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(The FASEB Journal. 1999;13:559-562.)
© 1999 FASEB


Research Communications

The Ice Man's diet as reflected by the stable nitrogen and carbon isotopic composition of his hair

S. A. MACKOa , G. LUBECb , 1 , M. TESCHLER-NICOLAc , V. ANDRUSEVICHd and M. H. ENGELd


a Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia 22903; USA;

b Department of Pediatrics, University of Vienna, Vienna, Austria;

c Department of Anthropology, Vienna, Austria; and

d School of Geology and Geophysics, University of Oklahoma, Norman, Oklahoma 73019, USA


   ABSTRACT
TOP
ABSTRACT
INTRODUCTION
MATERIALS AND METHODS
RESULTS
DISCUSSION
REFERENCES
 
Establishing the diets of ancient human populations is an integral component of most archaeological studies. Stable isotope analysis of well-preserved bone collagen is the most direct approach for a general assessment of paleodiet. However, this method has been limited by the scarcity of well-preserved skeletal materials for this type of destructive analysis. Hair is preserved in many burials, but is often overlooked as an alternative material for isotopic analysis. Here we report that the stable carbon and nitrogen isotope values for the hair of the 5200 year-old Ice Man indicates a primarily vegetarian diet, in agreement with his dental wear pattern. Whereas previous investigations have focused on bone collagen, the stable isotope composition of hair may prove to be a more reliable proxy for paleodiet reconstruction, particularly when skeletal remains are not well preserved and additional archaeological artifacts are unavailable.—Macko, S. A., Lubec, G., Teschler-Nicola, M., Andusevich, V., Engel, M. H. The Ice Man's diet as reflected by the stable nitrogen and carbon isotopic composition of his hair.


Key Words: stable isotopes • amino acids • paleodiet • neolithic


   INTRODUCTION
TOP
ABSTRACT
INTRODUCTION
MATERIALS AND METHODS
RESULTS
DISCUSSION
REFERENCES
 
TRADITIONAL METHODS FOR the determination of paleodiets are often based on incomplete and sometimes misleading archaeological records of, for example, faunal and floral remains, artifacts or other cultural evidence, and dental records of ancient populations. Subsequent to early reports that the stable isotope composition of heterotrophs tend to reflect the isotope compositions of their respective diets 1; 2) , there have been numerous attempts to use this approach for paleodietary reconstructions, including ancient human populations (e.g., refs 3; 4 ) and even dinosaurs (5) . Work on ancient populations has focused on the stable isotopic analysis of bone collagen, the assumption being that the preservation of bone collagen is sufficient to retain the original isotopic signal of the organism. However, even under the best of circumstances, bone collagen tends to be altered by diagenetic reactions such as hydrolysis, decarboxylation, and deamination (6) . Thus, how closely the stable isotope composition of residual collagen is likely to reflect that of the original biomolecule has been the topic of much debate (e.g., ref 7 ).

An alternative proteinaceous material that is commonly encountered in ancient human burials is hair. Consisting of {alpha}-keratins, which include hair and fingernails as well as horn, skin, and wool (8) , hair is composed of hydrophobic proteins that are not easily degraded (9) . The microbial degradation of these insoluble macromolecules depends on the secretion of extracellular enzymes with the ability to act on the surface. Keratins have a mechanical stability dependent on the tight packing of the {alpha}-helix, and can be degraded by a few species of parasitic and saprotrophic fungi as well as thermophilic anaerobic bacteria (10, 11).

Minagawa (12) recently demonstrated that the stable carbon and nitrogen isotope compositions of modern human hair are a reliable indicator of the diets of these individuals. Based on these and our own isotopic studies of modern hair (S. A. Macko and M. H. Engel, unpublished results), we hypothesize that it should be possible to estimate the paleodiets of ancient humans based on the stable isotope composition of their hair. Hair is often observed at archeological sites and potentially could be used to show not only dietary differences, but also short time scale variation in diet, perhaps on a seasonal basis. Collagen, on the other hand, represents a material that is on a longer time scale integration of dietary preferences. By using several hairs at different distances from the roots, hair can similarly be used in an integrative fashion. The relationships between the isotopic compositions of collagen and hair have not been well established, although the isotopic composition of hair appears to exhibit the previously observed 3{per thousand} shift with trophic level (13, 14)

Here we report a first test of this hypothesis, focusing on reconstruction of the paleodiet of Ice Man, who was preserved in a glacier of the Oetztaler Alps during the neolithic period, ~5200 years ago. Farming was already widespread in Europe at that time, and meat and crops were readily available (15) . Plant and pollen material found in association with the Ice Man confirm the availability of cereals (16) , and suggest that these materials could have been a portion of his diet. Furthermore, the pronounced dental attrition/abrasion of the Ice Man's teeth (16) point to a predominantly herbivorous diet.


   MATERIALS AND METHODS
TOP
ABSTRACT
INTRODUCTION
MATERIALS AND METHODS
RESULTS
DISCUSSION
REFERENCES
 
Hair samples
Hair samples from the Ice Man were provided by Dr. G. Wortmann, Deutsches Wollforschungs Institut, Aachen, Germany. For comparison, modern hair samples were also analyzed from two vegans (individuals who reported that they consumed no animal protein) and from nine other individuals who either described themselves as vegetarians (deriving nutrition from plants, eggs, or milk products: ovo-lacto-vegetarians) or subsisted on an omnivorous diet (one of the authors, S.A.M.). The hair samples, consisting of several strands of hair of different lengths, were cleaned with distilled ethanol to remove any possible superficial debris and minimize the levels of surface lipids on the hair. Although the keratin structure is a protein, the presence of lipids could strongly bias the carbon isotope signal if they were not removed. In addition we examined samples of the goat fur that was found with the Ice Man. Finally, stable isotope analyses were also performed on samples of a grass-like plant, a possible dietary source of the goat recovered in association with the Ice Man. With these samples, we hoped to allow for a representation of the potential diets available to the Ice Man—the goat being a meat source, and the grass allowing for the isotope signals of plants to be suggested. These samples are in all likelihood the best ones for comparison, since they represent materials of precisely the same age and reduce the potential for variation due to geography, climate, and the effects of modern fertilizers and fossil fuel on the carbon pools.

Amino acid distributions and stereochemistry
Given the expectation that even well-preserved ancient hair keratin will likely have undergone alteration to some minor extent (17) , samples of the author's (S.A.M) hair and that of the Ice Man were analyzed for their respective amino acid distributions as a first approximation of relative preservation. The individual hair samples were hydrolyzed (6N HCl, 24 h, 100°C) and the resultant hydrolysates were analyzed for their amino acid distributions by high performance liquid chromatography (postcolumn derivatization with o-phthaldialdehyde) using the method of Hare et al. (18) . Whereas proline has been reported to be a component of keratin, it could not be detected by the high-performance liquid chromatographic method used in this study. Proline, however, was observed in the analyses done by gas chromatography (GC)2 but was not quantified. Aliquots of the hydrolysates of the Ice Man's hair and of the modern hair (S.A.M.) were derivatized and analyzed by GC using an optically active stationary phase (Chirasil-Val) to determine the extent to which amino acids may have been racemized. Details of the GC method are reported elsewhere (19) .

Stable isotope analyses
Stable carbon and nitrogen isotope analyses of the individual hair samples, the grass-like plant, and the goat fur were performed using a Carlo Erba elemental analyzer interfaced to a Micromass Optima isotope ratio mass spectrometer. Details of the method are reported elsewhere (20) . Stable carbon and nitrogen isotope values are presented by using the standard convention:

where N is the heavier stable isotope of the element E, and R is the abundance ratio of the heavy to light isotopes of the element (i.e., 13C/12C or 15N/14N). The reference for {delta}15N is air (0%); values have a standard deviation of 0.2{per thousand}. The reference for {delta}13C is NBS-22 (-29.8{per thousand}) relative to PDB carbonate (0%); values have a standard deviation of 0.2{per thousand}.


   RESULTS
TOP
ABSTRACT
INTRODUCTION
MATERIALS AND METHODS
RESULTS
DISCUSSION
REFERENCES
 
Compared to modern hair, the Ice Man exhibited, as expected, slight decreases in the absolute abundances (Fig. 1A ) of several unstable amino acids (e.g., serine, threonine). However, the relative percentages of individual amino acids that comprise the modern hair and that of the Ice Man were remarkably similar (Fig. 1B ). The elevated percentages of hydrophobic amino acids (e.g., leucine, alanine, glycine, valine, isoleucine) in the Ice Man hair sample are consistent with the distribution observed for the modern hair keratin, and may in part account for its resistance to hydrolysis subsequent to interment. The fact that none of the amino acid constituents of the Ice Man's hair exhibited any indication of partial racemization above background also supports excellent preservation of this ancient hair keratin. In addition, the low C/N seen in the hair (3.2 to 3.4) is consistent with that of pure proteins.



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Figure 1. A) Amino acid concentrations in the Ice Man and modern hair. B) Relative distribution of amino acids in the Ice Man and modern hair.

The stable carbon and nitrogen isotope values for the Ice Man's hair and the associated remains of goat fur and grass-like plants (Table 1 ) provide some significant clues with respect to his diet. Depending on the complexity of a food web, {delta}13C values of an organism's protein may show slight to moderate enrichment in 13C relative to diet (6) . However, the key to distinguishing trophic levels of heterotrophs is the stable nitrogen isotope composition of their proteins. This is because with increasing progression in a food chain, the {delta}15N values of protein of organisms tend to become from 2 to 3{per thousand} enriched relative to the preceding (lower) food chain level (6) because most of the animal's nitrogen is derived from the protein of its food (21, 22). As will be discussed below, a {delta}15N value of 7.0 for the Ice Man clearly points to a primarily vegetarian diet, consistent with the tooth abrasion observed for this specimen (Fig. 2 ).


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Table 1. Stable isotope values of hair and plant samples



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Figure 2. Photograph showing abrasion of the Ice Man's teeth.


   DISCUSSION
TOP
ABSTRACT
INTRODUCTION
MATERIALS AND METHODS
RESULTS
DISCUSSION
REFERENCES
 
With the remains of goat fur found on this site, one might intuitively suggest that goat meat was a significant component of the Ice Man's diet. However, if this were the case, the stable nitrogen isotope composition of his hair should have been 3{per thousand} enriched relative to the goat {delta}15N value, and clearly this is not so. Rather, the {delta}15N value for the Ice Man's hair is approximately 3{per thousand} enriched relative to the {delta}15N values of plants, indicating that plants were likely a primary component of his diet at the time of his death. The stable nitrogen isotope composition of the Ice Man is consistent with that observed for modern vegetarians with low levels of animal protein in their diet (Table 1) and who are depleted in 15N by several per milligram relative to modern humans on omnivorous diets. The goat should reflect the vegan diet, being enriched by 3{per thousand} over primary production. In all likelihood it does, but represents an integration of browsing on a variety of terrestrial plants, some of which may be more depleted in 15N owing to nitrogen fixation. The fact that the {delta}13C value of the Ice Man was depleted in 13C reflects a high percentage of grains in the diet that can be attributed to plants that utilized the C-3 pathway for photosynthesis (Table 1) . In general, C-3 plants (e.g., wheat, rice, legumes) are depleted in 13C by 5 to 15% relative to C-4 plants (e.g., corn) due to differences in enzymes used for the primary fixation of carbon (e.g., ref 23 ). A similar preference for C-3 plants (or for organisms that subsisted on C-3 plants) was reflected in the diets of the other omnivores, all of which are expected to be enriched in 13C by a few per milligram relative to their respective C-3 sources. Strict adherence to only vegetation is not suggested, however. Small amounts of animal protein in the diet, as well as variation in the isotopic signals of potential plant and animal foods, could be masked by the consumption of large amounts of plant proteins.

In summary, stable isotopes provide a powerful probe for the reconstruction of paleodiets of organisms. Our initial results indicate that when hair is well preserved, under burial conditions such as mummification, its stable isotope composition can be used to help reconstruct the paleodiet of the individual by making use of very small amounts (milligram quantities) of material. Our stable isotope results confirm the initial indication of a vegetarian diet for the Ice Man that was based on the abrasion of his teeth.


   ACKNOWLEDGMENTS
 
We thank Dr. G. Wortmann and the British Museum for providing the hair samples. S.A.M. and M.H.E. acknowledge the National Science Foundation (Geology and Paleontology) for support of this research. We also are grateful for the efforts of the two anonymous reviewers. G.L. is highly indebted to the Red Bull Company, Salzburg, Austria, for generous financial support.


   FOOTNOTES
 
1 Correspondence: University of Vienna, Dept. of Pediatrics, Waehringer Guertel 18, A 1090 Vienna, Austria. E-mail: GERT.LUBEC{at}AKH-WIEN.AC.AT

2 Abbreviation: GC, gas chromatography.

Received for publication March 23, 1998. Revision received October 29, 1998.
   REFERENCES
TOP
ABSTRACT
INTRODUCTION
MATERIALS AND METHODS
RESULTS
DISCUSSION
REFERENCES
 

  1. DeNiro M. J., Epstein S.. Influence of diet on the distribution of carbon isotopes in animals. Geochim. Cosmochim. Acta 1978;42:495-506.
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