Groundtruth · radiocarbon

Where the Curve Goes Flat

A radiocarbon laboratory can measure a sample to plus or minus twenty years and still not be able to tell you the century. Not because the machine is bad: because the calendar answer is obtained by inverting a curve, and the curve has stretches where it is nearly horizontal. Set the dial below to 2450 and watch a single measurement come apart into several separate calendar dates. Everything on this page is computed in your browser from the published calibration curves, which are embedded in this file.

Instrument 1 of 11

The calibrator

The calibrator Bayesian calibration against the published curve, computed live

Conventional radiocarbon age as a laboratory reports it, in years before AD 1950.

The quoted measurement error. Drag it down and watch how little the outer bounds move.

Marine samples need the ocean curve plus a local reservoir correction.

Disjoint intervals

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separate calendar ranges in the region

Calendar years selected

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total width of the region

Outer span

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oldest bound to youngest bound

Uncalibrated guess

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radiocarbon age read as a calendar age

    That is the whole difficulty of the method in one control. A laboratory measurement is a number with an error bar. A calendar date is what you get after pushing that number backwards through a curve built from tree rings, and the curve is not a straight line. Where it climbs steeply, one radiocarbon year buys you less than one calendar year and the answer is sharp. Where it flattens, or worse doubles back on itself, one radiocarbon year buys you decades, and a measurement that is beautifully precise in its own units becomes almost mute in calendar years.

    Eleven instruments, all computing live

    1. The calibrator (above): any determination, any of four published curves
    2. The precision bench: what better laboratory precision actually buys
    3. The plateau atlas: every flat stretch, found by your own criterion
    4. The half-life ledger: the wrong half-life, and where it cancels
    5. The mixing bench: contamination in both directions
    6. The reservoir desk: differencing the marine and southern curves
    7. The spike finder: the two years the curve moves fastest
    8. The wiggle-match bench: how the plateau is actually defeated
    9. The revision bench: how much the curve moved from 2013 to 2020
    10. The Thera bench: an unresolved argument, with the knobs exposed
    11. The bomb clock and the Suess dial: the method's own expiry date

    Plus the substrate ledger, three real cases where a radiocarbon date was correct and the object was still a fake, and the check.

    Vocabulary, once, plainly

    BP, cal BP, cal BC

    BP means "before present", and "present" was fixed at AD 1950, the approximate start of the atmospheric bomb tests that made any later definition useless. A conventional radiocarbon age in years BP is not a calendar age. It is a transform of the measured isotope ratio, computed as t = -8033 · ln(F14C), where F14C is the sample's 14C activity as a fraction of a defined modern standard. A cal BP or cal BC date is a calendar date, and it only exists after calibration. Everything the laboratory hands you is on the left of that line; everything an archaeologist wants is on the right.

    What the laboratory actually measures t = -8033 · ln(F)

    Fraction of the modern standard. Above 1 means the carbon fixed after the bomb tests.

    Conventional 14C age

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    years BP, on the 5568-year convention

    Δ14C, approximately

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    (F - 1) × 1000, an approximation (see below)

    Percent of the standard

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    what a mass spectrometer counts

    The mean life 8033 years is fixed by convention, not by physics: it is 5568/ln 2, and 5568 years is Libby's original half-life, which is known to be wrong. The next instrument but two shows exactly how much that matters, which is both more and less than people say.

    An honest note about Δ14C. The proper Δ14C carries an isotopic-fractionation normalisation and a decay correction to the year of measurement; it is not simply (F - 1) × 1000. This page uses F14C as its primary quantity everywhere and labels any place it slips into the approximation, which is what the readout above does. In the regimes shown the difference is small, but it is not zero, and it is a real error to conflate them silently.
    Why it shatters

    The curve, read raw

    No statistics are needed to see the problem. The table below is read directly out of the embedded IntCal20 file at twenty-year steps, live, when this page loads. Look at what the radiocarbon column does between 731 BC and 411 BC.

    Read live from the embedded IntCal20 table. The right-hand column is the change in radiocarbon age per calendar year across each step: it should be near 1 for a well-behaved stretch of curve.
    Calendar yearcal BP14C age BPcurve 1σΔ14C age / Δyr

    This is the Hallstatt plateau, named for the central European Iron Age culture whose chronology it wrecks. It is not a defect in the curve. It is a real feature of the past atmosphere: a rise in 14C production, driven by a decline in solar activity, that happened to cancel radioactive decay for three centuries. Every laboratory in the world inherits it.

    Instrument 2 of 11 · the first objection

    "That is just a precision problem. Better machines will fix it."

    It is the obvious response and it is worth testing rather than arguing about. The bench below takes two determinations, runs the full calibration at nine laboratory precisions from ±80 down to ±2 radiocarbon years, and prints what each precision buys. The twentyfold improvement from ±40 to ±2 is far beyond anything routine accelerator mass spectrometry delivers today. Watch the interval count as you read down the table.

    The precision bench nine full calibrations per column, recomputed on every change
    Lab 1σA: outer spanA: years selectedA: intervals B: outer spanB: years selectedB: intervals

    A: gain from ±40 to ±2

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    reduction in outer span

    B: gain from ±40 to ±2

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    reduction in outer span

    Curve's own 1σ at A

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    the floor no laboratory can go under

    A: interval count as precision improves

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    read left to right as the laboratory gets better

    Read the interval count first, because it is the thing nobody expects. On the plateau a bad measurement gives you one broad answer. Improving it does not collapse that answer to a point; it splits it. One interval becomes two, then three, then five or six thin slivers, and the outer bounds hardly move at all. Precision buys a finer comb inside the same box, and the box is set by where the curve stops being flat.

    The limiting case makes it exact. Send the laboratory error to zero and the posterior converges on the preimage of the measured radiocarbon age under the calibration curve: the set of calendar years where the curve takes that value. On a plateau that preimage is several separated bands, and a perfect instrument returns a set, not a date. Off the plateau, where the curve is monotone and steep, the preimage is a single point and the same slider does honest work. Compare the two columns.

    There is also a hard floor. The calibration curve is itself a measurement with an uncertainty, listed in its own third column, and the calibration convolves the two variances. Drive the laboratory error to zero and the answer converges on what the curve alone can say, which through the Iron Age is about a dozen radiocarbon years.

    Instrument 3 of 11

    The plateau atlas

    The Hallstatt plateau has a name because it wrecked a chronology people cared about. Run one uniform criterion across the whole curve and it is not alone, and it is not obviously the worst. The atlas below has two modes, and they disagree in instructive ways, because "plateau" is not one definition.

    Mode A, the resolution sweep, is the criterion that means something: at every calendar year in the domain, it invents a sample that dates exactly on the curve at that year, runs the full calibration on it, and records how wide the answer comes back. No arbitrary threshold, just a lab precision you set. Mode B, the flatness scan, is the criterion people usually reach for: a least-squares local slope of the curve, and a run of years where the slope stays under a threshold. Mode B needs three arbitrary numbers, so all three are knobs, and you can watch the answer move when you move them.

    The plateau atlas one criterion, applied to the whole curve

    Rankcal BPcalendarlengthworst span / 14C changenative grid

    A cross-check with no threshold in it at all

    Both modes above need a number you chose. Here is a measure that needs none: for a given radiocarbon age, simply count the calendar years at which IntCal20 takes that value to within the width of a good measurement. That count is the ambiguity, with no criterion in the middle.

    Calendar years inside the band

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    searched over cal BP 0 to 14,000

    Worst radiocarbon age found

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    scanned live in steps of 10 14C yr

    Best case for comparison

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    the least ambiguous age in the same scan

    Two things this atlas is not. First, it is not a discovery. We could not find a published ranked atlas of IntCal20 plateaus as of 2026-07-24, but plateaus are entirely standard subject matter in the field, individual ones are named and studied in the literature, and what is above is a computation over a published curve rather than a new fact about the world. Change the criterion and you get a different list, which is exactly why every knob is exposed. There are settings under which nothing qualifies, the Hallstatt plateau included: narrow mode B's window to fifty years and the annual curve is wiggly everywhere, so no run survives. That is not a bug in the scan, it is the point. "Plateau" is a definition, not an object. Second, beyond cal BP 5000 IntCal20 is published on a five-year grid, and beyond 15,000 on ten- and twenty-year grids. Runs found there are measured on a curve that cannot represent a wiggle shorter than its own spacing, so their flatness is partly a property of the grid. Every run in the table is tagged with the native spacing of the region it sits in, and the default domain is the single-year part only.

    Two things fall out of mode A that are worth pausing on. The stretch near the top of the ranking is usually not Hallstatt. And the very worst region in the whole single-year record is the one closest to the present: dates from roughly the mid-seventeenth century onwards calibrate appallingly, because the industrial dilution of atmospheric 14C pushed the curve back down through values it had already occupied. A piece of wood from AD 1700 and a piece from AD 1900 can be radiocarbon twins. Hold that thought; the last instrument on this page is about what happens when that region keeps growing.

    Instrument 4 of 11 · the second objection

    "But they still use Libby's wrong half-life, so every date is 3% out."

    Half true, and the half that is true is not the half people mean. Libby's original half-life of 5568 years is indeed wrong; the better value, published as the mean of three determinations reported at the 1962 Cambridge radiocarbon conference, is 5730 ± 40 years published. And the 1977 reporting convention that laboratories still follow says, in as many words, that a conventional radiocarbon age implies "the use of the 5568 yr half-life (mean life 8033 y)" published, verbatim. So laboratories knowingly report ages on a half-life they know to be wrong.

    The ledger below computes both columns. On the left, the conventional age and the age you would get on the better half-life. On the right, both of those calibrated, because the calibration curve is itself published as conventional radiocarbon ages on the same 5568 convention. Watch which column the error survives in.

    The half-life ledger two conventions, two calibrations, one calendar answer

    Age on 5568 (as reported)

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    mean life 8033 yr

    Age on 5730 (physically better)

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    mean life computed live from 5730/ln 2

    Difference

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    the "3%" everybody quotes

    Calibrated on the 5568 convention

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    95.4% outer bounds

    Calibrated on the 5730 convention

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    sample and curve both converted

    Calendar disagreement

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    years, at either bound

    The exact ratio 5730/5568 is computed live and printed above. The cancellation is not magic: both the sample and the curve are divided by the same mean life before they are compared, so the factor drops out. It only cancels because the curve is published on the same convention as the sample. Compare an uncalibrated conventional age against a clock that is not radiocarbon (a dendro date, a historical record, a varve count) and the 3% is fully present.

    So both of the confident statements are wrong. "Radiocarbon dates are 3% too young" is false for calibrated dates, which is what any modern publication quotes. "The half-life does not matter" is false for the uncalibrated conventional ages that fill older literature and every laboratory report, and false the moment you compare one against a non-radiocarbon clock. The convention survives because changing it would silently invalidate every conventional age ever published, and because calibration makes it harmless where it counts.

    A detail that shows how carefully this was thought through in 1977: the same convention that fixes 5568 for the reported age specifies the 5730 half-life for the small decay correction between a sample's collection and its measurement, and for percent-modern reporting. The convention is not ignorant of the better number. It is deliberately keeping two books.

    Instrument 5 of 11 · the third objection

    "So the real enemy is contamination. Keep the sample clean."

    True, and the interesting part is that contamination is not one problem. It is two, and they are exact mirror images of each other. The bench below does two-component isotopic mixing and then inverts to an age. Nothing but arithmetic: no curve is involved.

    The mixing bench Fmeas = (1-c)·Ftrue + c·Fcontam

    Slide to the far right for a sample so old it holds no 14C at all.

    Slider is in hundredths of a percent: 100 means 1.0%, and the range runs to 2.0%.

    1.00 = modern carbon (rootlets, handling, humic acids). 0.00 = dead carbon (petroleum, limestone, old groundwater).

    Measured F14C

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    Apparent age reported

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    Error

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    apparent minus true

    The ceiling

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    apparent age of an infinitely old sample at this contamination

    Dead-carbon offset

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    added 14C years per 1% dead carbon, at every true age

    Contamination for a 50,000 BP ceiling

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    modern carbon needed to make dead carbon read 50 kyr

    The two sweeps are worth doing in order. Modern contamination is nearly harmless to a young sample and catastrophic to an old one: the same one percent that shifts a thousand-year-old sample by about a decade puts a floor under everything older, and that floor, not radioactive decay, is what sets radiocarbon's practical ceiling near fifty thousand years. There is still measurable 14C in a hundred-thousand-year-old sample in principle; what there is not, is a laboratory able to certify that the last one part in ten thousand of its carbon did not come from a fingerprint. That is why pretreatment exists, and why the ceiling has moved outward with chemistry rather than with counting statistics.

    Dead-carbon dilution does the opposite, and its behaviour is startlingly simple: it adds a constant number of radiocarbon years, the same number at every true age, because it multiplies F rather than shifting it, and the age transform is a logarithm. Run the second sweep and watch a flat line. That single constant is the entire mechanism of reservoir effects, hard-water effects, and volcanic-CO2 effects. Which brings us to the next desk.

    Instrument 6 of 11

    The reservoir desk

    Carbon that did not come from the contemporary atmosphere arrives already old. Surface seawater carries carbon that has been out of contact with the air for centuries; a lake over limestone dissolves carbon that has been out of contact for millions of years; a shellfish, a whale, a person who ate a lot of fish, all inherit it. The global marine offset is not a constant to be looked up. It is the difference between two published curves, and it can be drawn.

    The reservoir desk R(t) = Marine20(t) - IntCal20(t), computed at every tabulated year

    Global marine reservoir age R(t)

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    Marine20 minus IntCal20 at this year

    Southern hemisphere offset

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    SHCal20 minus IntCal20 at this year

    Holocene mean R

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    averaged live over cal BP 500 to 11700

    Glacial mean R

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    averaged live over cal BP 20000 to 40000

    cal BPIntCal20Marine20R = M - ISHCal20SH - I

    What using the wrong curve costs

    Against IntCal20

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    Against SHCal20

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    shift vs IntCal20, in calendar years

    Against Marine20, ΔR = 0

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    shift vs IntCal20, in calendar years

    Do not read a single number off this desk. R(t) at the modern edge is depressed by the industrial dilution already present in the atmospheric curve, so the value the desk computes at cal BP 0 is smaller than the pre-industrial global average usually quoted for Marine20. That is a real property of the difference of two curves at their modern end, not a mistake, and it is why the desk shows the whole function rather than headlining one figure. A real marine sample also needs a local ΔR for its own coastline, which the calibrator above will accept, and which comes from a regional database rather than from any curve.

    The southern hemisphere offset is the same idea at a smaller scale: the southern atmosphere sits over more ocean, exchanges more carbon with it, and runs a few decades old relative to the north. Use the northern curve on a southern sample and the answer moves. The desk computes by how much.

    Two things that look like reservoir effects and are not. Old wood: a beam cut from the heart of a three-hundred-year-old oak dates the heartwood, not the building, and no correction fixes it because nothing is wrong with the measurement. Inbuilt age in driftwood or long-lived charcoal is the same problem. These are sampling errors, they are asymmetric (they can only make things look older), and they are the reason short-lived material, a seed, a twig, a single tree ring, is worth more than a large charcoal lump.

    Instruments 7 and 8 of 11

    How the flat stretches are actually beaten

    Nothing above is news to anyone who dates things for a living. The field has three standard answers to a plateau, and two of them can be run here.

    The spike finder

    The first answer is to find a year where the curve does the opposite of flattening. Rank every single-year step in IntCal20's native annual record by how far the radiocarbon age moves in one calendar year, and see what comes out on top. The table below does that live over all 5,000 annual points, sorting nothing in advance.

    The spike finder every one-year step in IntCal20, ranked
    RankCalendar stepcal BP14C age changeas a fraction of F

    AD 772 to AD 778, total fall

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    computed across the whole event in IntCal20

    AD 991 to AD 998, total fall

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    the second event, same computation

    Those are the two Miyake events. In 2012 Fusa Miyake and colleagues reported a rapid increase of about 12 parts per thousand in the 14C content of Japanese cedar rings between AD 774 and AD 775, roughly twenty times anything ordinary solar modulation produces published; a second was reported at AD 993 to 994 the following year published. They are now written into IntCal20 itself, which is why the finder above lands on them without being told where to look. Note that the compiled curve smooths the event across several years, so the single-year step it shows is smaller than the single-tree measurement; the two readouts above sum the whole event instead, and they land in the same range as the published single-tree magnitudes.

    What this buys you is enormous. A sequence of tree rings crossing AD 775 does not calibrate to a range. It calibrates to a year, because there is exactly one year in the last several millennia where the curve does that. The same trick anchors floating chronologies that have no dendrochronological link at all.

    The wiggle-match bench

    The second answer needs no spike. If you have several samples whose calendar spacing is known, for instance rings n, n+10, n+20 of the same timber, then you are no longer inverting a curve at a point. You are sliding a rigid comb along it and asking where it fits. The plateau that made a single date useless is precisely what makes the comb's position unambiguous, provided the comb is long enough to reach off the flat part.

    The wiggle-match bench joint posterior over a rigid sequence, computed live

    Slider is cal BP; the label converts. The default lands on the Hallstatt plateau.

    The samples are synthetic, drawn from the curve itself with seeded pseudo-random noise. Reseed to see how much the answer wobbles.

    First sample alone

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    95.4% outer span, one date

    Whole sequence together

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    95.4% outer span of the sequence start

    Improvement

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    factor by which the span shrinks

    Truth recovered?

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    does the joint region contain the year the samples were drawn from?

    This bench simulates. The samples are generated from IntCal20 plus Gaussian noise rather than measured, which is why it can tell you whether the answer is right. Real wiggle-matching is done in a Bayesian framework (OxCal, BCal) that also carries stratigraphic priors; the third standard answer to a plateau, not simulated here, is exactly those priors: if you know layer B lies above layer A, that ordering alone can cut a plateau-wide posterior down hard.

    Instrument 9 of 11 · what would falsify all of this

    The curve is a hypothesis, and it gets revised

    The calibration curve is not a definition. It is a reconstruction of past atmospheric 14C, assembled from material whose calendar age is known independently: tree rings counted one by one to about 13,900 cal BP, and beyond that a statistical integration of speleothems, corals, and marine and lake sediments on their own timescales published. That makes it testable, and it has been revised repeatedly: IntCal98, 04, 09, 13, 20. The bench below carries both IntCal13 and IntCal20 and computes the difference.

    The revision bench IntCal20 minus IntCal13, and what it did to real answers

    Under IntCal13

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    Under IntCal20

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    Median shift

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    calendar years the answer moved

    Largest curve change, 0 to 12000 cal BP

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    computed across the whole overlap

    What would falsify the central claim of this page. The claim is that a single radiocarbon determination on the Hallstatt plateau returns a multi-century, multi-modal calendar answer that laboratory precision cannot repair. It would be falsified by a demonstration that IntCal20 is wrong through the first millennium BC in a way that removes the flat stretch: for example, a set of dendrochronologically dated single rings from 800 to 400 BC whose measured radiocarbon ages climb steadily instead of stalling. Work of exactly that kind has been done, and it sharpened the structure inside the plateau rather than removing it. It would also be falsified if the plateau turned out to be regional rather than hemispheric, in which case a regional curve would fix it. The known regional offsets in this era are of order tens of radiocarbon years, not the hundreds that would be needed.

    Instrument 10 of 11 · the frontier

    Thera: forty years, two answers, and the knob nobody can pin

    Some time in the mid second millennium BC the volcano at Santorini erupted, burying a Bronze Age town and leaving an ash horizon that would let archaeologists in the Aegean, Egypt and the Near East synchronise their chronologies with each other. Dating it has been contested for about forty years. The disagreement is not scientists against traditionalists. It is two evidence-based reconstructions that do not agree, and the honest summary is the one in the abstract of the most careful recent radiocarbon paper: a discrepancy between radiocarbon evidence, "late 17th-early 16th century BCE", and archaeological evidence, "mid 16th-early 15th century BCE" published, verbatim.

    A wiggle-match on an olive branch buried alive by the eruption constrained it to 1627-1600 BC at 95.4% published. Annual-resolution measurements on calendar-dated tree rings across 1700-1500 BCE later found an offset from the international curve and reported a shift of the calibrated Thera range toward the sixteenth century published. Regional offsets in the Mediterranean and Anatolia have since been measured at roughly 0 to 22 radiocarbon years published.

    So here is the frontier, made operable. Below, knob A applies a regional radiocarbon offset and propagates it through IntCal20's own local slope; knob B applies a shift to the archaeological chronology. Turn knob A up to the largest offset anyone has measured here and watch how few calendar years it actually buys. Then turn knob B and watch how much it has to move.

    The Thera bench two plausible corrections, one gap, no adjudication

    Measured range for the Mediterranean and Anatolia is about 0 to 22 years. The slider goes further so you can see where it stops helping.

    Egyptian chronology is a reconstruction with its own error bars, not a fixed ruler. Twenty to thirty years of slack in this period is not a fringe position.

    Published radiocarbon range, offset applied

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    1627-1600 BC moved by knob A, at first order

    Local curve slope here

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    computed from IntCal20 around 1613 BC

    Calendar years knob A buys

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    offset divided by the local slope

    Gap to the archaeological range

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    zero means the two overlap

    Offset alone that would close it

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    computed live, with knob B where you left it

    One single date at 1613 BC

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    a synthetic on-curve sample, calibrated live

    Two different objects are on that plot and they must not be confused. The green bar is the published wiggle-match range 1627-1600 BC, moved by knob A using the local slope of IntCal20 as a first-order propagation of a uniform regional offset. The orange bar is a live calibration of a synthetic short-lived sample whose radiocarbon age is exactly IntCal20's own value at 1613 BC, with your offset subtracted: it is a probe of the curve's shape, not a published determination, and it is far wider than the published range because a single date cannot do what a wiggle-matched sequence does. The violet bar is the published archaeological range, moved only by knob B.

    What that bench shows, and what it deliberately will not do, are both worth stating flatly. A uniform regional offset of the size that has actually been measured, propagated through the curve's local slope, buys only a handful of calendar years here, well short of the gap. Knob B has to do most of the work if the gap is to be closed by these two mechanisms alone. That is not an argument that the archaeologists are wrong: it is a demonstration that a uniform offset is the wrong shape of correction, which is exactly what the annual-resolution work found. The 2018 result did not shift the curve up or down by a constant; it changed its shape at one-year resolution across 1700-1500 BCE, and a change in shape can move a calibrated range in ways a constant cannot. The page has no standing to adjudicate between the camps and does not try. It also declines to imply that one side is the scientific one: Egyptian chronology is an evidence-based reconstruction with its own error bars, not a tradition being defended.

    A recent treatment of exactly this problem points out that the interval 1620-1540 BC is itself a difficult stretch of curve, and that ordered sequences of dates across it tend to spread rather than converge unless outside information is brought in published. Which is this page's own subject, arriving at the one place where it costs the most.

    Instrument 11 of 11 · the second frontier

    The bomb clock, and the dilution coming the other way

    Between 1955 and 1963 atmospheric nuclear testing nearly doubled the 14C content of the air. Anything that fixed carbon after that carries a label, and the label is a clock: the excess has been washing into the ocean and the biosphere ever since, on a curve that can be inverted. This is how a wine, an ivory tusk, a painting's canvas or a human tooth gets dated to a few years. The zonal annual curves loaded below are the published Hua et al. compilation for 1950 to 2019 published data; everything computed from them here is computed here.

    The bomb clock inversion by root finding, all roots returned

    Slider is F × 1000.

    Slider is σ × 10000. Typical modern AMS is a few parts per thousand.

    Calendar years matching this F

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    all roots, not just the convenient one

    Zone peak

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    annual-mean maximum for this zone, found live

    Dating resolution at the newest root

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    σF divided by the local slope |dF/dt|

    Resolution in 2019

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    same computation at the end of the record

    Two honest limits on that clock. Before about 1965 the inversion is double-valued: the rising limb and the falling limb cross the same F, and the readout above returns both, because a single measurement genuinely cannot separate them. And after about 1990 it is single-valued but the curve is flattening toward 1, so the same measurement error buys fewer and fewer years. Drag the F slider down toward 1.01 and watch the resolution readout degrade. The bomb clock is not a permanent instrument. It is a transient that is currently expiring.

    The peak value depends on which dataset you are using. These are annual means for five broad zones; monthly data from individual stations reach higher, and the figure often quoted in the region of 965 parts per thousand comes from higher-resolution records than the one loaded here. The peak the readout shows is the maximum of the annual-mean series it actually holds, found by scanning it.

    The Suess dial

    Fossil fuel is carbon that has been out of the atmosphere for tens of millions of years, which means it has no 14C at all. Burning it is a dead-carbon dilution of the whole atmosphere, and from the mixing bench above you already know what dead-carbon dilution does: it adds radiocarbon years to everything, uniformly. The bomb pulse has been masking it. As the pulse decays, the dilution keeps going.

    The Suess dial t = -8033 · ln(1 + Δ/1000)

    Conventional age new material reports

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    a plant grown in that atmosphere, dated today

    Calendar date it would calibrate to

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    run through the calibrator, 95.4%, ±25

    F14C

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    The two marked settings are the endpoints of a published simulation study, not predictions: it found that "ambitious emission reductions could sustain Δ14CO2 near the preindustrial level of 0 per mil through 2100, whereas 'business-as-usual' emissions will reduce Δ14CO2 to -250 per mil, equivalent to the depletion expected from over 2,000 y of radioactive decay", and that this "implies that radiocarbon dating may no longer provide definitive ages for samples up to 2,000 y old" published, verbatim. The same paper's significance statement says that "by 2050, fresh organic material could have the same 14C/C ratio as samples from 1050, and thus be indistinguishable by radiocarbon dating" published, verbatim. The dial does not know which path we are on; it is your knob, and the page declines to set it. The scenario labelled business as usual there is RCP8.5, which is now more often described as a high-end pathway than a central expectation, and that is a live argument this page has no standing in.

    The rhyme is hard to miss. A technique whose worst region is a plateau in the Iron Age is being handed a plateau in the present, by the same physics, running the other way.

    Provenance

    The date is on the atoms, not on the meaning

    The most common way to be wrong with a radiocarbon date is not to get the number wrong. It is to get the number right and attach it to the wrong claim. A radiocarbon determination bounds the death of the organism whose carbon you sampled. It does not bound when someone wrote on it, painted it, assembled it, or decided what it meant. The ledger below works three real cases: for each, choose what was sampled, and it prints what that sample can and cannot bound.

    The substrate ledger what a date on this component actually bounds

    What the date is on

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    Published determination

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    quoted, not recomputed

    This bounds

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    This leaves untouched

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    On the Shroud entry. This page takes no position on the Shroud of Turin's authenticity and does not have the standing to. It appears here because it is the most thoroughly documented example of a radiocarbon determination on one component of a complex object, and because the original paper reported its own inter-laboratory heterogeneity, which is a piece of scientific honesty worth showing. The published lab means, the unweighted mean, and the chi-squared statistic in the ledger are all from the 1989 paper itself. A named 2019 reanalysis of the released raw data argued that the sample was not homogeneous and that the published uncertainty is therefore understated. That is stated as what its authors argued, and this page does not adjudicate it. Nothing here says the medieval date is overturned, and nothing here says the critiques are frivolous.

    Two of the three are settled forgery cases, and they make the same point twice. The Vinland Map's parchment passed. It really is fifteenth-century, and the radiocarbon test that established that was correct and remains correct. What convicted the map, in 2021, was an X-ray fluorescence survey finding a titanium compound "used in inks first produced in the 1920s" pervading its lines and text, together with a medieval Latin inscription on the back overwritten in modern ink to look like binding instructions published, verbatim. All sixteen of the Museum of the Bible's Dead Sea Scroll fragments were judged modern forgeries in a report the museum itself commissioned; the material was old leather rather than the parchment genuine scrolls use, and the giveaway was ink pooling in cracks and running off torn edges that would not have existed when the material was new published. In neither case was radiocarbon the instrument that caught the fake. In the Vinland case it was the instrument that cleared the substrate and thereby made the fake look stronger for half a century.

    The third case is in the ledger for a different reason, and the difference matters. Nothing on this page says the Shroud of Turin is a forgery; the page has no position on what it is. It is here because it is the best-documented example of a radiocarbon determination on one component of a complex object, because the sampling and the inter-laboratory scatter were published in full by the people who did the work, and because the general rule applies to it exactly as it applies to everything else: a date on the cloth is a statement about the cloth.

    The edges of the method

    What radiocarbon cannot date, and why

    Three separate walls, often confused with each other.

    No organic carbon, no date. Radiocarbon dates carbon that was once in a living thing. Stone tools, pottery fabric, metal and pigment minerals are outside its reach entirely; what gets dated is the charcoal in the hearth beside them, or the soot in the pot's residue, and the link from that to the object is an archaeological argument, not a measurement.

    Carbon that did not come from the contemporary atmosphere is datable but arrives already old, by the constant offset the mixing bench computes. Marine shell, freshwater fish, a plant growing in a volcanic CO2 vent, mortar made from limestone: each needs its own correction, and each correction is an extra assumption.

    Too old. The practical ceiling near fifty to fifty-five thousand years is set by contamination, not by decay. Run the mixing bench's ceiling readout down to a tenth of a percent of modern carbon and see where it puts the floor. This is worth being plain about, because the ceiling is often quoted as evidence that radiocarbon is unreliable in general. It is the opposite: the ceiling exists because the practitioners refuse to certify a date they cannot defend against a contribution of one part in a thousand. A three-hundred-year ambiguity in the Iron Age and a hard refusal to date past 55,000 years are the same discipline, visible from two sides.

    None of the difficulties on this page are hidden knowledge, and none of them is a criticism of the field. Every one is standard, taught, published, and routinely corrected for. What the instruments here do is let a stranger operate the corrections rather than be told about them.

    The check

    The central claim. Calibrating a conventional radiocarbon age near 2450 BP against IntCal20 returns a 95.4% highest-posterior-density region made of several disjoint calendar intervals spanning roughly three and a half centuries; and improving laboratory precision twentyfold, from ±40 to ±2 radiocarbon years, reduces the outer span of that region by under ten percent, while the same improvement off the plateau does substantially more. Both halves are computed in your browser, above, and both are recomputed independently offline by the verifier.

    Recomputed live, right now, in this page

    An independent re-derivation, and where it disagrees

    Before this page shipped, the central result was re-derived by a worker who had not seen it, working only from the published curve and the published literature. That re-derivation first reproduced the CALIB Manual's own worked example (3650 ± 50 BP on IntCal04), matching three of four published endpoints exactly after rounding and the fourth to 0.7 of a year, then ran CALIB REV8.2 itself on IntCal20 and obtained the same four intervals for 2450 ± 30 BP that the calibrator above computes.

    How the numbers are produced

    Every free choice, named

    Uncertainties and things we could not confirm

    What would falsify this

    Sources

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