Biology · Year 11 · Module 4 · Lesson 6
HSC Exam Practice
Abiotic Factors — The Physical and Chemical Environment
Short answer
1.Abiotic factors and tolerance ranges
Define the term abiotic factor and give two named examples from Australian ecosystems.
Distinguish between a tolerance range and an optimal zone, and state what occurs to an organism when it is in the zone of physiological stress.
Describe how soil pH affects plant distribution, using a specific mechanism (mineral availability or microbial activity) and a named Australian or global example.
Outline Liebig’s Law of the Minimum and Shelford’s Law of Tolerance, and state one key difference between them.
Data response
2.Data response — dissolved oxygen and temperature in a river
A scientist measured dissolved oxygen (DO) concentration and water temperature at five sites along a lowland river during late summer. Results are shown below.
(a) Describe the relationship between water temperature and dissolved oxygen concentration shown in the data.
(b) Explain the mechanism by which rising water temperature reduces dissolved oxygen concentration, and predict two consequences for fish species living at Site 5 compared with Site 1. Refer to the concepts of tolerance ranges and limiting factors in your answer.
(c) Assess whether dissolved oxygen or temperature is more likely to be the primary limiting factor for aerobic aquatic invertebrates at Site 5, justifying your answer using data from the graph.
Extended response
3.Extended response — the snow gum treeline
Analyse how the combined effect of three abiotic factors creates a distinct treeline for the snow gum (Eucalyptus pauciflora) at approximately 1,800 m in the Snowy Mountains. In your response, explain why the treeline is described as a “dynamic equilibrium” rather than a fixed barrier, and connect the role of temperature to your understanding of enzyme activity from Module 1.
Evaluate the prediction that a 2°C rise in average temperature in the Snowy Mountains would shift the snow gum treeline upward by 150–200 m. In your response you must:
- identify which abiotic factor is currently the primary limiting factor for snow gum recruitment above 1,800 m and justify your choice;
- assess how warming would alter this factor and at least two other abiotic factors acting at the treeline;
- consider whether the shift would be straightforward or whether other ecological consequences (including effects on endemic alpine species) complicate the prediction;
- reach an explicit evaluative conclusion about whether the prediction is likely to be an overestimate, underestimate or reasonable approximation.
Biology · Year 11 · Module 4 · Lesson 6
Answer Key & Marking Guidelines
Section 1 · Short answer · 2 marks · Band 3
Sample response. An abiotic factor is a non-living physical or chemical component of an ecosystem that influences the survival, distribution and abundance of organisms. Examples include water temperature and salinity in the Great Barrier Reef, soil pH in mallee shrublands, or rainfall in the semi-arid interior.
Marking criteria. 1 mark — definition must include “non-living” (or “physical/chemical”) AND reference to influence on organisms. 1 mark — two distinct named examples, each clearly abiotic (not biotic). Accept any accurate Australian or global examples.
Section 1 · Short answer · 3 marks · Band 3
Sample response. A tolerance range is the full span of values for a single abiotic factor within which an organism can survive, from the minimum tolerable value to the maximum tolerable value. The optimal zone is the narrower central portion of the tolerance range where growth is fastest, reproduction is most successful and survival is highest. In the zone of physiological stress, the organism can survive but growth slows, reproduction is impaired and energy must be diverted to coping with the suboptimal conditions.
Marking criteria. 1 mark — tolerance range correctly defined as the full min-to-max survival span. 1 mark — optimal zone correctly identified as the portion within the tolerance range where the organism thrives. 1 mark — physiological stress zone: organism survives but growth/reproduction is reduced (not zero, not lethal). Do not award the stress-zone mark if the student states the organism dies in that zone.
Section 1 · Short answer · 2 marks · Band 3
Sample response. Soil pH affects the availability of minerals to plants. In acidic soils (pH below 6), phosphorus becomes bound to iron and aluminium ions and is unavailable for plant uptake, limiting plant growth even when total phosphorus in the soil is high. Many Australian native plants (e.g. banksias, proteaceous shrubs) are adapted to naturally acidic, phosphorus-poor soils and are outcompeted if pH is raised. Alternatively, acid rain lowering lake pH below 5 kills freshwater fish by disrupting ion regulation across gill membranes.
Marking criteria. 1 mark — states a correct mechanism (mineral lock-up / unavailability at acidic pH, OR altered microbial decomposition rate, OR enzyme denaturation in aquatic organisms at extreme pH). 1 mark — names a specific example (Australian plant community, acid rain lake, ocean acidification, acid sulphate soil). Generic statements without a mechanism or example score 0.
Section 1 · Short answer · 3 marks · Band 3–4
Sample response. Liebig’s Law of the Minimum states that growth is dictated not by the total resources available, but by the scarcest resource (the limiting factor); if one essential resource is absent or deficient, growth will be limited regardless of the abundance of other resources. Shelford’s Law of Tolerance states that an organism’s distribution is controlled by the factor for which it has the narrowest tolerance range — too little or too much of that factor will exclude the organism. The key difference is that Liebig focuses on the minimum supply of a single scarcest resource, while Shelford focuses on the breadth of tolerance (narrowest range = most restricting), acknowledging that both deficiency and excess can be limiting.
Marking criteria. 1 mark — Liebig correctly described (growth limited by the single scarcest/most deficient resource). 1 mark — Shelford correctly described (distribution limited by the factor with the narrowest tolerance range). 1 mark — states a meaningful difference: Liebig is about minimum supply, Shelford is about breadth of tolerance (both too little and too much). Accept other valid distinctions.
Section 2 · Data response · 8 marks · Band 4–5
Sample response (a) — 2 marks. As water temperature increases from Site 1 (18°C) to Site 5 (33°C), dissolved oxygen concentration decreases from 10.2 mg/L to 4.2 mg/L. The relationship is inverse: higher temperature is associated with lower dissolved oxygen across all five sites. The drop is consistent and substantial (a 15°C rise in temperature is associated with a 6.0 mg/L decrease in DO).
Marking criteria (a). 1 mark — identifies an inverse/negative relationship (as temperature rises, DO falls). 1 mark — supports the trend with at least one correctly quoted figure pair from the data (e.g. “from 10.2 mg/L at 18°C to 4.2 mg/L at 33°C”).
Sample response (b) — 4 marks. Warm water holds less dissolved gas than cold water because the kinetic energy of water molecules at higher temperatures is sufficient to break gas-water interactions, allowing O2 molecules to escape to the atmosphere (reduced gas solubility). At Site 5 (33°C, 4.2 mg/L DO), fish will experience reduced aerobic respiration capacity compared with Site 1 (18°C, 10.2 mg/L DO), as available O2 for mitochondrial respiration is lower. Consequence 1: if the DO at Site 5 falls below the lower tolerance limit for a species (e.g. Murray cod requires approximately 5 mg/L), dissolved oxygen becomes the limiting factor and the species cannot persist — distribution is restricted to cooler upstream sites. Consequence 2: even if DO remains within the stress zone, fish must increase gill ventilation rate and expend more energy on osmoregulation and thermoregulation, reducing energy available for growth and reproduction (physiological stress).
Marking criteria (b). 1 mark — mechanism: reduced gas solubility at higher temperature causes O2 to escape to atmosphere (not simply “warm water holds less O2” without mechanism). 1 mark — tolerance range concept applied: if DO falls below lower tolerance limit at Site 5, it becomes the limiting factor. 1 mark — consequence 1 stated with ecological outcome (restricted distribution / exclusion from downstream). 1 mark — consequence 2 stated (physiological stress: reduced growth or reproduction even if organism survives).
Sample response (c) — 2 marks. At Site 5, dissolved oxygen (4.2 mg/L) is more likely to be the primary limiting factor for aerobic invertebrates than temperature (33°C). For many aquatic invertebrates, 4.2 mg/L is near or below the lower stress zone (many species require ≥5 mg/L for normal aerobic function), meaning DO is closest to or beyond the lower tolerance limit. While 33°C is warm, some invertebrates (e.g. yabbies) can tolerate temperatures up to 35°C, so temperature alone may not be lethal. Shelford’s Law supports this: the factor with the narrowest tolerance is most limiting, and DO at 4.2 mg/L narrows the tolerance for aerobic respiration more critically than temperature at 33°C for most species in this context.
Marking criteria (c). 1 mark — correctly identifies DO as the more likely primary limiting factor with reference to the data value (4.2 mg/L). 1 mark — justification references Shelford’s Law or the concept that DO is closest to the lower tolerance limit, using data from the graph. Accept a well-reasoned case for temperature if it is supported by data and tolerance range reasoning.
Section 3 · Extended response · 4 marks · Band 4–5
Sample response. Above 1,800 m in the Snowy Mountains, three abiotic factors interact to exclude snow gum trees. Temperature: the growing season above this elevation is too short (snow cover persists into November and frost returns in March) for snow gums to accumulate sufficient carbohydrates via photosynthesis to support growth and reproduction; this connects to Module 1, where enzyme activity (including RuBisCO in the Calvin cycle and amylase for starch mobilisation) requires temperatures above ~10°C — persistent cold means enzymes operate below their optimal temperature, drastically slowing metabolic rates. Wind: increasing wind speed causes mechanical desiccation by driving transpiration beyond what shallow root systems can replace, and also causes physical damage to branches. Soil: soils above 1,800 m are thin, poorly developed and subject to frost heave, which ruptures root cells and destabilises seedlings. Together these three factors mean mortality of snow gum seedlings exceeds recruitment — seedlings can germinate in warm summers but rarely survive their first winter. This makes the treeline a “dynamic equilibrium”: it is not an impenetrable barrier but a zone where, under current conditions, deaths consistently exceed successful establishments. Mild summers allow occasional establishment attempts above 1,800 m, but the combination of abiotic stresses prevents any cohort from surviving to maturity.
Marking criteria. 1 mark — correctly identifies and explains temperature (short growing season limits photosynthesis/carbohydrate accumulation). 1 mark — correctly identifies and explains at least one of: wind (desiccation/physical damage) or soil (thin, frost heave). 1 mark — connects temperature to enzyme activity from Module 1 (optimal temperature, reduced metabolic rate at low temperatures). 1 mark — explains dynamic equilibrium: mortality exceeds recruitment; treeline is not fixed but reflects a balance where germination can occur but survival to maturity does not, under current conditions.
Section 3 · Extended response · 6 marks · Band 5–6
Sample response. Temperature is the primary limiting factor for snow gum recruitment above 1,800 m: the growing season is currently too short for seedlings to survive winter, and this is the factor that would be most directly relaxed by a 2°C warming. A longer frost-free period (potentially 2–4 additional weeks per year) would allow more carbohydrate accumulation, increase seedling survival rates and shift the zone of physiological stress upward — supporting the prediction of an upward treeline shift. However, evaluating the prediction requires considering whether temperature is the only factor that changes, and whether 150–200 m is the right magnitude. Regarding other abiotic factors: wind speed and soil thickness do not change with temperature in the short term, so these factors would remain limiting at the new upper boundary, potentially slowing or capping the upward shift. Soil development at newly exposed subalpine surfaces above the current treeline is slow (decades to centuries), meaning the mechanical and nutrient support for trees would not immediately be available 200 m higher. This suggests the prediction of a full 150–200 m shift may be an overestimate in the short term (decades), though achievable over centuries as soil develops. Regarding ecological consequences that complicate the prediction: below the shifted treeline, alpine herbfields and bogs would be invaded by snow gum woodland, reducing habitat area for endemic species such as the mountain pygmy possum (Burramys parvus), which requires herbfield and rock-heap habitat as well as reliable snow cover for hibernation insulation. Bogong moth numbers may also decline if their breeding habitat (subalpine areas with moisture from snowmelt) diminishes, compounding pressures on the possum via a biotic pathway. Evaluative conclusion: the prediction that a 2°C warming shifts the treeline upward is directionally sound — temperature relaxation will increase snow gum recruitment above 1,800 m. However, 150–200 m is likely an overestimate in the short term because soil, wind and biotic competition from other eucalypt species (e.g. E. delegatensis expanding from lower elevations) will slow the shift. The prediction also underestimates the ecological disruption below the treeline, where alpine community composition changes may be more immediate and severe than the treeline position itself suggests.
Marking criteria. 1 mark — correctly identifies temperature as the primary limiting factor and justifies (short growing season limits seedling survival/carbohydrate accumulation). 1 mark — explains how 2°C warming alters this primary factor (longer growing season, increased recruitment, upward shift of optimal zone). 1 mark — assesses at least two other abiotic factors (wind, soil development, or changed precipitation/snow cover) and explains whether/how they moderate the treeline shift. 1 mark — considers a biotic/ecological consequence that complicates the prediction (e.g. competition from invading eucalypts, loss of mountain pygmy possum habitat, phenological mismatch with bogong moths, or loss of alpine herbfield). 1 mark — reaches an explicit evaluative conclusion on whether the 150–200 m prediction is an overestimate, underestimate or reasonable approximation, with reasoning. 1 mark — quality of argument: response is well-structured, uses correct terminology (tolerance range, limiting factor, optimal zone, dynamic equilibrium, fundamental/realised niche, or phenology) and maintains an evaluative (not merely descriptive) stance throughout. Award only if four or more of the preceding criteria are met.