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BAC1 tech · Biology, Geology and Environmental Sciences
History of the Earth and of life · Geological time

Dating methods

A geologist looking at a rock section faces two different questions: in what order did everything happen? and how many years ago did it happen? The first question is answered by relative dating; the second, by absolute dating. Neither is enough on its own: the complete history of the Earth is reconstructed by combining both.

Before you start, make sure you know: Geological sections (4th ESO)
Before you start, make sure you know: Rocks and the rock cycle (1st ESO)

Relative dating: the stratigraphic principles

On the wall of a gorge we see three layers of rock stacked horizontally and crossed by a vertical crack: how can we know for certain what happened first without measuring any numerical date?

Stratigraphic section with three horizontal layers (slates, conglomerate and sandstones) cut by an inclined igneous dyke, which, since it cuts all of them, is younger than they are. igneous dyke 3rd, sandstones 2nd, conglomerate 1st, slates the dyke cuts everything: it is the most recent
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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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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 there is a stratum with the same index fossil (an ammonite), which allows them to be correlated 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 kilometres 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 kilometres 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

In the laboratory we find that a sample with $1\,000$ radioactive atoms falls to $500$ after $10$ days, $250$ after $20$ days and $125$ after $30$ days, regardless of pressure or heat: how does this unchanging rate make it possible to calculate the exact age of a rock?

Animation of the decreasing exponential curve of the radioactive parent isotope: a point moves along the curve and, on reaching the first half-life (50 %) and the second (25 %), the dashed lines and their labels appear; then everything returns to the start. time % isotope 100 50 1 half-life 25 2 half-lives
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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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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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Combining and calibrating methods

Comparison between the growth rings of a cut tree trunk, where each ring is one year and its thickness reflects the climate, and the varves of a lake, where each pair of summer and winter layers is one year. tree rings 1 ring = 1 year wide ring: favourable year narrow ring: unfavourable year lake varves water older summer layer thicker 1 varve = 1 year (summer + winter) winter layer thin, clay
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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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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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Summary

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