Biology  by Bradford
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IB Biology 2025 · Theme A · Unity and diversity

A2.1 Origins of cells (HL). Practice questions with markscheme.

69 original IB-style questions on A2.1, written from the 2025 guide: 32 multiple-choice, 23 short-answer, 8 data-based, 3 extended-response parts, 2 drawing, 1 labelling. This subtopic is additional higher level in its entirety, so below is a 22-mark higher-level practice paper built from them. Hand one out as a class quiz or homework, or sit it yourself and mark against the scheme. Print it, project it, or build a fresh one on the same topic.

What the guide asks for

All 9 statements are additional higher level, so this subtopic is HL only.

  1. A2.1.1HL Conditions on early Earth and the pre-biotic formation of carbon compounds
  2. A2.1.2HL Cells as the smallest units of self-sustaining life
  3. A2.1.3HL Challenge of explaining the spontaneous origin of cells
  4. A2.1.4HL Evidence for the origin of carbon compounds
  5. A2.1.5HL Spontaneous formation of vesicles by coalescence of fatty acids into spherical bilayers
  6. A2.1.6HL RNA as a presumed first genetic material
  7. A2.1.7HL Evidence for a last universal common ancestor
  8. A2.1.8HL Approaches used to estimate dates of the first living cells and the last universal common ancestor
  9. A2.1.9HL Evidence for the evolution of the last universal common ancestor in the vicinity of hydrothermal vents

In the bank for A2.1

  • 32 multiple-choice
  • 23 short-answer
  • 8 data-based
  • 3 extended-response parts
  • 2 drawing
  • 1 labelling
  • 69 higher level only

Every question is original and tagged to a guide statement. See the whole bank →

Make your own

The practice paper

Additional higher level only · 22 marks
Take it online → Build a fresh paper Paper code BbB-EAEEAAAAABQAOiLc
Biology · topic quiz
Higher level · topic practice, not an exam format
35 minutes22 marks

Paper code: this paper was generated, so the code is its recipe. Enter it at biologybybradford.com/exam-maker to rebuild this exact paper and its markscheme.

Covers A2.1 Origins of cells · HL
Name:
1.

Why are alkaline hydrothermal vents considered a plausible setting for the origin of life?

[1]
  1. They contain free oxygen needed by the first aerobic cells
  2. They provide cold, still conditions that stabilize RNA
  3. They provide chemical gradients, mineral catalysts and hydrogen
  4. They allow sunlight to penetrate to the sea floor for photosynthesis
2.

Ultraviolet radiation from the Sun reached the surface of the early Earth far more intensely than it does today. What is the reason for this difference?

[1]
  1. The Earth orbited much closer to the Sun, so far more ultraviolet radiation reached it
  2. The atmosphere of the early Earth was much thinner, because it contained far less carbon dioxide and methane
  3. Methane in the early atmosphere absorbed visible light and re-emitted it as ultraviolet radiation
  4. There was no free oxygen in the early atmosphere, so no ozone layer could form to absorb ultraviolet
3.

Discuss whether a fire should be regarded as living, given that a fire consumes fuel and oxygen, releases energy as heat and light, grows, and spreads by starting new fires.

[3]
4.

Explain how the design of Pasteur's swan-necked flask experiment allowed him to falsify spontaneous generation.

[3]
5.

The last universal common ancestor (LUCA) is the population of cells from which all living organisms descend. LUCA left no fossils, so its date cannot be measured directly; evidence from the rocks sets limits within which it must lie: the age of the Earth, the oldest rocks and crystals that show liquid water existed, the oldest rocks whose carbon has the isotope ratio produced by living cells, and the oldest fossils. The timeline summarises this evidence and the range of current estimates for the date of LUCA.

4.64.03.42.82.2 Time before present / billion years range of estimates for LUCA Earth forms oldest rocks oldest stromatolites (microbial fossils) oldest zircon crystals (liquid water present) oldest carbon with a biological ¹³C signature oxygen accumulates in the atmosphere
(a)State the age of the oldest known fossils of microorganisms.[1]
(b)Deduce, giving a reason from the timeline, the latest date at which LUCA could have existed.[2]
(c)Suggest why LUCA is unlikely to have existed before 4.4 billion years ago.[1]
(d)Deduce, using the timeline, what the evidence implies about how long life has been evolving on Earth compared with the age of the Earth.[3]
6.

Fatty acids are simpler amphipathic molecules than phospholipids and were probably available on the early Earth. A research group shook fatty acids in water at a range of pH values and used microscopy to record the structures formed after 24 hours.

pHStructures formedMean number of vesicles per field of view
6oil droplets only0
7droplets and some vesicles11
8membrane-bound vesicles62
9membrane-bound vesicles58
10micelles (single-layered spheres)3
(a)Describe the relationship between pH and the formation of vesicles.[2]
(b)Explain how amphipathic molecules such as fatty acids can assemble into vesicles without any enzymes.[2]
(c)Outline the significance of vesicle formation for the origin of the first cells.[2]
(d)Suggest one reason why these laboratory results should be applied to the early Earth with caution.[1]

Original practice questions © Biology by Bradford · CC BY-NC-SA 4.0 · Not affiliated with or endorsed by the International Baccalaureate Organization.
Rebuild or edit this exact paper (and its markscheme): biologybybradford.com/exam-maker?code=BbB-EAEEAAAAABQAOiLc

Show the markscheme

Markscheme BbB-EAEEAAAAABQAOiLc

One mark per point; / separates alternative wording within a point, OR separates alternative answers, words in brackets are not required, underlined words are essential. OWTTE = or words to that effect.

1. A2.1.9 [1]
  • C: natural gradients across mineral pores resemble chemiosmosis, with catalysts and reduced chemicals available, conditions suited to early metabolism;
2. A2.1.1 [1]
  • D: ozone forms from free oxygen, which was absent until photosynthesis released it, so nothing absorbed ultraviolet before it reached the surface; A is wrong because the Earth's orbit has not changed significantly; B is wrong because the early atmosphere was rich in carbon dioxide and methane; C describes a process that does not occur;
3. A2.1.2 [3]
  • a fire shows some features associated with life: it uses a source of energy (fuel and oxygen) / it 'grows' / it 'reproduces' by spreading, OWTTE;
  • however, it is not made of cells / has no membrane-bound compartment separating it from its surroundings;
  • it has no genetic material / does not pass information (DNA/RNA) to new fires / new fires are not copies made from a template;
  • it does not carry out metabolism controlled by enzymes / homeostasis / does not respond to stimuli in a regulated way;
  • the smallest unit of self-sustaining life is a cell, so a fire is a chemical process and non-living;

For full marks, at least one point for and one point against. Do not accept 'a fire is not an organism' without a reason.

4. A2.1.3 [3 max]
  • broth was boiled/sterilized, killing any cells already present;
  • the curved (swan) neck admitted air but trapped dust/microbes (in the bend);
  • no growth occurred while the neck was intact, but growth followed when the neck was snapped/broth was tipped into the bend;
  • (so) growth requires entry of pre-existing cells, not air/broth alone / cells only come from pre-existing cells, OWTTE;
5. A2.1.8
  • (a) [1]
    • 3.5 (billion years);

    Accept any value from 3.4 to 3.6 (billion years) read from the timeline.

  • (b) [2]
    • 3.5 billion years ago / no later than the oldest fossils;
    • (because) fossil cells already existed by then, so their common ancestor must be at least as old, OWTTE;

    Accept any value from 3.4 to 3.6 billion years read from the timeline. Accept 3.7 billion years with the biological carbon signature as the reason.

  • (c) [1]
    • there is no evidence of liquid water before the oldest zircons / cells require liquid water, OWTTE;

    Accept: the Earth was too hot / molten.

  • (d) [3]
    • life existed by 3.5 billion years ago (the oldest fossils), and possibly earlier (3.7 billion years from the carbon signature / up to 4.2 billion years from the estimates for LUCA);
    • the Earth formed 4.6 billion years ago, so life has existed for at least 3.5 / 4.6 = about 76 % / about three quarters of the Earth's history;
    • (so) life arose early, within about 1.1 billion years of the Earth forming, and has been evolving for an immense length of time, OWTTE;

    Accept 74 % to 78 %, or ECF from the value given in (a). Accept about 80 % if 3.7 billion years (the carbon signature) is taken as the start of life.

6. A2.1.5
  • (a) [2]
    • vesicles form only in a limited pH range / few or none at pH 6 and pH 10;
    • formation is greatest at (around) pH 8–9 / rises to a peak near pH 8 then falls, OWTTE;
  • (b) [2 max]
    • each molecule has a hydrophilic (head) and hydrophobic (tail) region;
    • tails associate away from water / heads face the water, so bilayers form spontaneously (self-assembly);
    • bilayer sheets close into spheres/vesicles (minimizing exposed edges), OWTTE;
  • (c) [2]
    • provides compartmentalization: an internal chemistry separated from the surroundings;
    • (so) replicating molecules and their products stay together / concentrations can be maintained (a protocell), OWTTE;
  • (d) [1]
    • conditions (pH/temperature/concentrations) of early oceans are uncertain / lab concentrations may be unrealistically high / other molecules present may interfere, OWTTE;

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