Stable carbon and oxygen isotope analysis of human and animal tooth enamel carbonate has been used as a proxy for individual diet and environmental reconstruction. Here, we provide a detailed description and visual documentation of bulk and sequential tooth enamel sampling as well as pretreatment of archaeological and paleontological samples.
Stable carbon and oxygen isotope analysis of human and animal tooth enamel carbonate has been applied in paleodietary, paleoecological, and paleoenvironmental research from recent historical periods back to over 10 million years ago. Bulk approaches provide a representative sample for the period of enamel mineralization, while sequential samples within a tooth can track dietary and environmental changes during this period. While these methodologies have been widely applied and described in archaeology, ecology, and paleontology, there have been no explicit guidelines to aid in the selection of necessary lab equipment and to thoroughly describe detailed laboratory sampling and protocols. In this article, we document textually and visually, the entire process from sampling through pretreatment and diagenetic screening to make the methodology more widely available to researchers considering its application in a variety of laboratory settings.
Stable carbon and oxygen isotope analyses of tooth enamel carbonate has been used to study past human dietary intake, weaning, and mobility, as well as faunal reliance on vegetation, the movement of animals, and livestock foddering. These applications have been comprehensively discussed and reviewed for a variety of environmental conditions indicating the effects of local aridity, temperature, water sources, and vegetation compositions1,2,3,4,5,6. The diversity of potential applications in archaeology and paleontology, as well as the good preservation of tooth enamel carbonate, has made it an attractive material for stable isotope work3. Methods of sampling, pretreatment, and diagenesis screening are briefly described in a number of previous publications1,7. However, thorough verbal and visual demonstrations remain largely unavailable, particularly to people outside of archaeological science laboratories and among laboratory groups with limited funding where the interest in the use of this technique is increasing5.
Tooth enamel is primarily made up of hydroxyapatite (bioapatite) crystallites8 larger than those in bone, making it more resistant to post-mortem diagenetic ionic substitutions and contamination3. Modern studies have demonstrated that stable carbon isotope (δ13C) measurements of faunal tooth enamel reliably record animal diet and behavior9,10. The stable oxygen isotope (δ18O) value of tooth enamel is determined by the oxygen isotopic composition of ingested water, which includes water in plant and animal foods, drinking water, respiration, as well as various environmental impacts on the water which can lead to further isotopic fractionation (e.g., aridity, temperature, altitude, rainfall amount, continental location)11. This has made it a popular method for dietary and environmental reconstruction in archeological, paleoecological, and paleontological research.
The period of tooth enamel formation is relatively short (years) and differs depending on the tooth being sampled. For humans, first molar enamel mineralizes between birth and 3 years of age, premolars mineralize between 1.5 and 7 years of age, second molars mineralize between 2.5 and 8 years of age, and third molars mineralize during adolescence, between 7 and 16 years12. Given that tooth enamel forms incrementally over its period of formation, it can be sampled in bulk along the entire growth axis or sampled sequentially in order to investigate the changes in diet and environment that have occurred during the formation period13. Chronologically-ordered dietary change within a given tooth is observable for humans and other animals1,14, providing information regarding inter-annual seasonal and dietary variation.
While enamel is usually resistant to diagenesis, isotopic modifications resulting from the burial environment are possible and have been observed15,16, making experimental checks and pretreatment choices useful. While it is not the only available method, Fourier transform infrared spectroscopy (FTIR), particularly in Attenuated Transmission Mode, has emerged as a quick, inexpensive, and relatively accessible method for assessing taphonomic alteration in tooth enamel, particularly in paleontological contexts17,18,19,20. However, detailed protocols and recording standards remain relatively inaccessible to many people outside the fields of geochemistry or material science.
Reaction times and the chemicals employed by researchers in the pretreatment of tooth enamel also vary considerably in the literature, often with limited consideration as to what this variability may do to stable carbon and oxygen isotope values of the sample21,22. Here, we report an approach that uses dilute acetic acid (0.1 M) for the pretreatment of enamel powder samples. However, given that the differences in isotopic measurements resulting from pretreatment are relatively minor for tooth enamel, it is best for the researchers to follow the protocols for datasets with which they wish to compare their data to11. Furthermore, where small sequential samples are taken, particularly on Holocene samples, no pretreatment may be chosen (following pilot diagenetic tests) to avoid sample wastage.
Although the methods we report here are by no means new, to our knowledge, this is the first time that a thorough written and visual documentation of bulk and sequential sampling, pretreatment choices, and diagenetic check methods (in the form of FTIR) for tooth enamel have been made widely available to a varied academic audience. While we hope our efforts will make this approach more easily accessible to a wider number of individuals and laboratories, researchers who want to apply and publish this technique must be aware of minimum reporting standards, diagenetic considerations, and presentation requirements overviewed elsewhere20, as well as potential interpretive complexities that will be unique to their study region, taxa analyzed, and time period5.
The following protocol follows the guidelines of the Light Isotope Mass Spectrometry Laboratory at the Max Planck Institute for the Science of Human History. Appropriate ethics permissions from national and international committees should be sought for analyses involving endangered modern or historical faunal specimens, and for the use of archaeological and faunal material of interest to contemporary stakeholders. In this paper, the samples used were archaeological and fossil specimens. No living humans were used in this study and full ethical, institutional, and governmental permissions have been gained for any destructive analysis.
1. Bulk Sampling
Note: For humans and animals, the basic method of bulk tooth enamel sampling is the application of a drill to the buccal edge of the tooth.
2. Sequential Sampling
Note: Sequential sampling can be approached in a variety of forms and will depend on the taxon being sampled, the size of the tooth, as well as the desired temporal resolution.
3. Fourier Transform Infrared Spectrometry/Attenuated Total Reflectance method
4. Simple Acetic Acid (0.1 M) Pretreatment
5. Weighing and Measuring Samples and Standards
Using the sampling procedure presented above, incremental enamel bioapatite samples were prepared. The analysis of bioapatite in enamel depends on the accuracy of sampling, whether bulk or incremental. In this case, we have chosen to present the results of archaeological samples (two sheep) from different climatic zones. Incremental samples were analyzed from sheep second molars and labelled starting at the ERJ (Figure 4). Incremental sample locations were numbered, and each location was measured as its distance in mm from the ERJ (Figure 7).
Diverse carbon and oxygen stable isotope results from the two sheep confirm that they lived in different environments, in this case a tropical grassland (A) and a temperate dry-steppe grassland (B), respectively. Incremental δ18O values for sheep A show a narrow range between 3.3 to 5.1‰, suggesting the ingestion of water sources with similar isotopic values and a lack of strong seasonal shifts in precipitation (Figure 8). In contrast, δ18O values for sheep B have a high amplitude of variation, ranging from ─5.2 to ─13.1‰, indicating strong seasonal variation in precipitation. Stable carbon isotope values suggest strong differences in ingested vegetation between samples, with sheep A having a diet consisting mainly of C4 plants, while sheep B ingested primarily C3 vegetation. These sheep were specifically chosen to demonstrate environmental variation evident in incremental oxygen and carbon stable isotope results.
Human teeth are similarly sampled from the ERJ to the crown along the growth axis. Incremental δ18O and δ13C values for a human tooth from a rainforest environment are highly constrained, within a 2‰ range. This suggests a lack of variation in foraging strategies over the period of enamel mineralization (Figure 9).
Figure 1: Drilling a Tooth. (A) Photo of a tooth being drilled on a rig set up. (B) Photo of enamel powder being collected in tin foil and placed into a 1.5 mL micro-centrifuge tube (with proper label). (C) Photo of different drill bits available for incremental sampling. Please click here to view a larger version of this figure.
Figure 2: Rig set up. Photo of rig set up with the drill in place. Please click here to view a larger version of this figure.
Figure 3: Sample preparation. Sample being placed into a micro-centrifuge tube and agitated on a vortex after chemicals were added. Please click here to view a larger version of this figure.
Figure 4: Incrementally sampled sheep teeth. Sheep teeth (A and B) that were incrementally sampled. Please click here to view a larger version of this figure.
Figure 5: Chromatogram of gasbench run. Photo of a chromatogram of one sample displaying intensity of reference gas peaks and sample peaks over time. Detected masses are 44, 45 and 46. The first three peaks are CO2 reference gas peaks with a known isotopic composition. Ten peaks that follow are sample peaks decreasing in intensity. Peaks should always be separated by several seconds to ensure a strict discrimination between the peaks and hence a clean peak integration. Numbers on top of each peak state the time (s) of peak detection. Please click here to view a larger version of this figure.
Figure 6: Weighing carbonate sample. Photo of sample being weighted into glass vials using a spatula. Please click here to view a larger version of this figure.
Figure 7: Incremental samples on a sheep tooth. Incremental samples along the growth axis of the tooth from the ERJ to the top of the crown plotted alongside carbon and oxygen stable isotope values. Please click here to view a larger version of this figure.
Figure 8: Sheep enamel carbonate isotope results. Stable oxygen and carbon isotope values for two incrementally sampled sheep teeth. Please click here to view a larger version of this figure.
Figure 9: Human enamel carbonate isotope results. Stable oxygen and carbon isotope values for an incrementally sampled human tooth. Please click here to view a larger version of this figure.
PCI (Phosphate Crystallinity Index) | Sponheimer and Lee-Thorp, 1999b | |
other names: | ||
CIIR (Crystallinity Index InfraRed) | Shemesh, 1990 | |
IRSF (InfraRed Splitting Factor) | Weiner and Bar-Yosef, 1990 | |
BPI (B-carbonate on Phosphate Index) | LeGeros, 1991 | |
API (A-carbonate on Phosphate Index) | Sponheimer and Lee-Thorp, 1999b | |
BAI (relative amount of B- to A-site carbonate) | Sponheimer, 1999; Sponheimer and Lee-Thorp, 1999b | |
WAMPI (Water-Amide on Phosphate Index) | Roche et al., 2010 |
Table 1: Empirical indices that characterize the crystal-chemical properties of enamel bioapatite. We recommend using the empirical indices from Sponheimer (1999), Sponheimer and Lee-Thorp (1999), and Roche et al. (2010) to characterize the crystal-chemical properties of enamel bioapatite.
The challenges of successful sampling (bulk and incremental) of dentition relies on the access to knowledge regarding drilling techniques and sample preparation, alongside the investment in relatively inexpensive equipment. These challenges are easily surmountable when clear instructions are available concerning sampling and pretreatment approaches. In this article, we hope to have disseminated these in a clear, concise fashion for researchers new to these methods. Scholars applying these methods for the first time should practice on accessible modern fauna prior to the analysis and sampling of valuable archeological and paleontological samples.
The sampling of human and animal tooth enamel carbonate for stable isotope analysis is a simple procedure that has been undertaken at multiple laboratories. However, there is a tendency for techniques and technology associated with the drilling of dentition to vary by laboratory and be included in a broader set of insider technical knowledge that is not shared openly. Incremental sampling has major advantages, permitting the identification of detailed intra-individual variation in dietary intake and the ingestion of water. This is illustrated by compelling the differences found between individuals from different regions as dietary and environmental information is preserved in tooth enamel bioapatite. In our representative data, significant isotopic variation is evident between the sheep from tropical grasslands compared to the sheep from temperate dry-steppe grasslands (Figure 8).
Critical steps within the protocol are related to the accuracy in drilling, preservation of tooth enamel, and pretreatment techniques. Small inaccuracies in drilling, for example, through the enamel into the tooth dentine, could result in hugely variable isotope measurements29. The preservation of tooth enamel can be checked through a variety of methods, including the estimated carbonate proportion of a given sample measured, as well as the FTIR set-up discussed here. Researchers should also inform the laboratories of the burial environment, specifically whether water-logged or in acidic soils, which can affect the structural preservation of fossil tooth enamel. The hardness of tooth enamel should be considered as an initial indicator of preservation, which may only become evident during drilling. Enamel that is soft and easily drilled suggests that the bioapatite crystal lattice may have degraded and should be checked with FTIR or other means reported in the literature30. The variation in sample pretreatment seems to result in limited isotopic variation in tooth enamel21,22. Therefore, we suggest the use of simple protocols (e.g., 0.1 M acetic acid for less than 4 h followed by washing with distilled water).
There are several limitations to the technique, associated with the sampling design and interpretation. Drilling sequential samples is a skill that takes some time to master. A clear understanding of the taxa and tooth to be analyzed is essential in formulating a sampling design2,25. Further, drilling of samples can take a considerable amount of time to complete. However, the resulting carbon and oxygen stable isotope values for sequentially sampled dentition allow the researchers to track dietary and environmental changes. As these changes are related to natural seasonal variations, often in ancient periods, thoughtful interpretations that are contextualized within an understanding of variation in isotopic reference sets are integral to this research6.
In the article, we have demonstrated incremental sampling and bulk sampling of both human and sheep dentition. Further, we instruct the researchers on pretreatment methods for both sample sets. Incremental sampling method can be successfully applied to ancient and modern fauna with similar enamel growth and mineralization (e.g., cattle and horses). Pretreatment of enamel bioapatite as shown in the article can be used on samples from a cross-section of ancient remains. The most important lesson from our sampling procedure is bulk and incremental sampling of dentition, which is not easily explained in a document. Further demonstrations could democratize other archaeological isotope sampling and pre-treatment approaches (e.g., bone collagen extractions or the sampling of archaeological pottery for stable isotope measurements of fatty acids) enhancing the spread of knowledge and technology in this field. Such democratization should not, however, be seen as a complete replacement for consultation with the experts, or the available literature, to establish the standards of measurement and interpretation in a given context20,28.
The authors have nothing to disclose.
We would like to thank the Max Planck Society for funding this research as well as the recent setting up of a Stable Isotope laboratory at the Department Archaeology, Max Planck Institute for the Science of Human History.
Dremel Micro | Dremel | https://www.dremel.com/en_US/products/-/show-product/tools/8050-micro | |
Diamond-tipped drill bit | Dremel | https://www.dremel.com/en_US/products/-/show-product/accessories/7122-diamond-wheel-point | |
1.5 mL micro-centrifuge tube | Sigma Aldrich | https://www.sigmaaldrich.com/catalog/product/sigma/t2422?lang=de®ion=DE&gclid=EAIaIQobChMI7pHRpauW2QIV77ftCh1p1wjhEAAYASAAEgKzkvD_BwE | |
Methanol | Linear Formula: CH3OH | ||
Acetic Acid | Linear Formula: CH3CO2H | ||
Dremel rig set-up (workstation) | Dremel | https://www.dremel.com/en_US/products/-/show-product/tools/220-01-workstation | |
Microcentrifuge | Thermo Scientific | http://www.thermofisher.com/order/catalog/product/75002401 | |
Mini-centrifuge | Sprout | http://www.heathrowscientific.com/sprout-mini-centrifuge-4 | |
Freeze drier | Zirbus Technology | http://www.zirbus.com |