climax, carbon storage across biomes, woodland nutrient cycling, climate change in savanna grasslands, and coral reef sustainability.
Practise this questionQuestion
Question text
Question 6 Ecosystems under stress
06.1 Outline the concept of climatic climax.
[4 marks]
Extra space …
Figure 11 is in the insert.
Figure 11 shows the amount of organic carbon stored in different parts of various
world biomes.
06.2 Analyse the data shown in Figure 11.
[6 marks]
… 8
(35)
Extra space …
Figure 12 is in the insert.
Figure 12 shows the nutrient cycle in a typical temperate deciduous woodland.
06.3 Using Figure 12 and your own knowledge, assess impacts of human activity on the
cycling of nutrients in a temperate deciduous woodland.
[9 marks]
(36) …
Extra space …
… 38
… 8
(37) …
06.4 Assess the potential impact of climate change upon people living in savanna
grasslands.
[9 marks]
Extra space …
(38) …
06.5 With reference to a coral reef that you have studied, assess the sustainability of
human activity within the area.
[20 marks]
… 40
… 8
(39)
… 41
Extra space …
(40)
Mark scheme
Show the mark scheme
Question 6 Ecosystems under stress
Total
Qu Part Marking guidance
marks
06 1 Outline the concept of climatic climax. 4
AO1=4
Point marked
Allow 1 mark per valid point with extra mark(s) for developed points (d).
For example:
Notes for answers
AO1
• This is the final stage of succession in an area where the dominant
vegetation has reached equilibrium with the surrounding environment
(1). No further changes will occur unless the environment changes or
a new more suitably adapted species is introduced (1) (d). Any new
species would need to outcompete the existing dominant vegetation in
the community (1) (d). This vegetation community is best adapted to
the prevailing climatic conditions of the area (1) (d).
• To reach this stage pioneers initially colonise the area requiring nothing
more than light, heat, water and the most basic nutrients found on bare
rock (1). Examples includes moss and lichen (1) (d).
• When these pioneers die (and with some weathering of parent rock) a
very basic soil forms allowing other species to colonise (1). The
addition of organisms (decomposers) also aids this process (1) (d).
• New species continue to hold the niche but they themselves are
outcompeted (succession) until the climax is achieved (1).
• Max 1 for example e.g. temperate deciduous woodland (1).
– A-LEVEL GEOGRAPHY – –
The notes for answers are not exhaustive. Credit any valid points.
06 2 Analyse the data shown in Figure 11. 6
AO3=6
AO3 – Analysis relates to identification of pattern and trends as well as
anomaly. There is also opportunity to manipulate data.
Mark scheme
Level 2 (4–6 marks)
AO3 – Clear analysis of the quantitative evidence provided, which makes
appropriate use of data in support. Clear connection(s) between different
aspects of the data and evidence.
Level 1 (1–3 marks)
AO3 – Basic analysis of the quantitative evidence provided, which makes
limited use of data and evidence in support. Basic connection(s)
between different aspects of the data and evidence.
Notes for answers
AO3
• Tropical wet and moist store most of their carbon in the biomass
40 compared to the other biomes. For example, Tropical moist stores
over 150 gigatonnes of carbon in its biomass compared to 25 gigatons
for warm temperate moist, a difference of over 125 gigatons.
• In terms of total biomass, Tropical moist may at first glance appear to
be the biggest store at around 300 gigatons (155 biomass, 75 topsoil
and 70 subsoil). However, this is comfortably exceeded by the Boreal
moist biome which has around 365 gigatons stored in total (25 in
biomass, 160 in topsoil and 190 in subsoil). This is a difference of 65
gigatons.
• Tropical wet and moist also represent an anomaly in that they are the
only two biomes with more carbon in the biomass than the combined
soils total, e.g. tropical wet has around 140 gigatons in biomass
compared to a combined 125 gigatons in the two soil types.
• There are three biomes with more carbon in the topsoil compared to
the subsoil. The difference appears to be around 5-10 gigatons.
• Boreal moist has the largest differential between topsoil and subsoil; a
difference of around 30–35 gigatons.
– A-LEVEL GEOGRAPHY – –
Credit any other valid analysis.
06 3 Using Figure 12 and your own knowledge, assess impacts of human 9
activity on the cycling of nutrients in a temperate deciduous AO1=4
woodland. AO2=5
AO1 – Knowledge and understanding of nutrient cycling. Awareness of
ecosystem responses to changes in one or more of their components.
AO2 – Application of knowledge and understanding to assess the impact
of human activity on nutrient cycling.
Mark scheme
Level 3 (7–9 marks)
AO1 – Demonstrates detailed knowledge and understanding of concepts,
processes, interactions and change. These underpin the response 41
throughout.
AO2 – Applies knowledge and understanding appropriately with detail.
Connections and relationships between different aspects of study are
fully developed with complete relevance. Assessment is detailed and
well supported with appropriate evidence.
Level 2 (4–6 marks)
AO1 – Demonstrates clear knowledge and understanding of concepts,
processes, interactions and change. These are mostly relevant though
there may be some minor inaccuracy.
AO2 – Applies clear knowledge and understanding appropriately.
Connections and relationships between different aspects of study are
evident with some relevance. Assessment is evident and supported with
clear and appropriate evidence.
Level 1 (1–3 marks)
AO1 – Demonstrates basic knowledge and understanding of concepts,
processes, interactions and change. This offers limited relevance with
inaccuracy.
AO2 – Applies limited knowledge and understanding. Connections and
relationships between different aspects of study are basic with limited
relevance. Assessment is basic and supported with limited appropriate
evidence.
Notes for answers
AO1
• Mineral nutrient cycling.
• Ecosystem responses to changes in one or more of their components
or environmental controls.
• Factors influencing the changing of ecosystems including human
exploitation.
• Succession and climatic climax as illustrated by lithoseres.
• The characteristics of the climatic climax: temperate deciduous–A-LEVEL GEOGRAPHY– –
woodland biome.
42 AO2
• Deforestation is one obvious activity which would impact on mineral
nutrient cycling. This would immediately remove the biomass store
and also remove the transfer to the litter.
• Afforestation would have the opposite effect to the above but this
depends on the species planted. An orchard or a plantation for the
timber industry would inevitably change the size of the biomass store
depending upon what was planted.
• Similarly, if trees are planted for specific purposes, such as Christmas
trees (fir and spruce conifers), these are likely to have negative
impacts on the litter as they are evergreen. Needles are less easy to
decompose and release fewer nutrients into the soil.
• If trees are removed and nothing is replanted, the area becomes at risk
of increased loss by leaching, thus increasing the size of that pathway
out of the system. Similarly, loss by run off is likely to increase with no
canopy to protect the soil underneath.
• Input from dissolved nutrients in rainfall may increase with no canopy
to intercept vegetation. With more water reaching the ground there
may be more infiltration and percolation. This may possibly increase
the input of nutrients from weathered rock.
• Knowledge of specific nutrients are not required but some reference to
nitrogen, phosphorus and potassium etc.–A-LEVEL GEOGRAPHY – –
Credit any other valid assessment.
06 4 Assess the potential impact of climate change upon people living in 9
savanna grasslands. AO1=4
AO2=5
AO1 – Knowledge and understanding of pressures facing the savanna
grasslands.
AO2 – Application of knowledge and understanding to assess the
potential impact of climate change on this region for people, plants and
animals.
Mark scheme
Level 3 (7–9 marks)
AO1 – Demonstrates detailed knowledge and understanding of concepts,
processes, interactions and change. These underpin the response
throughout.
AO2 – Applies knowledge and understanding appropriately with detail.
Connections and relationships between different aspects of study are
fully developed with complete relevance. Assessment is detailed and
well supported with appropriate evidence.
Level 2 (4–6 marks)
AO1 – Demonstrates clear knowledge and understanding of concepts,
processes, interactions and change. These are mostly relevant though
there may be some minor inaccuracy.
AO2 – Applies clear knowledge and understanding appropriately.
Connections and relationships between different aspects of study are
evident with some relevance. Assessment is evident and supported with
clear and appropriate evidence.
Level 1 (1–3 marks)
AO1 – Demonstrates basic knowledge and understanding of concepts,
processes, interactions and change. This offers limited relevance with
inaccuracy.
AO2 – Applies limited knowledge and understanding. Connections and
relationships between different aspects of study are basic with limited
relevance. Assessment is basic and supported with limited appropriate–A-LEVEL GEOGRAPHY– –
evidence.
Notes for answers
AO1
• The concept of the biome. The global distribution of major terrestrial
biomes.
• Savanna grassland to include:
o the main characteristics of the biome
o ecological responses to the climate, soil and soil moisture budget –
adaptations by flora and fauna
o human activity and its impact on the biome
o typical development of issues in the biome to include changes in
population, economic development, agricultural extension and
intensification, implications for biodiversity and sustainability.
44 AO2
• The climate of the savanna is considerably varied depending on
location. It is characterised by a wet and dry season, but within this
both precipitation and temperature show considerable variation.
• Species are highly adapted to these conditions: the baobab and acacia
are two examples of species adapted to cope with the high
temperature and lack of all-year-round water; grasses are well adapted
to cope with drought and fire.
• Most agree that temperatures are set to increase generally across the
savanna and rainfall will become less reliable and predictable in terms
of volume and timeliness.
• The ramifications of this for people are expected to be substantial.
• The grasses provide the basis of the food chain, whilst the rains
provide the water for the arable farmers in the savanna. This has
implications for both the pastoralists and arable farmers.
• Similarly, the wildlife is wholly dependent on the seasonal rains for
food from grass or water for drinking. Those species further up the
food chain have little chance of surviving if there is no water and their
food source is under threat.
• Other industries such as tourism are also totally (albeit indirectly)
reliant on a reliable climate. Hotels require substantial quantities of
water for guests and most tourists are in these areas to visit the wildlife
of the game reserves.
• It is hard to see anything other than a very challenging future for the
people and ecosystem of the savanna grasslands.
Credit any other valid approach. Assessment–A-LEVEL GEOGRAPHYshould be based upon– –
preceding content.
06 5 With reference to a coral reef that you have studied, assess the 20
sustainability of human activity within the area. AO1=10
AO2=10
AO1 – Knowledge and understanding of the pressures facing coral reefs.
AO2 – Application of knowledge and understanding to assess the
sustainability of coral reef exploitation.
Notes for answers
AO1
• The distribution and main characteristics of coral reef ecosystems. 45
• Environmental conditions associated with reef development. The
following aspects should be examined with reference to a named,
located coral reef:
o factors in the health and survival of reefs
o natural: water temperature, acidity, salinity, algal blooms
o human activity and its impact: major drainage basin schemes,
onshore development, desalination, pollution, tourism, fishing
o future prospects for coral reefs.
AO2
• The direction of the response will depend on the choice of supporting
material.
• Most are likely to argue that current practices exploiting coral reefs are
unsustainable. There are many threats facing the reef systems.
Pollution (from factories on land and boats at sea), overfishing
(particularly dangerous practices include dynamite fishing as well as
the use of cyanide), souvenir hunting as well as coral extraction for use
in industries such as construction.
• Probably the biggest threat is from climate change. Though the human
activity has a limited link to the area itself, the impacts certainly are
within the area. Coral bleaching occurs when the temperatures
become too high for the coral. The algae dies and the mutually
dependent symbiotic relationship is destroyed.
• Natural predators such as the crown of thorns starfish may be
increasing in number due to certain human activities. Offshore
dredging for example is thought to increase the amount of
phytoplankton which the starfish larvae feed off.
• Finally, increased frequency and intensity of tropical storms may also
be indirectly attributable to human activity through climate change.
Whilst coral protects coastlines from the worst impacts of tropical
storms, the associated storm surges can do enormous damage to the
coral once they strike the coast.
• There are a number of success stories in sustainable coral
management. In Australia, work has been undertaken to promote the
growth of algae on corals which are more tolerant to increased global
temperatures, surviving in temperatures up to 31 °C.
• Corals in the Gulf of Aqaba, in the northernmost region of the Red Sea,
are capable of withstanding ocean temperature fluctuations that
normally cause coral bleaching elsewhere.–A-LEVEL GEOGRAPHYIdentifying the durability of– –
the reef may be key to maintaining the protection of coral reefs in other
46 regions of the world with vulnerability to ocean temperature
increases. In 2020, experts applied to UNESCO to designate the
2500-mile coral reef of the Red Sea a Marine World Heritage Site.
• Dense root systems of mangrove trees capture sediments moving
down rivers. Mangrove helps to protect the coastline and prevents
tides and hurricanes from eroding. The trees also shield coral reefs
and seagrass meadows from being smothered in sediment. Protecting
mangrove is increasingly becoming seen as having an associated
positive impact on coral as often they occupy adjacent locations in the
same places.
• Overall, the future is not looking positive but there are measures in
place to try to improve this outlook. – A-LEVEL GEOGRAPHY – –
Credit any other valid approach.
Marking grid for Question 06.5
Level/ Criteria/Descriptor
Mark
Range
Level 4 • Detailed evaluative conclusion that is rational and firmly based on knowledge and
(16–20 understanding which is applied to the context of the question. Interpretations are
marks) comprehensive, sound and coherent (AO2).
• Detailed, coherent and relevant analysis and evaluation in the application of knowledge
and understanding throughout (AO2).
• Full evidence of links between knowledge and understanding to the application of
knowledge and understanding in different contexts (AO2).
• Detailed, highly relevant and appropriate knowledge and understanding of place(s) and
environments used throughout (AO1).
• Full and accurate knowledge and understanding of key concepts, processes and
interactions and change throughout (AO1).
• Detailed awareness of scale and temporal change which is well integrated where
appropriate (AO1).
Level 3 • Clear evaluative conclusion that is based on knowledge and understanding which is
(11–15 applied to the context of the question (AO2).
marks) • Generally clear, coherent and relevant analysis and evaluation in the application of
knowledge and understanding (AO2).
• Generally clear evidence of links between knowledge and understanding to the
application of knowledge and understanding in different contexts (AO2).
• Generally clear and relevant knowledge and understanding of place(s) and
environments (AO1).
• Generally clear and accurate knowledge and understanding of key concepts and
processes (AO1).
• Generally clear awareness of scale and temporal change which is integrated where
appropriate (AO1).
Level 2 • Some sense of an evaluative conclusion partially based upon knowledge and
(6–10 understanding which is applied to the context of the question (AO2).
marks) • Some partially relevant analysis and evaluation in the application of knowledge and
understanding (AO2).
• Some evidence of links between knowledge and understanding to the application of
knowledge and understanding in different contexts (AO2).
• Some relevant knowledge and understanding of place(s) and environments which is
partially relevant (AO1).
• Some knowledge and understanding of key concepts, processes and interactions and
change (AO1). 47
• Some awareness of scale and temporal change which is sometimes integrated where
appropriate. There may be a few inaccuracies (AO1).
Level 1 • Very limited and/or unsupported evaluative conclusion that is loosely based upon
(1–5 knowledge and understanding which is applied to the context of the question (AO2).
marks) • Very limited analysis and evaluation in the application of knowledge and understanding.
This lacks clarity and coherence (AO2).
• Very limited and rarely logical evidence of links between knowledge and understanding
to the application of knowledge and understanding in different contexts (AO2).
• Very limited relevant knowledge and understanding of place(s) and environments (AO1).
• Isolated knowledge and understanding of key concepts and processes (AO1).
• Very limited awareness of scale and temporal change which is rarely integrated where
appropriate. There may be a number of inaccuracies (AO1).
Level 0 • Nothing worthy of credit.
(0 marks)
How to answer it
AQA A-Level Geography: Ecosystems Under Stress
📋 What this question tests
This full exam question assesses core knowledge across biomes, succession, nutrient cycling, ecological vulnerability, and human management strategies under changing climatic conditions:
- 06.1 (4 marks): Precise conceptual understanding of ecological succession, pioneer species, dynamic equilibrium, and climatic climax communities (AO1).
- 06.2 (6 marks): Quantitative graph and data analysis (AO3), focusing on biomass vs. soil carbon stores across biomes, anomaly spotting, and data manipulation.
- 06.3 (9 marks): Systems application using Gersmehl diagrams (AO1 & AO2) to assess how human interventions (deforestation, afforestation, commercial plantation) disrupt nutrient transfers and stores in temperate deciduous forests.
- 06.4 (9 marks): Synoptic evaluation of climate change impacts on savanna grassland ecology and the subsequent socioeconomic consequences for human populations (AO1 & AO2).
- 06.5 (20 marks): Extended evaluative essay assessing the environmental, economic, and social sustainability of human actions on coral reef biomes, integrating global threats like ocean warming/acidification with local management (AO1 & AO2).
Concept of Climatic Climax
Outline the concept of climatic climax.
💡 Key Knowledge
- Definition: The final, stable stage of ecological succession where plant community development reaches dynamic equilibrium with the prevailing regional climate.
- Successional pathway: Begins with pioneer species colonising bare rock/substrate (lithosere), altering the environment by breaking down minerals and depositing organic humus upon death.
- Species competition: Succession progresses as taller, competitive species outcompete pioneers for sunlight, water, and soil nutrients.
- Climatic equilibrium: No further vegetation changes occur unless external factors change (e.g. climate shifts, human interference creating a plagioclimax).
✅ Model Answer (Full 4 Marks)
Climatic climax represents the final, stable stage of vegetation succession in an area, in which the ecosystem has achieved dynamic equilibrium with the ambient macroclimate.
Succession begins when hardy pioneer species (such as lichens and mosses) colonise barren ground. As these pioneer organisms die, decomposers break them down to create initial primitive soils. Taller, nutrient-demanding species then invade and progressively outcompete earlier pioneers for light, moisture, and space.
Eventually, a dominant vegetation type establishes that is best adapted to the local climatic conditions (e.g. temperate deciduous oak woodland in the UK). This state remains self-sustaining unless external environmental or anthropogenic perturbations occur.
🧠 Exam Technique & Mark Breakdown
- Point-marked scheme (1 mark per valid point, up to 4 marks; +1 for well-developed points).
- Always name a real-world example (e.g., deciduous woodland or boreal taiga) for an easy 1 mark.
- Ensure you show progression: bare rock → pioneer modification → progressive competition → final equilibrium with climate.
❌ Common Errors
- Confusing climatic climax with plagioclimax (a community arrested by human interference such as grazing or heather burning).
- Failing to mention the word climate: it is climax determined by climate, not local edaphic (soil) factors.
- Describing only the final forest without referencing the dynamic process of succession that led to it.
Data Analysis: Carbon Storage in World Biomes
Analyse the data shown in Figure 11 (Organic carbon in different parts of various world biomes).
🧠 Data Analysis Strategy (AO3)
To reach Level 2 (4–6 marks), you must synthesize patterns, anomalies, and perform data manipulation (calculating differences, ratios, or totals):
- Broad trend: Tropical wet and moist store the bulk of carbon in above-ground biomass, whereas higher latitude/colder biomes store far more in the soil.
- Soil breakdown: Topsoil vs. subsoil ratios across ecosystems.
- Data manipulation: Explicit calculations comparing totals or components.
📐 Step-by-Step Data Manipulations
- Total Ecosystem Carbon Comparison:
Tropical moist total = 155 (biomass) + 75 (topsoil) + 70 (subsoil) = 300 Gt .
Boreal moist total = 25 (biomass) + 160 (topsoil) + 180 (subsoil) = 365 Gt .
Calculated difference: Boreal moist stores 65 Gt more total organic carbon than tropical moist. - Biomass Dominance Contrast:
Tropical moist biomass ( 155 Gt ) exceeds warm temperate moist biomass ( 25 Gt ) by 130 Gt (over 6× greater). - Biomass vs Soil Anomaly:
Tropical wet and moist are the only biomes where carbon stored in living biomass ( 140–155 Gt ) exceeds combined soil stores ( 125–145 Gt ).
✅ Model Answer (Level 2: 6/6 Marks)
Figure 11 reveals clear contrasts in carbon partitioning between low-latitude and high-latitude biomes. Tropical wet and moist biomes store the majority of their carbon in living biomass, with tropical moist storing 155 gigatons (Gt) in biomass compared to just 25 Gt in temperate moist and 25 Gt in boreal moist—a difference of 130 Gt.
While tropical moist appears largest at first glance due to biomass dominance, calculation of total ecosystem carbon reveals that Boreal moist is the largest overall carbon reservoir at 365 Gt (25 Gt biomass + 160 Gt topsoil + 180 Gt subsoil), exceeding tropical moist (300 Gt total) by 65 Gt.
Anomalously, tropical wet and moist are the only two biomes where above-ground biomass carbon exceeds the combined soil store (e.g. tropical wet holds ~140 Gt in biomass versus 125 Gt across topsoil and subsoil combined). In all temperate and boreal systems, subterranean storage dominates due to reduced decomposition rates. Finally, boreal moist exhibits the single largest absolute difference between soil horizons, with subsoil (180 Gt) exceeding topsoil (160 Gt) by 20 Gt.
Human Impacts on Woodland Nutrient Cycling
Using Figure 12 and your own knowledge, assess impacts of human activity on the cycling of nutrients in a temperate deciduous woodland.
💡 Gersmehl Cycle Fundamentals
- Temperate Deciduous Baseline: Soil is usually the largest nutrient store due to deep leaf fall and moderate decomposition rates; biomass is medium-to-large; litter store is intermediate and fluctuates seasonally.
- Key Transfers: Fall of litter (leaves/twigs), decomposition/mineralisation into soil, plant uptake by roots, rainfall inputs, weathering inputs, runoff, and leaching losses.
🧠 Top-Level Assessment Framework
- You must examine both additions/replacements (e.g. afforestation, fertilisers) and depletions (deforestation, timber harvesting, acid rain).
- Directly track the cascades: If Store A shrinks, what happens to Flow B and Store C?
- Reference specific nutrients: nitrogen (N), phosphorus (P), potassium (K), or calcium (Ca).
✅ Model Assessment (Level 3: 8–9 Marks)
In a natural temperate deciduous woodland (Figure 12), the soil constitutes the largest store of nutrients, nourished by regular leaf litter fall and moderate decomposition, with efficient root uptake cycling nutrients back into the biomass store. Anthropogenic interference dramatically disrupts these internal pathways:
1. Clear-Felling / Commercial Deforestation: Direct extraction of timber immediately removes the primary organic nutrient pool held within the biomass store. Consequently, litter fall ceases, starving the litter layer. Without tree roots to absorb dissolved ions, the mineral soil becomes unprotected. Interception loss reaches zero, causing precipitation to hit bare ground directly; this escalates surface runoff and causes severe leaching of nitrates and potassium through the soil profile into groundwater, impoverishing the system.
2. Coniferous Afforestation (e.g. Monoculture Pine Plantations): Replacing native deciduous broadleaves (oak, beech) with commercial conifers radically alters litter chemistry. Coniferous needles are tough, waxy, and resinous, significantly retarding decomposition by soil fauna. This causes nutrients to become locked in a thick, acidic mor litter layer, restricting release into the soil store and leading to podsolisation.
Overall Assessment: Human impacts almost invariably destabilise the closed equilibrium of temperate nutrient cycling. Exploitative activities turn a recycling-dominated closed loop into an open, degraded system defined by severe output pathways (leaching and runoff).
❌ Common Misconceptions
Students frequently forget Figure 12 and write generic essays on deforestation. You must explicitly reference stores (circles) and pathways/fluxes (arrows) shown in the Gersmehl model (e.g., litter store, soil store, leaching, uptake, weathering).
Climate Change Impacts on Savanna Grasslands
Assess the potential impact of climate change upon people living in savanna grasslands.
💡 Savanna Biome Characteristics
- Climatic Regime: Marked distinct wet and dry seasons; controlled by the seasonal migration of the Intertropical Convergence Zone (ITCZ).
- Vegetation: Continuous C4 drought-resistant grasses dotted with xerophytic/pyrophytic trees (acacias, baobabs).
- Livelihoods: Pastoral nomadism (e.g., Maasai), subsistence farming (sorghum, millet), commercial cattle ranching, and eco-tourism/safaris.
❌ Pitfalls to Avoid
- Focusing only on animals and ignoring people (the question explicitly asks for impacts on people living in savanna grasslands).
- Ignoring positive or adaptive aspects: the best candidates assess vulnerabilities alongside adaptation efforts.
- Treating climate change purely as "it gets hotter"; rainfall variability and unpredictability of the wet season are far more critical in the savanna.
✅ Model Assessment (Level 3: 8–9 Marks)
Savanna grasslands (such as the Sahel and East African savannas) support millions of people through pastoralism, subsistence agriculture, and wildlife tourism. These communities are acutely vulnerable to climate change due to their direct dependence on predictable seasonal rainfall.
Impacts on Pastoralists and Subsistence Farmers: Projected temperature increases (1.5°C to 3°C) coupled with more erratic rainfall undermine the base of the savanna food web. Grass productivity drops sharply when rains fail. For pastoralists like the Maasai, prolonged droughts deplete livestock herds through dehydration and starvation. Crop failures of staple cereals (maize, sorghum) trigger severe food insecurity and famine. Competition for declining pasture and boreholes frequently sparks violent inter-community resource conflicts.
Economic and Tourism Impacts: Game reserves rely on seasonal waterholes to sustain megafauna (zebras, wildebeest, elephants). Reduced water availability forces wildlife migration away from protected areas or causes massive die-offs, directly threatening lucrative safari tourism—a crucial source of foreign exchange and employment for local guides, hospitality workers, and infrastructure development.
Conclusion / Evaluation: While some communities are adopting drought-tolerant crops and rainwater harvesting, the adaptive capacity of savanna populations is fundamentally constrained by poverty. The overall impact of climate change is overwhelmingly negative, threatening traditional cultures and driving rural-to-urban distress migration.
Extended Essay: Sustainability of Human Activity in Coral Reefs
With reference to a coral reef that you have studied, assess the sustainability of human activity within the area.
💡 Recommended Case Study: Great Barrier Reef (GBR) / Red Sea
- Optimal abiotic conditions: Water temperatures 23–29°C, clear saline water (32–42 PSU), high light penetration (<30m depth), low nutrient levels.
- Key Human Pressures:
- Local: Agricultural runoff (fertiliser-induced eutrophication, crown-of-thorns starfish blooms), sedimentation from coastal development, overfishing, anchor damage.
- Global: Rising sea surface temperatures causing mass bleaching (loss of symbiotic zooxanthellae) and ocean acidification lowering pH and calcification rates.
- Management Strategies: GBR Marine Park zoning, Reef 2050 Long-Term Sustainability Plan, indigenous ranger programs, mangrove restoration, crown-of-thorns culling.
🧠 Level 4 Essay Strategy (16–20 Marks)
- Define Sustainability: Explicitly evaluate environmental, economic, and social sustainability.
- Scale Distinction: Distinguish between local manageable activities (tourism, fishing, coastal runoff) and global unmanageable threats (climate warming, ocean acidification).
- Balanced Evaluation: Contrast high-tech/strict zoning successes with ongoing vulnerabilities; conclude with a substantiated overall judgement.
✅ Comprehensive Essay Structure & Key Evidence
Introduction:
Define sustainability in a marine context: human activities that meet current economic and social needs without compromising the ecological integrity and biodiversity of the reef ecosystem for future generations. The Great Barrier Reef (GBR), extending over 2,300 km off the coast of Queensland, Australia, provides a prime example where sophisticated local management struggles against insurmountable global anthropogenic pressures.
Theme 1: Tourism and Commercial Marine Use (Moderately Sustainable):
- Activities: Generates over A$6 billion annually and supports ~64,000 jobs through diving, snorkeling, and commercial boating.
- Pressures: Coral breakage from boat groundings, anchor drag, and sunscreen chemical pollution.
- Evaluation: Highly regulated under the Great Barrier Reef Marine Park Authority (GBRMPA). Measures like the Environmental Management Charge ("reef tax"), designated mooring buoys, and strict no-go zoning make tourism largely environmentally sustainable at localized scales while maintaining economic prosperity.
Theme 2: Land-Based Agricultural Runoff & Water Quality (Unsustainable):
- Activities: Intensive sugarcane farming and beef cattle grazing along the Queensland catchment basins.
- Pressures: Influx of nitrates and phosphates causes eutrophication and triggers outbreaks of the predatory Crown-of-Thorns Starfish (Acanthaster planci), which can decimate 90% of live coral tissue in affected sectors. Sediment plumes smother corals, blocking sunlight needed for zooxanthellae photosynthesis.
- Evaluation: The "Reef 2050 Plan" targets a reduction in nitrogen loads, and riparian mangrove buffers help trap sediments. However, compliance among farmers is incomplete, leaving catchment management currently environmentally unsustainable.
Theme 3: Global Climate Change & Ocean Acidification (The Ultimate Limit to Sustainability):
- Processes: Atmospheric CO₂ absorption elevates sea surface temperatures and reduces carbonate ion availability (ocean acidification). Prolonged +1–2°C thermal anomalies force polyps to expel zooxanthellae, leading to mass bleaching (notably in 2016, 2017, 2020, 2022, and 2024).
- Evaluation: Even if all local activities were 100% sustainable, local managers cannot halt global warming. Scientists are trialing genetically resilient "super-corals" and cloud-brightening, but these are palliative.
Substantiated Conclusion:
Local human activities (such as tourism and commercial fishing) show high levels of regulatory sustainability due to proactive zoning by GBRMPA. However, human activity evaluated as a whole—encompassing industrial emissions and global fossil fuel consumption—is fundamentally unsustainable. Without deep, rapid global decarbonisation, local conservation merely delays the systemic ecological collapse of the ecosystem.
❌ What Separates Level 2/3 from Level 4
- Level 2/3 response: General description of reef destruction ("people drop anchors", "global warming bleaches coral") without specific spatial naming, zoning details, or chemical/biological mechanisms.
- Level 4 response: Integrates precise place details (GBRMPA, Reef 2050, Crown-of-Thorns starfish, specific bleaching years), contrasts local governance against global climate threats, and sustains a clear evaluative line throughout.
Topics
3.1 Physical geography · 3.4 Geographical skills checklist · 3.1.6 Ecosystems under stress · 3.4.1 Qualitative skills and quantitative skills
Question and mark scheme from the AQA A-Level Geography examination, Paper 1, June 2025. QuestionVault is an independent revision resource; questions remain the copyright of the awarding body.