Evidence from Fossils
In 1861, quarry workers in Germany split a slab of limestone and found a creature with the feathers of a bird and the teeth, claws and bony tail of a reptile. Archaeopteryx was a fossil caught mid-transition, and it became one of evolution's most famous pieces of evidence. This lesson is about how rocks and the bones inside them record the changing history of life.
Orient yourself
Make a prediction, scan the goals and the key terms, and see which misconception this lesson is built to fix.
Before You Read
warm-upYou dig into a cliff and find fossils in horizontal layers of sedimentary rock, one above another.
Before reading: which fossils are oldest, those near the top or those near the bottom, and what assumption are you making to decide? Write your answer.
Learning Intentions
goalsKnow
- What transitional fossils and fossil assemblages are
- How relative dating orders rock layers by age
- The principle of superposition
Understand
- Why transitional fossils support gradual change in life forms
- How assemblages and index fossils correlate distant rock layers
- Why relative dating shows order but not exact age
Can Do
- Order fossils in a rock sequence using superposition
- Analyse fossil evidence for past changes in life forms
- Distinguish relative dating from absolute dating
Scan these before reading
vocabMatch each term to its meaning: use the Key Terms card above.
- Fossil
- Transitional fossil
- Fossil assemblage
- Relative dating
- Superposition
- In undisturbed sedimentary rock, lower layers are older than those above
- The collection of different fossils found together in one rock layer
- Preserved remains, impression or trace of a once-living organism
- Working out age order without giving an exact numerical age
- A fossil with features intermediate between an ancestral group and its descendants
Misconceptions To Fix
watch outTransitional Fossils, Caught Mid-Change
Fossils with a mix of old and new features
Core Content
Transitional Fossils, Caught Mid-Change
+5 XPFossils with a mix of old and new features
If life forms have changed over time, we should expect to find fossils that show a blend of features from an ancestral group and its descendants, and we do.
A transitional fossil is a fossil that displays features intermediate between an ancestral group and a later, derived group, providing direct palaeontological evidence of change in life forms over time. The classic example, Archaeopteryx, has feathers and a wishbone like a bird but also teeth, clawed fingers and a long bony tail like a reptile.
Other well-documented examples include Tiktaalik (between fish and four-legged amphibians) and a long sequence of fossil whales showing the gradual loss of hind limbs as ancestors moved from land to sea. Each transitional fossil is exactly the sort of intermediate form the theory of evolution predicts should exist.
Pause, copy the highlighted definition and the Archaeopteryx example into your book.
Australian transitional and assemblage evidence worth naming. The Riversleigh World Heritage fossil deposits in north-western Queensland preserve successive assemblages of Australian mammals, birds and reptiles across roughly 25 million years, including forms intermediate between earlier and later members of several marsupial families. The Naracoorte Caves in South Australia, the other half of the same World Heritage listing, preserve a continuous record of vertebrate assemblages spanning several hundred thousand years, which is how the composition of Australian faunas before and after the megafauna extinctions is known.
A fossil showing a mix of ancestral and derived features is called a _____ fossil.
Relative Dating and Superposition
Ordering life's history layer by layer
Relative Dating and Superposition
+5 XPOrdering life's history layer by layer
We just saw that transitional fossils record change. That raises a question: how do we know which fossils are older and which are younger? This card answers it → through relative dating and the principle of superposition.
In undisturbed sedimentary rock, sediment piles up over time, so the deeper you dig the further back in time you go, which lets us put fossils into an age order.
Text description
- Five undisturbed rock layers. Fossils are shown in three of them: a leaf in the top layer, a fish in the middle layer and a shell in the bottom layer.
- The top layer is the youngest; the bottom layer is the oldest.
- Deeper = older.
Relative dating establishes the age order of fossils, not their exact age. Its foundation is the principle of superposition: in undisturbed sedimentary rock, lower layers are older and upper layers are younger. Comparing fossils up a sequence therefore shows the order in which different life forms appeared, changed and disappeared.
Distinctive, widespread, short-lived index fossils let geologists match layers of the same age in rocks far apart, building a consistent timeline of past life across the globe.
Relative dating gives the age order (not exact age) of fossils. By the principle of superposition, lower sedimentary layers are older than higher ones, so reading a sequence from the bottom up shows the order in which life forms changed. Index fossils correlate same-age layers in distant locations.
Pause, copy the highlighted superposition rule into your book and label the diagram's oldest and youngest layers.
Where the rule was written into the global timescale, and it was written here. The Ediacara Member in the Flinders Ranges of South Australia preserves an assemblage of soft-bodied organisms older than the first shelly animals. Its position beneath those younger assemblages, read by superposition, is why the Ediacaran Period was defined in 2004 with its global type section in South Australia, the first new geological period ratified in more than a century. Relative dating is not a classroom simplification of "real" dating; it is the reasoning the global timescale is built on.
In an undisturbed sequence of sedimentary rock, which layer contains the oldest fossils?
Apply it: Order the Strata
Work the activity in your own book before you read on. This is the first point where you are on your own.
Activity 1
Order the Strata
Pattern, Apply superposition to data
A cliff face has four undisturbed layers. Layer 1 is at the surface, Layer 4 at the base. The fossils found are: Layer 1, modern fish; Layer 2, early amphibian; Layer 3, lobe-finned fish; Layer 4, simple marine invertebrates.
In your book: (a) list the fossils from oldest to youngest, (b) state the principle you used, and (c) explain what this sequence shows about changes in life forms over time.
Fossil Assemblages and the Bigger Picture
Reading whole communities, and the limits of the record
Fossil Assemblages and the Bigger Picture
+5 XPReading whole communities, and the limits of the record
We just ordered fossils by depth. That raises a question: what can the whole group of fossils in a layer tell us, and how reliable is the record? This card answers it → fossil assemblages reconstruct past environments, but the record is incomplete.
Looking at all the fossils preserved together in a layer reveals not just single species but whole communities and environments of the past.
A fossil assemblage is the set of different fossils found together in one rock layer. Because it captures many species at once, an assemblage reveals what kind of community and environment existed at that time, for example a layer rich in coral and shellfish indicates a warm shallow sea. Comparing assemblages up a sequence shows how whole communities, not just individual species, changed over time.
The fossil record is powerful but incomplete: fossilisation is rare and favours hard-bodied organisms in the right conditions, so soft-bodied life and many transitional forms are under-represented. This is why palaeontological evidence is always combined with other lines of evidence, relative dating, index fossils, and later molecular data, to build a reliable picture of past change.
A fossil assemblage (all fossils in one layer) reconstructs a past community and environment; comparing assemblages up a sequence shows how communities changed over time. The fossil record is incomplete because fossilisation is rare, so it is combined with relative dating, index fossils and molecular evidence.
Add the assemblage definition and the "record is incomplete" point to your notes before the check below.
Relative dating gives the age order of fossils but not their exact numerical age.
Gaps in the fossil record prove that transitional forms never existed.
A fossil assemblage can be used to reconstruct the community and environment of a past time.
See where it lands in the real world
Fossils that find oil, and warn of mass extinction
Fossils that find oil, and warn of mass extinction
Relative dating and index fossils are not just academic. Petroleum geologists use fossil assemblages to identify rock layers likely to hold oil and gas, correlating cores from boreholes thousands of kilometres apart. The same fossil record also documents Earth's five mass extinctions, sudden, global changes in the assemblages preserved in the rock, giving today's scientists a baseline against which to measure the current human-driven biodiversity crisis you will study across Year 12.
Odd one out: three of these follow from the card above. Which one does not?
Explain how the principle of superposition allows a fossil sequence to be placed in order, and explain what relative dating can and cannot establish.
Explain means cause and effect, and the second clause asks for a limit. A question that asks what a method cannot do is testing whether you understand the method rather than just its name.
5 marks. State the principle and why it holds, apply it to a sequence, state what that establishes, then state clearly what it does not, then say what supplies the missing part.
The principle of superposition states that in an undisturbed sequence of sedimentary rock, each layer is younger than the layer beneath it and older than the layer above. It holds because sediment is deposited from above, layer upon layer, so a layer cannot be laid down beneath one that already exists.
Because a fossil is formed within the layer in which the organism was buried, the fossil shares the age relationships of its layer. If species A is found only in a lower layer, species B in a middle layer and species C in an upper layer, then A lived before B, which lived before C. The vertical order of the rock therefore gives the chronological order of the organisms, and a change in form from A to C through B is evidence of change in life forms over time.
The conclusion depends on the sequence being undisturbed. Folding, faulting or overturning can invert layers, intrusions can introduce younger rock into older, and erosion can remove layers entirely, leaving an unconformity where time is missing from the record with nothing to mark it. Geologists therefore check for these before reading a sequence as a straight chronology.
Relative dating establishes order only, not age. It can show that A is older than B, but it cannot say by how much, nor give either an age in years. Two layers a centimetre apart may represent a year or a hundred thousand years, because deposition rate varies with conditions and is not recorded in the layer itself. It follows that relative dating alone cannot measure the rate of evolutionary change, which is precisely the quantity the gradualism and punctuated equilibrium models disagree about.
Absolute dating supplies what relative dating cannot, by measuring the decay of radioactive isotopes in the rock or in associated material to give an age in years with a stated uncertainty. The two methods are used together: superposition establishes the order and shows the sequence is coherent, while absolute dates anchor that order to a timescale, so that rates of change can be estimated rather than merely inferred.
The principle of superposition states that in an undisturbed sequence of sedimentary rock each layer is younger than the layer beneath it and older than the one above, and it holds because sediment is deposited from above, layer upon layer, so a layer cannot be laid down beneath one that already exists. Because a fossil forms within the layer in which the organism was buried, it shares the age relationships of that layer, so if species A occurs only in a lower layer, species B in a middle layer and species C in an upper layer, then A lived before B which lived before C, and the vertical order of the rock gives the chronological order of the organisms, with a change in form from A through B to C constituting evidence of change in life forms over time. The conclusion depends on the sequence being undisturbed: folding, faulting or overturning can invert layers, intrusions can place younger rock within older, and erosion can remove layers entirely, leaving an unconformity where time is missing from the record with nothing to mark it, so geologists check for these before reading a sequence as a straight chronology. Relative dating establishes order only, and not age: it can show A is older than B but not by how much, and cannot give either an age in years, because two layers a centimetre apart may represent a year or a hundred thousand years, deposition rate varying with conditions and not being recorded in the layer itself. It follows that relative dating alone cannot measure the rate of evolutionary change, which is exactly the quantity over which the gradualism and punctuated equilibrium models disagree. Absolute dating supplies what relative dating cannot, measuring the decay of radioactive isotopes in the rock or associated material to give an age in years with a stated uncertainty, and the two are used together, superposition establishing the order and showing the sequence coherent while absolute dates anchor it to a timescale so that rates of change can be estimated rather than merely inferred.
Analyse why the conditions required for fossilisation mean the fossil record is a biased sample of past life rather than simply an incomplete one.
Analyse asks you to identify components and their relationships. The question also draws a sharp distinction, between incomplete and biased, and the whole answer depends on respecting it.
5 marks. Define the distinction, list the conditions fossilisation requires, show that each condition favours particular organisms, then draw the consequence for inference.
An incomplete sample contains less than everything but in the same proportions as the original, so conclusions drawn from it still apply to the whole. A biased sample over-represents some parts and under-represents others, so conclusions drawn from it may not apply to the whole even if the sample is large. The fossil record is both, and the bias is the more serious problem.
Fossilisation is rare and requires a particular combination: rapid burial in sediment before the remains are scavenged or decay, conditions that slow decomposition such as low oxygen, and usually the presence of hard tissue such as bone, shell or wood that resists breakdown long enough to be mineralised. The remains must then survive geological time without being destroyed by heat, pressure or erosion, and finally must be exposed and found.
Each condition selects non-randomly. The hard-tissue requirement means organisms with bones or shells are heavily over-represented, while soft-bodied organisms such as worms, jellyfish and most microorganisms are almost absent regardless of how abundant they were. The rapid-burial requirement favours organisms living in or near environments where sediment accumulates, so marine and floodplain species are over-represented and species from upland, forest or arid environments, where remains are exposed and eroded, are under-represented. The survival and exposure requirements add further bias towards younger rocks, since older rock has had longer to be destroyed, and towards regions that are geologically accessible and well studied.
The consequence is that patterns in the record cannot be read directly as patterns in past life. An apparent absence of a group may mean it was absent, or that it was soft-bodied, or that it lived where fossils do not form. An apparent sudden appearance may be a real origin or the point at which a lineage acquired hard parts or entered a depositional environment. The record understates past diversity, and it understates it unevenly.
The bias is a reason for care rather than for dismissing the evidence. It can be partly corrected by comparing like with like, such as comparing marine shelly faunas across time rather than comparing a marine sequence with a terrestrial one, by concentrating on sequences with exceptional preservation where soft tissue is present, and by testing fossil-based conclusions against independent evidence from comparative anatomy and molecular data. A known bias with a known direction can be reasoned about, which is very different from an unknown one.
An incomplete sample contains less than everything but in the same proportions as the original, so conclusions drawn from it still apply to the whole, whereas a biased sample over-represents some parts and under-represents others, so conclusions may not apply to the whole however large the sample. The fossil record is both, and the bias is the more serious problem. Fossilisation is rare and requires a particular combination of conditions: rapid burial in sediment before scavenging or decay, conditions slowing decomposition such as low oxygen, and usually hard tissue such as bone, shell or wood that resists breakdown long enough to mineralise, after which the remains must survive geological time without destruction by heat, pressure or erosion, and must finally be exposed and found. Each condition selects non-randomly. The hard-tissue requirement heavily over-represents organisms with bones or shells while soft-bodied organisms such as worms, jellyfish and most microorganisms are almost absent however abundant they were; the rapid-burial requirement favours organisms in or near environments where sediment accumulates, over-representing marine and floodplain species and under-representing upland, forest and arid ones where remains are exposed and eroded; and the survival and exposure requirements bias the record towards younger rocks, older rock having had longer to be destroyed, and towards regions that are geologically accessible and well studied. The consequence is that patterns in the record cannot be read directly as patterns in past life: an apparent absence of a group may mean it was absent, or soft-bodied, or living where fossils do not form, and an apparent sudden appearance may be a real origin or the point at which a lineage acquired hard parts or entered a depositional environment, so the record understates past diversity and understates it unevenly. This is a reason for care rather than dismissal, and the bias can be partly corrected by comparing like with like, such as marine shelly faunas across time rather than a marine against a terrestrial sequence, by concentrating on sequences with exceptional preservation where soft tissue survives, and by testing fossil-based conclusions against independent evidence from comparative anatomy and molecular data. A known bias with a known direction can be reasoned about, which is very different from an unknown one.
Practise independently
Answer every question in your own words first. The model answers are for checking against, not for copying.
Multiple Choice
+5 XPA fresh set drawn from this lesson's question bank, feedback shown immediately. +5 XP per correct · +25 XP all correct
Pick your answer, then rate your confidence, that tells the system what to drill next.
Short Answer, 12 marks
+5 XPAnalyseBand 5(5 marks) 1. Analyse how transitional fossils, fossil assemblages and relative dating each provide evidence for past changes in life forms.
1 mark each: transitional fossils show intermediate forms · assemblages reconstruct past communities · relative dating/superposition gives age order · links each to "change in life forms" · coherent integrated answer
ApplyBand 4(3 marks) 2. A cliff face has four undisturbed sedimentary layers. From the surface downward the fossils are: modern fish (layer 1), early amphibian (layer 2), lobe-finned fish (layer 3), simple marine invertebrates (layer 4). List the fossils from oldest to youngest, name the principle you used, and state one thing this sequence shows about changes in life forms.
1 mark: correct order, simple marine invertebrates, lobe-finned fish, early amphibian, modern fish · 1 mark: names the principle of superposition and the assumption that the layers are undisturbed · 1 mark: draws a valid conclusion about change over time, for example that vertebrates appear after invertebrates and land forms after aquatic ones
EvaluateBand 5-6(4 marks) 3. "Gaps in the fossil record show that transitional forms never existed." Evaluate this claim, referring to how fossils form and to at least one named transitional fossil.
1 mark: explains why fossilisation is rare and biased toward hard-bodied organisms in particular conditions · 1 mark: concludes that absence of a fossil is not evidence of absence of the organism · 1 mark: names a transitional fossil and states the features that make it intermediate · 1 mark: reaches an overall judgement rejecting the claim, with the reason
Show all answers
Multiple choice
MC answers and full explanations are shown inline as you complete each question. Use the retry button to attempt a fresh set from the lesson bank.
Short Answer Model Answer
Q1 (5 marks): Transitional fossils such as Archaeopteryx display features intermediate between an ancestral group (reptiles) and a derived group (birds), providing direct evidence that one form of life changed into another over time. Fossil assemblages, the set of fossils found together in one layer, reconstruct the community and environment of a past time, so comparing assemblages up a rock sequence shows how whole communities of life forms changed. Relative dating, based on the principle of superposition (lower layers older than higher in undisturbed rock), orders fossils by age without giving exact dates, revealing the sequence in which different life forms appeared, changed and disappeared. Together these palaeontological and geological lines of evidence build a consistent record of past changes in life forms, though the record is incomplete because fossilisation is rare.
Q2 (3 marks): From oldest to youngest: simple marine invertebrates, lobe-finned fish, early amphibian, modern fish [1]. The principle used is superposition, that in undisturbed sedimentary rock the lower layers were deposited first and are therefore older, and it assumes the sequence has not been overturned by folding or faulting [1]. The sequence shows change in life forms over time: invertebrates appear before vertebrates, and a fish with lobed fins occurs below the first four-limbed amphibian, which is the order the theory of evolution predicts for the move from water onto land [1].
Q3 (4 marks): Fossilisation is a rare event. It requires rapid burial in sediment under conditions that prevent decay, and it strongly favours organisms with hard parts such as bones, teeth and shells, so soft-bodied organisms and species living where sediment is not accumulating are heavily under-represented [1]. It follows that the absence of a fossil is evidence about preservation, not about existence: we should expect gaps even if every intermediate form once lived, so a gap cannot show that intermediates never existed [1]. The claim is also contradicted by the fossils we do have. Archaeopteryx carries feathers and a wishbone like a bird together with teeth, clawed fingers and a long bony tail like a reptile, exactly the mixture of ancestral and derived features an intermediate should show, and Tiktaalik and the fossil whale series do the same for other transitions [1]. My judgement is that the claim fails twice over: it misreads absence of evidence as evidence of absence, and it is refuted by the transitional fossils that have in fact been found. What the gaps genuinely show is that the record is incomplete, which is why palaeontological evidence is weighed alongside relative dating, index fossils and molecular data rather than alone [1].
Retrieve and reflect
Do the spaced-review set from memory first, then look back at the prediction you made before you read anything.
Check what actually stuck
A short spaced-review set drawn from this lesson and the lessons before it. Answer from memory first, that is what makes it stick.
Lock it in
bossYou can now analyse how transitional fossils, fossil assemblages and relative dating provide evidence for past changes in life forms. Next lesson moves from rock to molecules: inferring evolutionary relationships from DNA and amino-acid sequences.
↩ Back to focus-area hubHow did your thinking change?
At the start you decided whether the oldest fossils sit near the top or bottom of a cliff. The answer is the bottom, by the principle of superposition, and the assumption you relied on was that the layers are undisturbed. If folding or faulting has overturned the rock, that order can be reversed, which is exactly why geologists check for disturbance before reading a sequence.
If you assumed exact ages could be read straight off the layers, revisit Card 2: relative dating gives order, not a number, absolute (radiometric) dating is needed for that.