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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.

Relative dating: the stratigraphic principles

On the wall of the Grand Canyon 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 dike, which, since it cuts all of them, is younger than they are. igneous dike 3rd, sandstones 2nd, conglomerate 1st, slates the dike cuts everything: it is the most recent

Unconformities

Sometimes tilted or folded strata are cut off by erosion and covered by flat-lying layers. This contact is an angular unconformity, and the missing time is the hiatus. You can see this kind of contact in the Grand Canyon, where tilted rocks lie under the flat Tapeats Sandstone.

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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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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 dike. 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

Fossils and fossilization

A fossil is any preserved evidence of ancient life. Types include hard parts (shells, bones, teeth), tracks and burrows, molds and casts, coprolites (fossil dung, which show diet) and insects trapped in amber (with very fine detail).

Fossilization needs rapid burial, so scavengers and decay do not destroy the remains, and then mineralization of the hard parts. Soft-bodied organisms such as jellyfish and worms have no hard parts and rot quickly, so they rarely fossilize. This is one reason the fossil record is incomplete.

Overturned strata

Superposition assumes the layers have not been flipped. Overturned folds and thrust faults can place older rocks on top of younger ones. Clues include graded bedding upside down, ripple marks or mud cracks facing down, and fossils in the wrong order.

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

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

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

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

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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 geologic 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 geologic 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 age of a rock? (Imagine a pile of $100$ coins from which you remove half each round: the same idea.)

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

Counting half-lives, resetting the clock and closed systems

If the ratio of daughter to parent atoms is $7:1$, then $1/8$ of the parent remains, so $3$ half-lives have passed. In general, the fraction left is $(1/2)^n$, where $n = t/t_{1/2}$.

A radiometric clock starts when a mineral crystallizes from magma (it is "reset"). A grain in a sandstone dates its original igneous source, not the sandstone.

The method also assumes a closed system: no parent or daughter atoms gain or loss. Groundwater can add younger carbon to a bone or carbonate crust, and hydrothermal alteration can remove lead, giving false ages. Also, each method fits only certain materials: C-14 for organic matter under about $50{,}000$ years (not fired clay or lava), K-Ar and U-Pb for igneous minerals (not sedimentary or metamorphic grains that formed later), and tree rings only for wood. Dendrochronology cannot date lava. Sedimentation time is best bracketed by datable volcanic layers or by paleomagnetic reversals.

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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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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 dike 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: favorable year narrow ring: unfavorable year lake varves water older summer layer thicker 1 varve = 1 year (summer + winter) winter layer thin, clay

Bracketing with datable layers

Sedimentary layers rarely hold datable minerals, so geologists date igneous layers above and below. A layer between a $115$ Ma ash and a $110$ Ma ash is between $110$ and $115$ Ma old. A dike that cuts a layer but not the layers above is younger than the cut layer and older than the overlying ones.

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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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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 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 dike dated at $112$ Ma, but this dike 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 dike, but an intercalated and concordant submarine lava flow.
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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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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.

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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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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.
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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.
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