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Secondary 4 · Biology
History of the Earth and of life · Geological time

Dating Methods

At a quarry in Santo Domingo, a Biology teacher shows her students a rock wall with layers and a coral fossil embedded in it. Two questions come up right away: in what order did everything form? and how many years ago? The first is answered by relative dating; the second, by absolute dating. Neither is enough on its own: the history of the Earth is reconstructed by combining both.

Fossils: witnesses of the past

A fossil is any remain or trace of a living thing from the past preserved in rock or in another material, such as amber. Dominican amber, with insects trapped in it millions of years ago, is one of the most famous in the world.

Type of fossil What it is What information it provides
Hard remains Bones, teeth, shells, mineralized wood The organism's shape and size, and its diet
Tracks or ichnofossils Footprints, trails, burrows How the animal moved and lived
Molds Impression of the shell or bone in the sediment The organism's external shape
Coprolites Fossilized droppings Diet
Inclusions in amber Insects, plants, or air bubbles trapped in resin Complete organisms and the environment of the time

Organisms with soft bodies (jellyfish, worms) hardly ever fossilize: they decompose or are eaten before being buried, and they have no hard parts to mineralize.

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Define fossil and name three different types of evidence that can become fossilised (hard remains, tracks or ichnites, moulds, coprolites, inclusions in amber),…

Define fossil and name three different types of evidence that can become fossilised (hard remains, tracks or ichnites, moulds, coprolites, inclusions in amber), explaining what information each type provides.

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Explain what the fossilisation process consists of (rapid burial, mineralisation of the hard parts) and discuss why soft-bodied organisms (jellyfish, worms) rarely…

Explain what the fossilisation process consists of (rapid burial, mineralisation of the hard parts) and discuss why soft-bodied organisms (jellyfish, worms) rarely appear as fossils.

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Relative dating: the stratigraphic principles

On the wall of a quarry we see three layers of rock stacked up and a vertical crack running through them: how can we tell what happened first without measuring any date?

Example: the order in which three layers were deposited is relative. The age of a lava flow, calculated in millions of years, is absolute.

Cross section with three horizontal layers (slates, conglomerate, and sandstones) cut by an inclined igneous vein, which, since it cuts all of them, is younger than they are. igneous vein 3rd, sandstones 2nd, conglomerate 1st, slates the vein cuts everything: it is the youngest

Unconformities

When an area is uplifted and eroded, the lower strata fold and wear down, and then horizontal strata are deposited on top. This structure is an angular unconformity. The contact surface represents a hiatus or stratigraphic gap: a span of time, sometimes millions of years, with no record, because there was erosion instead of sedimentation.

The order of events is: deposition of the lower strata → folding → erosion → new deposition of the horizontal strata.

When the series is overturned

Sometimes the strata appear upside down (for example, older fossils on top of more recent ones). Overturned folds and thrusts (a reverse fault that pushes old rocks on top of younger ones) can invert a series. It is detected by clues such as the polarity of sedimentary structures (ripple marks, mud cracks, or graded bedding reversed) and by fossils out of order.

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Explain the difference between relative dating and absolute dating, and give an example of a geological event that can be dated using each type of method.

Explain the difference between relative dating and absolute dating, and give an example of a geological event that can be dated using each type of method.

Solve
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State the law of superposition of strata and apply it to the quarry sequence in the diagram (layers A, B, and C). Which is the oldest layer and what environmental change…

State the law of superposition of strata and apply it to the quarry sequence in the diagram (layers A, B, and C). Which is the oldest layer and what environmental change does the sequence suggest?

C B A silts with fossil roots sands without fossils clays with marine remains
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In a cross-section, a series of horizontal strata is intersected by an igneous dyke, all of which is in turn cut by a fault. Applying the principles of cross-cutting…

In a cross-section, a series of horizontal strata is intersected by an igneous dyke, all of which is in turn cut by a fault. Applying the principles of cross-cutting relationships and superposition, list in order from oldest to newest: strata, dyke, and fault, justifying each step.

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Folded, eroded strata can be seen in an outcrop with horizontal strata above them. State the name of this structure, order the events that formed it (sedimentation,…

Folded, eroded strata can be seen in an outcrop with horizontal strata above them. State the name of this structure, order the events that formed it (sedimentation, folding, erosion, and renewed sedimentation), and explain what the "hiatus" or time gap represents.

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In an outcrop, from bottom to top, one can see: metamorphic slates, an eroded surface with slate pebbles at the base of a conglomerate, horizontal sandstones and,…

In an outcrop, from bottom to top, one can see: metamorphic slates, an eroded surface with slate pebbles at the base of a conglomerate, horizontal sandstones and, cutting across everything, an igneous dyke. Order the geological events from oldest to most recent and justify each relationship (superposition, cross-cutting, included clasts).

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Index fossils and correlation between sections

Two distant geological sections, A and B, with strata of different thickness. In both, a stratum appears with the same index fossil (an ammonite), which makes it possible to correlate them as strata of the same age even though they are not connected. no visible physical connection same index fossil (ammonite) → strata of the same age section A section B
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What is an index fossil (or characteristic fossil)? State the three requirements that a good index fossil must meet and explain why human beings cannot serve as such to…

What is an index fossil (or characteristic fossil)? State the three requirements that a good index fossil must meet and explain why human beings cannot serve as such to date ancient rocks.

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Explain the principle of faunal identity and how it allows strata from two quarries hundreds of kilometers apart to be correlated, indicating which type of fossils serve…

Explain the principle of faunal identity and how it allows strata from two quarries hundreds of kilometers apart to be correlated, indicating which type of fossils serve best for that task.

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In a cross-section, a stratum with trilobite fossils appears above another with ammonoids, the reverse of what the geological time scale indicates. Explain which two…

In a cross-section, a stratum with trilobite fossils appears above another with ammonoids, the reverse of what the geological time scale indicates. Explain which two tectonic processes can invert a series of strata (overturned folds, thrust faults) and what clues in the field reveal the inversion.

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Absolute dating: radioactive decay

A sample with 1,000 radioactive atoms drops to 500 after 10 days, 250 after 20, and 125 after 30, regardless of pressure or heat. How does this unchanging rate make it possible to calculate the age of a rock?

Imagine 100 coins. In each round you remove half: 50 are left, then 25, then 12.5… Each round is one half-life. By counting how many "rounds" have gone by from what is left of the isotope, you get the age. Radioactive isotopes are these clocks.

Exponentially decreasing curve of the radioactive isotope: after one half-life 50 % remains and after two half-lives 25 %. time % isotope 100 50 1 half-life 25 2 half-lives

The daughter/parent ratio

Sometimes you are not given what is left of the isotope, but how many "daughter" atoms (the product of the decay) there are for each "parent" atom that survives. Each atom that decays becomes a daughter atom, so parent + daughter always equals the initial total.

Which isotope for which sample

  • C-14 (half-life $5{,}730$ years): organic material (wood, bone, charcoal). It reaches back about $50{,}000$ years; after that, no measurable signal is left.

  • For rocks millions of years old, isotopes with a much longer half-life are used, found in minerals of igneous rocks. The calculation is the same: counting half-lives.

What about sedimentary rocks?

Sedimentary rocks hold almost the whole history of life, but they are rarely dated directly: their grains are fragments of older rocks, and radiometry marks when the mineral crystallized (the event that sets the clock to zero, such as the cooling of a magma), not when the sediment was deposited. This is solved by dating igneous rocks interbedded with them (lava flows, volcanic ash) or dikes: the stratum is bracketed between a maximum and a minimum age.

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Explain what the half-life of a radioactive isotope is using the example of a pile of $100$ coins from which you remove half in each round, and why this regularity turns…

Explain what the half-life of a radioactive isotope is using the example of a pile of $100$ coins from which you remove half in each round, and why this regularity turns radiometric isotopes into geological "clocks".

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Discuss why sedimentary rocks are the great archive of the history of life even though they can rarely be dated directly by radiometric methods, and indicate how this…

Discuss why sedimentary rocks are the great archive of the history of life even though they can rarely be dated directly by radiometric methods, and indicate how this problem is solved using intercalated igneous rocks.

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Carbon-14 has a half-life of $5\,730$ years. An archaeological wood sample retains a quarter of the $\text{C-14}$ it had when the tree died. Calculate the age of the…

Carbon-14 has a half-life of $5\,730$ years. An archaeological wood sample retains a quarter of the $\text{C-14}$ it had when the tree died. Calculate the age of the sample, explaining your reasoning.

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Carbon-14 has a half-life of $5\,730$ years. A fossil tissue retains $1/16$ of the $\text{C-14}$ it had when alive. Calculate the age of the fossil, showing the number…

Carbon-14 has a half-life of $5\,730$ years. A fossil tissue retains $1/16$ of the $\text{C-14}$ it had when alive. Calculate the age of the fossil, showing the number of half-lives elapsed and the final result.

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A research team analyzes the skeletal remains of a mammal found in a karst cave. Laboratory A extracts collagen from inside the bone and detects that it retains…

A research team analyzes the skeletal remains of a mammal found in a karst cave. Laboratory A extracts collagen from inside the bone and detects that it retains $12.5\ \%$ ($1/8$) of the initial $^{14}\text{C}$ activity. Laboratory B analyzes a carbonate crust that externally coated the bone and measures $50\ \%$ of the initial $^{14}\text{C}$.

  1. a) Calculate the numerical age yielded by each laboratory (half-life of $^{14}\text{C} = 5\,730$ years).
  2. b) Justify which of the two results is reliable for determining when the animal died and explain what geochemical process caused the error in the other sample.
  3. c) A team member proposes using radiocarbon to date a $1.2$-million-year-old volcanic tuff located at the cave entrance. Demonstrate mathematically why this is unfeasible and propose which alternative isotopic method they should use.
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To date a sandstone layer containing fossil footprints of early tetrapods, a student separates muscovite (potassium mica) crystals from the sediment itself. After…

To date a sandstone layer containing fossil footprints of early tetrapods, a student separates muscovite (potassium mica) crystals from the sediment itself. After measuring that $25\ \%$ of the original $^{40}\text{K}$ remains ($T_{1/2} = 1\,250$ Ma), they conclude that the footprints are $2\,500$ million years old (Precambrian).

  1. a) Refute the student's conclusion: what physical event resets the K-Ar clock to zero, and what are you actually dating when analyzing detrital clasts from a sandstone?
  2. b) In the same stratigraphic series, a lava flow is observed intercalated below the sandstone layer, and a volcanic dyke cuts across both the lava and the sandstone. Design a procedure to constrain the maximum and minimum age of the fossil-bearing sediment using these igneous bodies.
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In a marine basin, three outcrops correlated by the same ammonoid fossil species with a short biostratigraphic range are studied: Column A: the ammonoid-bearing bed is…

In a marine basin, three outcrops correlated by the same ammonoid fossil species with a short biostratigraphic range are studied:

  • Column A: the ammonoid-bearing bed is intercalated between a lower volcanic ash of $115$ Ma and an upper one of $110$ Ma.

  • Column B: the fossil-bearing bed is cross-cut by a basaltic dyke dated at $112$ Ma, but this dyke does not affect the overlying strata.

  • Column C: a researcher claims to have obtained a radiometric age of $114$ Ma by directly analyzing the calcareous cement of the fossil-bearing bed.

  1. a) Deduce the most precise and rigorous chronological interval for the existence of this ammonoid by combining the valid data from columns A and B.
  2. b) Evaluate the validity of the datum from Column C, justifying whether or not the cement of a sedimentary rock meets the requirements of the radiometric method.
  3. c) Predict how the time constraint for the species would change if a detailed analysis proved that the igneous structure in Column B is not a discordant dyke, but an intercalated and concordant submarine lava flow.
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A laboratory analyzes zircon crystals from a granitic pluton using the decay of $^{235}\text{U}$ to $^{207}\text{Pb}$ ($T_{1/2} = 704$ Ma). a) In an unaltered sample,…

A laboratory analyzes zircon crystals from a granitic pluton using the decay of $^{235}\text{U}$ to $^{207}\text{Pb}$ ($T_{1/2} = 704$ Ma).

  1. a) In an unaltered sample, the isotopic ratio shows that for every remaining $^{235}\text{U}$ atom, there are $7$ accumulated $^{207}\text{Pb}$ atoms. Calculate the number of half-lives that have elapsed and the crystallization age of the granite.
  2. b) In another sample taken from a shear zone with strong hydrothermal alteration, a ratio $^{207}\text{Pb}/^{235}\text{U} = 1$ ($50\ \%$ of original uranium) is measured. A geologist claims that this area of the pluton crystallized $1\,400$ Ma later. Refute their hypothesis by explaining what disruption of the closed system has occurred.
  3. c) Demonstrate why this isotopic pair is useless for dating a flint handaxe from a $100\,000$-year-old Paleolithic site: estimate what infinitesimal percentage of $^{235}\text{U}$ would have decayed and explain the resulting analytical problem.
Solve

Combining and calibrating methods

Comparison between the rings of a trunk, where each ring is one year and its thickness reflects the climate, and the varves of a lake, where each pair of a light summer layer and a dark winter layer is one year. rings of a tree 1 ring = 1 year wide ring: favorable year narrow ring: unfavorable year varves of a lake water light layer (summer) dark layer (winter) 1 light + 1 dark = 1 varve = 1 year oldest at the bottom

Uranium series: dating a stalagmite

Caves, like those in the Los Haitises region, hold speleothems (stalagmites, stalactites) formed by carbonate that precipitates from dripping water. That carbonate can be dated with another radioactive clock: the uranium series.

Calibrating C-14

Stable isotopes: what did it eat?

Not all isotopes are radioactive. Carbon has two stable forms, C-12 and C-13, which do not decay. Laboratories measure the proportion of C-13 in a bone and express it as δ¹³C (read "delta C-13," in ‰, per mil). Because foods leave a different "signature" in the body, δ¹³C reveals the diet.

Diet Approximate δ¹³C
Land plants and animals (fruits, herbivores) around $-21\ ‰$
Marine shellfish and fish around $-13\ ‰$
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Explain what dendrochronology consists of: what each ring of a tree records, how series from trees of different ages are overlapped to extend the chronology back…

Explain what dendrochronology consists of: what each ring of a tree records, how series from trees of different ages are overlapped to extend the chronology back thousands of years, and what climatic information the width of the rings contains.

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Varves are pairs of light and dark laminae deposited each year in certain lakes. Explain what causes this seasonal alternation, how they are used for dating, and why…

Varves are pairs of light and dark laminae deposited each year in certain lakes. Explain what causes this seasonal alternation, how they are used for dating, and why lake sediments are climatic "archives" comparable to ice cores.

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Atmospheric $^{14}\text{C}$ concentration is not constant over time: atmospheric nuclear testing (1955-1963) nearly doubled $^{14}\text{C}$ ("bomb effect"), whereas…

Atmospheric $^{14}\text{C}$ concentration is not constant over time: atmospheric nuclear testing (1955-1963) nearly doubled $^{14}\text{C}$ ("bomb effect"), whereas industrial fossil fuel emissions inject huge volumes of $\text{CO}_2$ completely devoid of $^{14}\text{C}$ ("Suess effect").

  1. a) If you date the wood of a tree felled in 1965 using the standard formula without calibration, will its apparent radiocarbon age be from the past or "from the future" (negative)? Justify your deduction based on the measured specific activity.
  2. b) Predict what error (artificial aging or rejuvenation) dating a lichen currently growing next to a highway with heavy diesel traffic would yield. Reason through the isotopic exchange involved.
  3. c) Justify how dendrochronology allows the construction of a calibration curve that resolves these discrepancies for the last $12\,000$ years.
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In a cave in Cantabria containing fossil human remains, the following stratigraphic sequence is recorded from top to bottom: Level 1: sediments with normal magnetic…

In a cave in Cantabria containing fossil human remains, the following stratigraphic sequence is recorded from top to bottom:

  • Level 1: sediments with normal magnetic polarity. An intercalated stalagmite is dated by uranium series to $0.45$ Ma.

  • Level 2: sediments with reversed polarity containing a rich lithic industry and bone remains.

  • Level 3: basal sediments with normal magnetic polarity.

Knowing that the Brunhes-Matuyama reversal (from normal to reversed going back in time) occurred $0.78$ Ma ago and the Matuyama-Gauss (from reversed to normal) $2.58$ Ma ago:

  1. a) Constrain the time interval in which the hominins of Level 2 could have lived based on the combined data.
  2. b) A team member suggests that the remains of Level 2 are $600\,000$ years old. Formally refute their claim based on the observed magnetic polarity.
  3. c) If a narrow band of normal polarity barely a few centimeters thick were to appear in the center of Level 2, does it force the entire chronology to change, or what short-duration geomagnetic phenomenon (subchron or event) would it represent within Matuyama?
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In a coastal necropolis, two human skeletons found in the same burial level are dated: Individual A: $4\,150 \pm 30$ years BP. Individual B: $4\,600 \pm 40$ years BP.…

In a coastal necropolis, two human skeletons found in the same burial level are dated:

  • Individual A: $4\,150 \pm 30$ years BP.

  • Individual B: $4\,600 \pm 40$ years BP.

Stable isotope analysis reveals that individual A based their diet on terrestrial fruits and herbivores ($\delta^{13}\text{C} = -21\ \text{‰}$), whereas individual B consumed predominantly shellfish and marine fish ($\delta^{13}\text{C} = -13\ \text{‰}$).

  1. a) Check whether the two standard deviation intervals ($2\sigma$, $95\ \%$ margin) of both individuals overlap.
  2. b) Formulate a hypothesis that explains the nearly $500$-year discrepancy based on the "marine reservoir effect". Which of the two dates is closer to the actual time of burial?
  3. c) If instead of extracting collagen, the mineral bone carbonate (hydroxyapatite) fossilized in a wet calcareous soil had been dated, predict and justify the direction of the error (apparent aging or rejuvenation) that diagenesis would cause.
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A team presents the following proposal to date various elements of a tectonic basin: 1. Date the pottery from a superficial layer using radiocarbon by analyzing the…

A team presents the following proposal to date various elements of a tectonic basin:

  1. Date the pottery from a superficial layer using radiocarbon by analyzing the silicon and aluminum of the fired clay.

  2. Date a basaltic volcanic flow using dendrochronology by measuring the concentric alteration bands of its gas vesicles.

  3. Date the time of sedimentation of a Precambrian schist using K-Ar applied to micas formed during regional metamorphism.

  1. a) Detect and explain the conceptual or methodological flaw that invalidates each of the three proposals.
  2. b) Design a valid methodological alternative for each of the three materials, specifying the appropriate analytical method and what physical or chemical event exactly represents the resetting of the clock.
  3. c) If in a wooden beam from the site you count $95$ growth rings but do not know the dendrochronological curve of the region, explain why you cannot assign it an absolute calendar date and how it would be complemented with radiocarbon to place it in time.
Solve

Back to the beginning: the order of the layers in the quarry is given by relative dating, and the age in years of the amber or of a lava is given by absolute dating; together they tell the complete story.

Summary

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