Forest canopy viewed from below, illustrating biodiversity and the natural carbon cycle

How carbon-14 analysis helps preserve biodiversity

Preserving biodiversity means more than just protecting visible species. To be effective, we also need to study the invisible mechanisms, natural cycles and slow transformations that have been affecting environments for millennia. The dating sciences play a key role in this quest for knowledge. Among them, carbon-14 analysis is an invaluable tool for tracing the history of organic matter in soils, sediments or biological samples.

Carbon-14 dating, the reference method used in specialized laboratories, makes it possible to establish reliable chronologies, identify ecological ruptures and measure the impact of climate change on ecosystems. It offers researchers, ecologists and environmental managers tangible, verifiable and scientifically exploitable data.

In this article, we'll first look at how this method works and why it's particularly well-suited to the study of ecosystems. We will then explore its practical applications to better understand and preserve biodiversity. Finally, we will explain why calling on the services of a laboratory specialized in carbon-14 analysis, such as CIRAM, is an essential step in guaranteeing the reliability and scientific value of the results obtained.

Understanding carbon-14 dating and its relevance to the study of ecosystems

Precise time references have become essential for analyzing the evolution of natural environments, at a time when ecological issues are becoming increasingly complex. Carbon-14 dating is now an essential method for environmental and biodiversity research, and not just for archaeology.

What is carbon-14 dating and how does it work in ecosystems?

The carbon-14 dating method is based on a simple, yet remarkably powerful analytical principle: all living organisms integrate carbon-14 throughout their lives. When they die, this radioactive isotope begins to decay at a known rate, with a half-life of 5,730 years. Scientists can therefore estimate the age of an object with great precision by measuring the amount of residual carbon 14 in its sample. 

This approach makes it possible to date the organic matter contained in soils, peat and lake or river sediments in an environmental context. It thus plays a key role in the reconstruction of past ecological dynamics, providing reliable chronological data on climatic events, vegetation changes or past human disturbances. 

Gas pedal mass spectrometry (AMS) can also be used to refine the analysis. This complementary method enables the dating of very small samples, while guaranteeing high precision, even for low-carbon materials.

Why carbon-14 dating is essential for environmental and biodiversity research

When applied to biological samples such as pollen, charcoal, plant remains or bones, carbon-14 dating can document the temporal structure of ecosystems. It reveals the lifespan of habitats, the frequency of disturbances, and the appearance or disappearance of species.

It also sheds light on organic matter degradation processes and soil carbon flows. These are crucial indicators of ecosystem health. From a conservation perspective, this data can be used to identify the most resilient areas, to better target conservation actions or to quantify the past impacts of human activity.

Radiocarbon dating is therefore an extremely relevant decision-making tool for researchers and managers of natural environments alike.

Practical applications of radiocarbon analysis to preserve biodiversity

Carbon-14 dating is proving extremely useful in the field. It is used in practical projects for environmental monitoring, analysis of ecological resilience and management of natural environments, providing them with reliable data. However, its real contribution depends on a clear understanding of its uses and limitations, as well as the conditions for its implementation.

Measuring the evolution and resilience of natural environments using carbon-14 dating

The chronologies constructed in environmental studies, based on radiocarbon dating, make it possible to place events in their temporal context. This enables us to understand, for example, the factors behind the draining of a wetland, reforestation or changes in agricultural practices. This historical perspective is invaluable for interpreting current ecosystem dynamics.

In this context, sediments are often used as natural archives. By analyzing their composition at different depths (by coring) and dating them precisely, it becomes possible to reconstruct ecological trajectories over several centuries. The data extracted can be used to identify breaking points, regeneration rhythms and periods of high anthropogenic pressure.

Isotope analysis (carbon 13 / carbon 12) also plays a role in tracing carbon flows. This is central to understanding the carbon cycle and modeling climate change. For researchers, this approach offers concrete indicators of an ecosystem's capacity to store or release carbon.

Limits and precautions: towards a reliable interpretation of radiocarbon data

Like all scientific methods, carbon-14 dating has its limitations. These include sample contamination, calibration errors and the presence of materials that are too old. Only rigorous preparation can limit the risk of error. This begins with the selection of the sample, right through to its processing in the laboratory.

The use of gas pedal mass spectrometry (AMS) is now the norm in specialized laboratories, as it allows high precision even on samples of a few milligrams. But rigorous processing does not stop at measurement: interpretation of the results also requires an interdisciplinary approach, combining ecology, geochemistry and paleoenvironment.

The data produced by carbon-14 dating should never be considered in isolation: they take on their full meaning when integrated into a coherent scientific protocol, where each result sheds light on a facet of the ecological prism.

The role of laboratories specializing in carbon-14 dating for environmental research professionals

Environmental research departments regularly work with laboratories specializing in carbon-14 dating, with a simple aim: to guarantee the robustness of their analyses. But what to expect? What does this collaboration entail, and what are the criteria for selecting the most efficient analytical laboratory to carry out reliable, rigorous and documented studies?

Why use an analysis laboratory like CIRAM for your environmental studies?

The quality of results from biodiversity-related projects depends to a large extent on the accuracy of measurements and the rigor of protocols. CIRAM, an independent French laboratory, works hand in hand with scientists, providing them with proven expertise in radiocarbon dating. This methodology, combined with our mastery of isotope analysis and organic material preparation techniques, guarantees clear, usable results.

CIRAM is able to process complex, very small samples, while guaranteeing high sensitivity. This level of performance enables researchers to work on fragile matrices, often difficult to exploit in an environmental context (coals, sediments, plant remains).

Beyond the technical aspects, the value of working with a laboratory specialized in 14-dating for environmental research lies in the quality of the support provided. Each project benefits from personalized follow-up, with direct exchanges between the scientific team and the professionals carrying out the study. The ultimate aim is to produce usable, documented results that are fully integrated into the client's research approach.

Integrating carbon-14 dating results into a biodiversity conservation strategy

Environmental teams need to be able to effectively mobilize the analyses delivered by the laboratory. CIRAM provides clear, structured reports, including raw data, uncertainties, methods used and possible interpretations. These documents can be easily integrated into an interdisciplinary research project, an ecological expertise mission or a conservation program.

The dating results obtained can also enrich databases, model climate scenarios or guide environmental management decisions. To achieve this, CIRAM does more than just produce figures: the laboratory works alongside biodiversity stakeholders to provide solid scientific evidence that is understandable and useful for action.

Ultimately, carbon-14 dating offers much more than a simple measure of age: it provides crucial information on how ecosystems have evolved, how they react to climatic or human pressures, and reveals the invisible dynamics of biodiversity. Thanks to this dating method, environmental professionals have a reliable tool for placing their observations in a long-term time perspective, essential to any conservation strategy.

We have seen how radiocarbon dating can be used to document the transformation of natural environments, analyze carbon fluxes in soils and build robust ecological chronologies. These valuable data, however, require specialized expertise to be obtained and interpreted rigorously.

This is precisely what CIRAM offers, an analytical laboratory recognized in France and internationally for the quality of its work in carbon-14 dating, both in the environmental and archaeological fields. Thanks to its cutting-edge equipment and demanding scientific approach, CIRAM supports researchers, institutions and public bodies in understanding and preserving living organisms.

Do you have a project requiring carbon 14 analysis?
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How does carbon-14 dating work?

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7–11 minutes

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Accurately dating an object or a work of art involves much more than a simple chronological measurement: it enriches knowledge, confirms authenticity and enhances the value of the work. Carbon-14 dating, a technique that has been in use for over 70 years, remains the benchmark method for analyzing organic materials, from archaeological remains to ancient works of art.

But how does this method actually work? Which objects can really be dated? And above all, what guarantees does carbon-14 dating offer in terms of scientific reliability?

In this article, we explore the fundamentals of carbon-14 dating, its fields of application and its limitations. You'll also discover the strategic role played by specialized laboratories such as CIRAM in assisting people wishing to have an object dated in their analysis, expertise or conservation projects.

In summary:

  • Carbon-14 makes it possible to reliably date organic materials used in archaeology and in works of art.
  • The accuracy of the results depends on the quality of the sample, the analyses, and their interpretation.
  • The expertise of a specialized laboratory is essential for obtaining reliable and usable dating results.

Understanding carbon-14 dating: principles and operation

Often used as a tool for authentication or absolute dating, carbon-14 dating is an analytical technique based on a physical principle that is as robust as it is precise. It offers professionals an essential scientific method for reliably and documentably dating organic materials.

The basic principle of carbon-14 dating

Carbon-14 dating was developed in the 1940s by American chemist Willard F. Libby, and rapidly revolutionized the human sciences. Libby achieved the first radiocarbon dating in 1949, a breakthrough that earned him the Nobel Prize in Chemistry a year later. 

The principle of carbon-14 dating is based on the natural decay of a radioactive carbon isotope: carbon-14 (14C). This radioactive carbon isotope is present in minute quantities in the upper atmosphere. It is formed by the interaction of cosmic rays with nitrogen 14, causing a transformation into carbon 14. It is then absorbed by the biosphere (plants, animals, humans).

When an organism dies, it ceases to exchange carbon with the environment, and radioactive decay of 14C can begin. This phenomenon makes it possible to date the organism's death with precision. The time it takes for half of the 14C to decay is known as the "half-life of carbon 14", and is estimated at 5,730 ± 40 years. It's important to note that early dating used a conventional value of 5,568 years, which explains some of the differences in interpretation in early literature.

This enables scientists to measure the ratio between residual 14C and 12C in a sample (wood, bone, textile, ivory...). They also apply isotopic fractionation corrections (natural variations in the 12C/13C ratio) to standardize results.

Unlike relative dating techniques, which establish chronological relationships between objects, radiocarbon dating provides absolute dating, with an accuracy of just a few decades.

The method has been greatly improved since Libby first formulated it, notably with the advent of gas pedal mass spectrometry (AMS). Results are then expressed in "Before Present (BP)" years, the "present" being conventionally set at 1950, the scientific reference date.

From laboratory to analysis: how does carbon-14 dating work?

Carbon-14 analysis follows a rigorous, codified protocol. First, the laboratory takes a controlled sample. This is often carried out with the customer to guarantee traceability. The sample is then purified to eliminate any contamination (glues, varnishes, preservatives, etc.).

The most widely used technique today is gas pedal mass spectrometry (AMS). It enables carbon-14 atoms to be counted directly, even on minute samples of the order of a few milligrams. Before this step can be carried out, the material must be converted to pure graphite, then ionized and accelerated for extremely sensitive analysis. This technical step requires precise know-how and highly specialized equipment, which only laboratories specializing in carbon-14 dating possess (with a few exceptions).

Finally, the raw results are adjusted using international calibration curves (such as IntCal20) to compensate for variations in atmospheric radiocarbon levels over time. Natural phenomena such as solar activity, magnetic fields or anthropogenic emissions can influence this calibration.

Please note that certain contexts require special precautions, such as the effects of marine or river reservoirs (concentration of old carbon in water), or the phenomenon of old wood, when the material used in a work is older than its creation. These specificities are taken into account by the analysis laboratory to enable precise dating of the sample analyzed.

Applications and limitations of carbon-14 dating

Carbon-14 dating is not applicable to all objects. Before initiating a dating process, the applicant must know which materials are compatible, over which periods this method is reliable, and how to interpret its results within the framework of a professional expertise.

What objects and materials can be carbon-14 dated?

The carbon-14 dating method can only be applied to organic materials: wood, bone, ivory, teeth, plant textiles (linen, cotton), leather, charcoal, plant fibers, pigments containing organic binders, and so on.

This analysis is essential in archaeology, for many applications such as dating habitats, burials, ancient structures or everyday objects.
In the field of art, it can be used to verify theauthenticity of works, from the dating of wooden sculptures to ethnographic objects, icons, musical instruments or even paintings.

It is also invaluable for identifying counterfeits, since it can detect modern copies or undocumented restorations.

Reliability, precision and limitations of the method

The reliability of carbon-14 dating results depends on several criteria:

  • Condition of sample
  • Sample quality (representativeness, absence of contaminants)
  • Method used (AMS is strongly recommended for works of art)
  • Rigorous chronological calibration

Dating accuracy can reach a few tens of years for the last two millennia. For very old objects, it can extend to several hundred years.
The theoretical limit of the method is around 60,000 years, but in practice, results beyond 45,000 years must be interpreted with caution due to the extremely weak residual signal.

Finally, it's important to bear in mind that the method dates the death of the organism (felling of the tree, harvesting of the flax, death of the animal) and not the making of the object. Cross-dating with stylistic, historical and technological data is therefore essential. This is why radiocarbon dating is often combined with other analytical methods, on the laboratory's recommendation. 

The role of specialized laboratories in securing scientific expertise

Obtaining a date is not an end in itself: the analysis must be reliable, traceable and interpretable. This is where the expertise of a laboratory specialized in carbon-14 dating, such as CIRAM, becomes decisive.

Why use an analysis laboratory?

Carbon 14 dating is not a simple technical operation, but an act of expertise with high added value for professionals or private collectors.
Entrusting an object to an accredited and independent laboratory helps avoid errors, contamination and haphazard interpretations.

Specialized laboratories like CIRAM know :

  • Determining whether an object is datable or not
  • Suggest non-destructive methods or micro-sampling of discrete areas
  • Apply material-specific purification protocols
  • Reject dubious analyses to avoid misinterpretation

A laboratory recognized for the quality of its carbon-14 dating also provides a clear, structured scientific report, mentioning the results, the margins of error and the calibration used, and plays an essential advisory role in interpreting the results.

CIRAM: your trusted partner for carbon-14 dating

Based in France, with over 20 years of expertise, CIRAM is today a leading player in the field of carbon-14 dating and scientific analysis of heritage objects, both nationally and internationally.

CIRAM performs carbon-14 dating for :

  • museums and public institutions
  • private collectors
  • auctioneers, sales houses, restaurateurs
  • archaeological research projects

Its approach is based on three pillars:

  • Cutting-edge technical expertise (AMS, micro-analysis, spectrometry) and state-of-the-art technologies
  • Personalized scientific support
  • A perfect understanding of the cultural and economic issues associated with each object

Thanks to its state-of-the-art equipment and multi-disciplinary team, CIRAM supports its customers from the sampling stage (choice of sampling point) right through to the interpretation of results, taking into account historical, stylistic and material constraints.

Carbon-14 dating is still the reference method for dating and authenticating objects made of organic materials, whether they come from the archaeological field or the art market. Whether you're a private collector or an archaeologist on a preventive excavation site, a good understanding of how this dating method works, its practical applications and its technical limitations, will enable you to make the most of it. 

However, it is essential to work with a specialized laboratory capable of guaranteeing the reliability of the results, and of applying a rigorous scientific approach in order to document the history of your object.

CIRAM, Europe's leading laboratory, is recognized for the quality of its radiocarbon dating analyses, its customized support and its in-depth knowledge of cultural heritage issues.

Would you like to have one or more works of art or archaeological artifacts analyzed? Contact the CIRAM team today to take advantage of our expertise in carbon-14 dating tailored to your needs.

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The post-atomic bomb effect has profoundly renewed our understanding of carbon-14. The radiocarbon peak resulting from the more than 500 nuclear tests carried out between the 1950s and 1960s has left a unique temporal signature. Today, this signature is exploited by scientists for carbon-14 dating for the art market and the analysis of organic materials such as wood, ivory, bone, teeth, linen, straw, paper and other textiles.

For art professionals who rely on authentication techniques to identify objects that can be composited or restored, the post-bomb effect represents an opportunity to make provenance more reliable. Mastery of post-bomb reference frames (Northern/Southern hemisphere) and isotopic corrections is therefore essential to guarantee the reliability of results and their interpretation (provenance, historical consistency, due diligence).

In this article, we clarify the mechanisms and analytical implications of the post-bomb effect, detail carbon-14 measurement by AMS and calibration reference frames applied to art. You will also find case studies (linen canvases, wooden stretchers, papers, ivories, bones/teeth) and explanations of the role of an expert laboratory like CIRAM in transforming a carbon 14 measurement into scientific evidence useful to experts, auction houses, galleries, museums and collectors.

Carbon-14 and the post-bomb effect: mechanisms & analytical implications

Mastering the isotopic behavior of carbon 14 lays the foundations for rigorous dating and credible authentication.

Carbon-14 dating in art contexts: principles, the Suess effect and analytical issues

The sudden increase in atmospheric carbon-14 following nuclear testing generated a very distinct radiocarbon curve, known as the "bomb-peak". Nuclear bombs led to a massive production of radiocarbon from 1954 onwards, almost doubling its concentration in 1963 and 1964. This allows us to draw a strict line between organisms that lived before and after 1954. This isotopic anomaly, long perceived as a disturbance, has become a time marker of unprecedented precision for scientists. 

Carbon-14, produced by cosmic rays, is integrated into living organic matter (plants, animals). Measuring carbon enables us to date a variety of materials: wood, plant fibers (linen, straw, paper), ivory, bone and teeth. 

Two notable phenomena are upsetting the natural balance:

  • Suess effect: burning fossil CO₂ (without carbon 14) reduces the proportion of atmospheric carbon 14
  • Post-bomb effect: conversely, nuclear testing greatly increased carbon-14 concentrations (peaking between 1963 and 1964).

Unlike conventional carbon-14 dating (which is limited to a few hundred years' accuracy for recent periods), the post-bomb signal enables organic material to be dated to within ±1-2 years between 1954 and 2020. The abnormal concentration of carbon 14 in living organisms that lived after 1954 is ideal for spotting recent fakes.

Identifying this over-concentration is particularly useful for :

  • Determining whether an object is pre or post-1954: a critical threshold for "modern" or "post-war" objects
  • Check whether a work claimed to be from 1963, for example, was actually produced during the radiocarbon peak (which is measurable).
  • Distinguish between old ivory (pre-CITES) and modern, illegally harvested ivory.

What materials can be dated using the post-bomb effect?

The post-bomb effect exclusively concerns materials of organic origin that have incorporated atmospheric carbon after 1954. Here are the main materials that can be analyzed using post-bomb analysis:

  • Wood (supports, stretchers, sculptures): to distinguish modern from old wood, to identify a replaced stretcher or a datable restoration, or to spot young wood in a supposedly old work.
  • Linen canvases, papers, textiles: it's possible to date the fiber (and not the paint), to reveal a post-1960 canvas behind a 19th-century attribution or, for example, to check the homogeneity of the constituent elements (canvas, lining, passe-partout, collage).
  • Ivories, bones, teeth: analysis can show that a supposedly ancient ivory is in fact modern (post-bomb signal), or on the contrary, confirm the absence of a bomb-pulse.

However, there are limits and precautions to be noted:

  • Carbon-14 dating targets the material sampled: dating canvas ≠ dating paint and dating wood ≠ dating sculpture.
  • Restorations (PVA adhesives, varnishes, consolidants) can contaminate organic materials, so targeted sampling and appropriate pre-treatment (alpha-cellulose extraction for fibers, collagen purification for bone/dentine or acid-alkali acid procedures, ultrafiltration, etc.) are essential.
  • Old reused wood exists (which is rare but possible): it is then crucial to cross-reference this method with xylology/dendrochronology, imaging and provenance studies.

Each material, depending on its origin, preparation and possible treatments, requires a rigorous sampling strategy, which CIRAM establishes in collaboration with curators, restorers and experts.

Post-bomb carbon-14 measurement methods for the art market

Gas pedal Mass Spectrometry (AMS): precision, reliability and use cases

Gas pedal coupled mass spectrometry (AMS) is the reference method for post-bomb in art. It directly measures carbon ratios ¹⁴C, ¹³C and ¹²C with excellent sensitivity from micro-quantities (discrete samples, not visible after intervention).

This technology enables :

  • Micro-sampling : analysis of very small quantities of material (a few milligrams): linen thread, wood flakes, ivory micro-splinters, paper fibers.
  • Ability to handle restored materials (with appropriate decontamination protocols).
  • Results in pMC (percent Modern Carbon), with a precise calendar interval.

The process takes place in several stages:

  1. Targeted sampling (masked areas, edges, excess wire)
  2. Pretreatment: mild/strong solvents depending on matrix, alpha-cellulose extraction (fibers/paper), collagen purification (bone/ivory), varnish/glue removal.
  3. Graphitization to isolate pure carbon
  4. AMS measurement with isotope correction via δ¹³C
  5. Interpretation according to the post-bomb frame of reference (North or South) and submission of a documented scientific report.

Reference systems, calibration and interpretation: making the material speak

CIRAM uses post-bomb calibration curves published by the scientific community (such as NH1, NH2, NH3, SH1-2, SH3) to convert measured pMC into calibrated dates. This reading enables us to answer specific questions:

  • Was the work created before or after 1954?
  • Does the material correspond to a production made after the artist's death?
  • Is it possible to distinguish an original piece from a modern reproduction based on the same material?

To convert a measurement into proof, laboratories specializing in carbon-14 dating for art:

  • Use post-bomb calibration curves (different NH/SH) reflecting changes in atmospheric carbon-14 since 1954
  • Apply international standards and deliver comparable results (pMC/Fcarbon 14, probable year interval)
  • Interpret results on a case-by-case basis: they relate support, context, presumed geographical origin, restoration history and sampling strategy.

Thanks to the post-bomb effect, each variation in pMC becomes a clock, and each work a witness to its era. CIRAM follows comprehensive QA/QC protocols (blanks, bomb-peak standards, duplicates, yield validation) and records every step. Reports are quotable, written in operational language (useful for sales catalogs, expert reports, committees and insurers).

The post-bomb effect and the art market: broader use cases & the role of laboratories

Advanced use cases for art: from suspicion to opposable proof

Post-bomb analysis is particularly useful for art market professionals in the following cases:

  • Authentication of modern works: this can prove, for example, that a material actually dates from the 1960s-1970s.
  • Detection of fakes or imitations: this identifies materials that are too recent to be consistent with the advertised attribution.
  • Regulatory compliance (CITES): this differentiates pre-1975 ivory (legal) from more recent ivory (prohibited).
  • Litigation or insurance: it is used to establish scientific proof that can be used in the event of a dispute or claim.

Here are a few examples of how post-bomb analysis can be used by art professionals and collectors:

  • 19th century" painting on canvas: with linen dating. If a bomb-pulse is detected, then the canvas is post-1954. We can therefore consider a replacement canvas, an apocryphal work, or a copy.
  • Drawing on paper: the absence or presence of a post-bomb signal can validate or disqualify an alleged dating. This analysis is particularly useful in the case of contested archives or manuscripts.
  • Assemblies, collages, marouflages: cross-dating (support, lining, glue) enables us to reconstruct the chronology of interventions. This analysis is essential for insurance purposes.

In the end, a post-bomb analysis transforms a doubt (stylistic incoherence, incomplete provenance, contentious signatures) into an objective scientific element that can be understood by a committee, a court or an auction house.

CIRAM: from samples to authentication arguments

The scientific teams at CIRAM laboratories provide end-to-end support to art market professionals. Their action covers several stages: 

  1. Framing: choice of the most convincing material (flax vs. glue, frame wood vs. key, dentin vs. dental cement, etc.), proposal of a micro-sampling strategy, anticipation of contamination risks.
  2. AMS measurement: implementation of procedures dedicated to organic art materials, NH/SH references, isotopic corrections, management of mixed matrices.
  3. Interpretation & writing: creation of a clear, citable report, presenting results (pMC/Fcarbone 14), post-bomb calendar interval, uncertainty, interpretation scenarios and reasoned conclusion.
  4. Confidentiality: signature of an NDA, anonymization of samples, secure circuits, traceable chain of custody. This is a key issue for sensitive dossiers.

If the situation requires it (depending on the subject of the study), CIRAM also carries out complementary analyses (FTIR for binders and glues, dendrochronology for wood, imaging for interventions, pigments and/or binders on a pictorial layer) in order to provide a coherent material reading.

Far from being a scientific curiosity, the post-bomb effect has become an indispensable tool for authenticating works of art. Thanks to post-1954 carbon-14 dating, it is now possible to provide rigorous scientific proof of the temporal origin of organic materials such as wood, ivory, linen and paper. When properly used, post-bomb analysis strengthens authentication, identifies restorations, secures sales and protects collectors and institutions alike. The key to a successful study lies in appropriate sampling, rigorous AMS protocols and contextualized interpretation.

With its experience of art market issues, CIRAM transforms carbon 14 measurements into legible evidence, which can be integrated into appraisals, catalogs and due diligence procedures. As an expert laboratory in dating and material characterization for the art market, CIRAM puts its skills, cutting-edge equipment and customized support at your disposal to transform every carbon-14 analysis into usable, documented and enforceable proof.

If you would like to have your art object(s) analyzed by the leader in carbon-14 dating in France, contact the CIRAM teams and request your study.

Carbon-14 dating - Multiple uses

Reading time:

3–5 minutes

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Carbon-14 dating is the most widely used dating method. It applies to all organic materials such as wood, charcoal, bone, teeth, paper, textiles, ivory and plant macroremains. 

Find out more about its scope of action and the methods used to meet your needs. 

In summary:

  • Carbon-14 dating makes it possible to date organic materials up to about 60,000 years old and to establish their chronology.
  • Using accelerator mass spectrometry (AMS), it provides accurate results from very small amounts of material.
  • This method is essential in archaeology, for authenticating works of art and detecting recent forgeries.
  • In industry, it makes it possible to quantify the proportion of bio-based and fossil carbon in materials, in accordance with regulatory requirements.

The Importance of Carbon-14 in Materials Analysis 

Radiocarbon analysis was developed in the 1940s and is based on the physical properties of the 14 isotope of carbon. This isotope is radioactive, meaning that it is unstable over time. It will disappear and be transformed into nitrogen. Every 5,730 years, the concentration of carbon 14 is halved, disappearing completely after 60,000 years. The quantity of carbon is stable for living beings, because on the one hand, carbon 14 disintegrates, but on the other, it is reintegrated through respiration or photosynthesis. This is why C14 dating will date the death of the individual (or plant), i.e. the moment when the disappearance/integration equilibrium is broken. 

Cutting-edge technologies for analyzing carbon-14 

For radiocarbon measurement, we use state-of-the-art technologies such as elemental analysis (EA), isotope ratio mass spectrometry (IRMS), automatic graphitization and particle gas pedal mass spectrometry (AMS). The AMS method requires very little material (1 mg of carbon vs. 1g previously), for a more accurate result than the liquid scintillation technique. 

An Essential Analysis for Archaeological Excavations 

Charcoal and bone are very good chronological markers in an archaeological dig, as they are closely linked to the stratigraphy in which they are found. This is why carbon-14 dating is the most widely used scientific technique to support archaeological excavations. Depending on the period, dating accuracy can range from forty years to several centuries. 

Authenticating Works of Art Through Radiocarbon Analysis 

Carbon 14 will also be used to authenticate works of art, such as wooden or ivory sculptures, or painting supports, such as textiles and paper.  

It's important to note that organisms that lived after 1950 have a very high 14C concentration, far exceeding the "classic" concentration of the carbon isotope 14 compared to the other two isotopes. This is mainly due to atmospheric nuclear testing, which resulted in massive radiocarbon production. That's why there's a real dating frontier in 1950. This boundary is ideal for formally identifying recent fakes. Moreover, post-1950 dating is exceptionally accurate. 

C14 Analysis in the Agri-Food and Industrial Sectors 

Radiocarbon analysis is also used in industry to qualify biobased products and quantify their biogenic and petroleum-based components. As mentioned above, after 60,000 years, carbon 14 has completely disappeared. As petroleum is derived from the decomposition of organic matter over millions of years, it no longer contains any 14C. Conversely, biomass (i.e. living organisms) is "full" of carbon-14. Radiocarbon analysis enables us to distinguish between the proportion of biosourced/biogenic carbon (modern) and fossil carbon (ancient) present in all types of material, whether solid, liquid or gaseous. We measure the ratio of 14C, 13C and 12C isotopes in a sample. Although the proportion of 14C is very low (1 atom of 14C for 1012 atoms of 12C), it is nevertheless present in all molecules containing modern carbon".

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