© August, 2004
Updated: January 2010
Table of Contents
All living things use proteins as building blocks in the construction of
their physical forms. In turn,
proteins are composed of folded strands of 20 different smaller subunits called
"amino acids". All amino acids, except for one (glycine), come in two
different forms known as the levoratory (L - left) and dextrorotary (D - right)
forms. These two forms are called
"enantiomers", "chirals", or "stereoisomers",
which basically means that they have the same molecular and structural formula
but cannot be superimposed on each other no matter how they are oriented in
space. In other words, they are
like one's left and right
hands, which are mirror images of each other, but cannot be superimposed onto one
What is especially interesting about these two L- and D-forms, at least for the purposes of this topic, is that the vast
majority of living things only use the L-form.
However, as soon as the creature dies, the L-amino acids start to
spontaneously convert to the D-form through a process called
"racemization". If the rate of conversion can be determined, this process of
racemization might be useful as a sort of "clock" to determine the time of death.
order to use the rate of racemization as a clock to accurately estimate when a
living thing died, one must know how various
environmental factors may have affected the rate of change from the L- to the
D-form. As it turns out, this rate,
which is different for each type of amino acid, is also exquisitely sensitive to
certain environmental factors. These
Amino acid composition of the protein
Water concentration in the environment
pH (acidity/alkalinity) in the environment
Bound state versus free state
Size of the macromolecule, if in a bound state
Specific location in the macromolecule, if in a bound state
Contact with clay surfaces (catalytic effect)
Presence of aldehydes, particularly when associated with metal ions
Concentration of buffer compounds
Ionic strength of the environment
these, temperature is generally thought to play the most significant role in
determining the rate of racemization since a 1o
increase in temperature results in a 20-25% increase in the racemization rate.1,2
Clearly, this factor alone carries with it a huge potential for error. Even
slight ranges of error in determining the "temperature history" of a
specimen will result in huge "age" calculation errors.
for even a known temperature history also seems to be rather problematic.
Consider that the rate of racemization for various amino acids is
determined by placing a protein into a very high temperature environment
and 150o C) and
then extrapolating these results to low temperature environments.1
extrapolations have been fairly recently (1999) called into question by
experiments showing that models based on high temperature kinetics fail to
predict racemization kinetics at physiologic temperatures (i.e., 37o C). The
authors of this particular paper went on to suggest that, "As conformation
strongly influences the rate of Asu [cyclic succinimide] formation and hence Asx
[aspartic acid + asparagine] racemization, the use of extrapolation from high
temperatures to estimate racemization kinetics of Asx in proteins below their
denaturation temperature is called into question . . . We argue that the D:L
ratio of Asx reflects the proportion of non-helical to helical collagen "3
Others, such as Collins and Riley have commented in the press that,
in free amino acids has, unfortunately, little bearing on observed racemization
of archaeological biominerals."1
experiments have shown that the L- and D-forms of the same amino acid do not
racemize at the same rate. This
means that the equilibrium ratio may be off from "50:50" by as much as
far as pH is concerned, it seems that the temperature of a solution also affects
the pH of that solution. So, the
amino acid racemization (AAR) rates not only change with the effects of
temperature, but also with the concurrent effects of pH changes, which are
themselves affected by temperature.1 This can only increase the
potential range of error for age determinations.
The local buffering effects of bone and shell matrixes are supposed to
limit this effect, but it is still something to consider as potentially
significant when acting over the course of tens of thousands to millions of
the actual physical structure of an intact protein significantly affects the
rate of racemization of various amino acids.
In fact, in many cases this may even be a more significant factor than
the temperature history. As it
turns out, the N-terminal amino acids racemize faster than the C-terminal amino
acids of the same types. Also, the
surface amino acids racemize much faster than the interior amino acids.
And, interestingly enough, free amino acids have the slowest racemization
rate of all. Studies with short
peptides have shown that, "replacement
of the asparagine residue with aspartic acid resulted in a 34-fold
decrease in the rate of succinimide (Asu) formation. In the position carboxyl to
asparagine in the peptide the replacement of glycine with a bulky amino acid
such as proline or leucine resulted in a 33-50-fold decrease in the rate
of deamidation"1 [Emphasis added] This clearly emphasizes the
rather dramatic importance that amino acid position and overall protein amino
acid sequence has on the racemization rate.
or the process of breaking down a protein into smaller and smaller fragments,
clearly affects the rate of racemization. The rate itself of hydrolysis
"depends on the strength of the individual peptide bonds, which in turn is
determined by the characteristics of the amino acids on either side of the bond,
the presence of water and the temperature."1 With increased
hydrolysis, the overall rate of the whole specimen would increase since there
are more terminal end and surface amino acids to undergo higher rates of
racemization. All of these are
confounding factors, which, if not known exactly over extended periods of time,
would play havoc with any sort of age determinations. Even the process of
preparing a specimen for racemic dating can affect the D/L ratio.
this light, consider that age determinations are usually performed on specimens
for which the amino acid order of the original proteins is unknown.
For example, consider that neither the structure nor the proportion of
the amino acids used for dating coral, ostrich eggshell, or snail shells is
known. Again, those like Goodfriend and Hare (1995) have pointed out the
"difficulties in estimating the amount of asparagine in proteins and
reminded researchers of the dangers of extrapolating from the behaviour of pure
Asn in solution at high temperature, to the behaviour of Asn in proteins
associated with biominerals at ambient temperature . . . Using
a simplified model of 'racemization kinetics' of bone collagen over geological
time Collins shows that almost any value of D-Asx can be obtained by varying the
rates of collagen denaturation and
leaching of the denatured product."1
The Interaction of bacteria and fungi with organic specimens may also be problematic. Such creatures have various enzymes that can digest various types of proteins, such as collagen, that are commonly used for dating. Various studies, such as those dealing with 18th and 19th century burials, showed "unexpectedly high levels of aspartic acid racemization." The authors "suggested that either biological or chemical degradation of the tooth collagen might have caused these results." 1 Also, certain types of bacteria and other creatures actually produce the D-form instead of the L-form of amino acids. So, special care is obviously needed in order to particularly avoid this sort of contamination.
"Amino acid dating cannot obtain the age of the material purely from the data itself. The rate of racemization can not be standardized by itself because it is too changeable. Thus, because of the rate problem, this dating technique must rely on other dating techniques to standardize its findings. As a matter of fact, the ages obtained from racemization dating must rely on other techniques such as Carbon 14, and if the dating of Carbon 14 is not accurate, racemization dating can never be certain."6
"The potential variation in the racemization rate has led some paleoanthropologists to consider this dating technique relative rather than chronometric. It is, perhaps, best considered to be a calibrated relative dating technique which puts it somewhere between relative and chronometric methods."7
See additional references on the relative nature of amino acid racemization dating in the addendum section ( Link )
all of the above described variables for amino acid racemization rates create great difficulty for
AAR as a
dating technique. In fact, the
difficulties are so great that this technique cannot be and is not used as any
sort of "absolute" dating technique. So, how is it
thought to be at all helpful? Well,
it is thought to be helpful as a "relative" dating technique.
To overcome the various uncertainties
inherent to amino acid dating, the method must be "calibrated" based
on other more reliable techniques such as radiocarbon dating (carbon 14 dating).
What happens is that a specimen from a site is chosen as the
"calibration sample" and both a radiocarbon date as well as a D/L
amino acid ratio is determined. These
values are used to solve for a constant or "k" in the formula used to
estimate ages based on the calibration sample.
Of course, the "major assumption required with this approach is that the
average temperature experienced by the 'calibration' sample is representative of
the average temperature experienced by other samples from the deposit."1
Much effort has gone into transforming the
data in various ways to achieve linearity between the D/L ratio and the
calibrated age of the specimens in a given location.
At first "cubic transformations"' and then later "power
function transformations" were used that seemed to show a "strong
correlation with time, but did not explain the observed kinetics."
What this basically means is that amino acid
dating is not based on any sort of understanding about how racemization takes
place, but is strictly a function of correlation with other dating techniques,
such as the radiocarbon technique. So, if there is any problem with the basis of
the correlation (i.e., radiocarbon dating) then there will also be the same
problem with amino acid dating.
In this light, it is interesting to consider what happened in 1974 when some of the major proponents of amino acid dating (Bada et al) decided to analyze the Paleo-Indian skeletal material from Del Mar, California. Their estimated age of 48,000 years before present (BP) "stunned" the archaeological community who generally believed these bones to be less than 10,000 years old. Bada went on to date other skeletal specimens between the 35,000 and 48,000 year range with one specimen from Sunnyvale being dated at an astonishing 70,000 years BP. Then, in the 1980s, something very interesting happened.
"The Sunnyvale skeleton and the Del Mar tibia were re-dated using uranium series dating. This resulted in dates of 8,000 to 9,000 years BP for Sunnyvale and 11,000 to 11,500 for Del Mar. Conventional plus accelerator mass spectrometry (AMS) radiocarbon dating (Taylor et al. 1983) was carried out on the Sunnyvale skeleton and results of between 3,600 and 4,850 years BP were obtained. The original amino acid extractions from the racemization studies of the Paleo-Indian remains were independently dated by the AMS radiocarbon method at the Oxford Radiocarbon Accelerator Unit of Oxford University and the NSF Accelerator Facility for Radioisotope Analysis, University of Arizona. Bada et al., (1984) published the Oxford results and Taylor et al., (1985) published a paper combining the results from both laboratories. The Oxford dates were all between 4,500 and 8,500 years BP and the Arizona dates were between 3,000 and 6,600 years BP. Bada et al., (1984) stated that the Oxford AMS results reveal no clear relationship between the radiocarbon ages of the various skeletons and the extent of the aspartic acid racemization. They did note that there appeared to be a direct relationship between the extent of racemization and the level of preservation of collagen in the bones. Those samples with the most racemization had the lowest amino acid content and this poor preservation of protein would contribute to anomalous AAR results.
Later, based on AMS radiocarbon dates, Bada (1985) calculated a new value for kasp for the Californian samples. He used the Laguna skull and the Los Angeles Man skeleton as 'calibration' samples for this. Using the revised value for kasp he recalculated the AAR dates of the other Paleo-Indian samples. They all fell within the Holocene but had much larger error estimates than those of the AMS values. Although Bada claimed consistency between AAR and AMS dates others (Pollard and Heron 1996, p. 228) argue that the dates only appear to be consistent with one another because of the unacceptably large error range associated with the AAR dates. Pollard and Heron also point out that there is poor concordance between the conventional and the AMS radiocarbon dates and there is no concordance between the uranium series dates and any of the other dates either. At best three of the four methods put the bones in the Holocene."1
Because of these problems AAR dating of bone and teeth (teeth in different locations in the same mouth have been shown to have very different AAR ages) is considered to be an extremely unreliable practice even by mainstream scientists. That is because the porosity of bones makes them more "open" to surrounding environmental influences and leaching. Specimens that are more "closed" to such problems are thought to include mollusk shells and especially ratite (bird) eggshells from the emu and ostrich. Of course, even if these rather thin specimens were actually "closed" systems (more so than even teeth enamel) they would still be quite subject to local temperature variations as well as the other above-mentioned potential problems. For example, even today "very little is known about the protein structure in ratite eggshell and differences in primary sequence can alter the rate of Asu formation by two orders of magnitude [100-fold] (Collins, Waite, and van Duin 1999). Goodfriend and Hare (1995) show that Asx racemization in ostrich eggshell heated at 80 oC has complex kinetics, similar to that seen in land snails (Goodfriend 1992). The extrapolation of high temperature rates to low temperatures is known to be problematic (Collins, Waite, and van Duin 1999). A pilot study would be necessary and a reliable relationship between racemate ratio and time could remain elusive."1
The Changing Correlation Constant (k)
Also, there is a potential problem with radiocarbon correlations that is quite interesting. Note what happens to the correlation constant (k) with assumed age of the specimen in the following figures.
Interestingly enough, the racemization
constant or "k" values for the amino acid dating of various specimens
decreases dramatically with the assumed age of the specimens (see figures).5
This means that the rate of racemization was thousands of times (up to 2,000
times) different in the past than it is today.
Note that these rate differences include shell specimens, which are
supposed to be more reliable than other more "open system" specimens,
such as wood and bone.
Is this a reasonable assumption?
Well, this simply must be true if radiocarbon dating is accurate beyond a
few thousand years. But, what if
radiocarbon gets significantly worse as one moves very far back in time beyond
just a few thousand years? In other
words, what would it mean for one to assume that the k-values remained fairly
constant over time as would seem intuitive?
Well, with the k-values plotted out horizontally on the graph, the
calculated ages of the specimens would be roughly affected as follows:5
Current Fossil Age Assignment
Adjusted Fossil Age Assignment with horizontal k-values
Clearly this is a dramatic adjustment that seems to suggest that amino acid racemization may be more a reflection of the activities of local environmental differences than any sort of differences in relative ages. This seems especially likely when one considers that each type of specimen and each different location have different k-values meaning that the radiocarbon-derived constant in one region or with one type of specimen cannot be used to calculate the age of any other specimen or even the same type of specimen in a different location.1
Radiocarbon Calibration Dependent Upon State of Preservation
Add to this the fact that radiocarbon dating is also dependent upon the state of preservation of the specimen.
"Stafford et al., (1991) discussed AMS radiocarbon dating in bone at the molecular level. They dated a number of fractions (ranging from insoluble collagen to individual amino acids) from each of a selection of differentially preserved mammoth and human bone. Age estimates from the fractions within a bone were consistent if it was well preserved. They concluded that a poorly preserved Pleistocene-age fossil >11,000 years in age would go unrecognised because it would yield a Holocene 14C date. Thus the final irony is that the poorly preserved Californian Paleo-Indian bones would return Holocene 14C dates even if they were actually Pleistocene. The state of preservation of the bone appears to be as important an issue for radiocarbon dating as it is for AAR dating."1
So, what do we have? In short, it seems like the claims of some scientists that amino acid racemization dating has been well established as reliable appears to be wishful thinking at best. The huge number of confounding factors and a complete inability to explain the calibrating k-values in terms of amino acid kinetics leaves those with even a tiny pessimistic bone in their bodies just a bit underwhelmed.
Optically Active Petroleum:
For many decades the observation that petroleum shows optical activity, usually favoring L-enantiomers, was used to prove the biogenic origin of petroleum. However, more recently there have been scientists who have argued for the non-biogenic origin of petroleum, citing situations where optical activity can be produced in non-organic materials, to include hydrocarbons. A particularly impressive proof of this hypothesis was the discovery of L-enantiomers in proteins within meteorites ( Link ).
Subsequent analysis by Bada et. al., challenged this demonstration of L-enantiomers within meteorites, suggesting that this particular finding is the likely result of contamination rather than in situ formation of optical activity within the meteoric proteins ( Link ).
However, in 1997 research showed that individual amino-acid enantiomers from Murchison were enriched in the nitrogen isotope 15N relative to their terrestrial counterparts, which seemed to suggest an extraterrestrial source for an L-enantiomer excess in the Solar System ( Link ).
Then in 2001 a paper by Pizzarello and Cooper again seemed to confirm the contamination argument for the origin of optical activity for amino acids within meteorites. There is currently still some debate, but the consensus seems to currently favor the contamination theory ( Link ).
This is all very interesting because optical activity decays over time toward a racemic state. Optically active petroleum is usually found with temperatures of 66 degrees Celsius. At such temperatures, optical activity should not be maintained for more than 10 or 20 million years at most. Yet, optical activity within petroleum, usually of the L-enantiomeric type, seems to be maintained in significant degrees despite ages assumed to be over 300 million years old? How is this explained?
Robins, Martin Jones and Elizabeth Matisoo-Smith, Amino
Acid Racemization Dating in New Zealand: An overview and Bibliography,
Auckland University, Auckland, New Zealand, March 20, 2001 ( Link
Brown, Amino Acid Dating, Molecular History Research Center and Mikes
Origins Resource, Accessed July, 2004 ( Link
Collins MJ, Waite ER, van Duin AC, Predicting protein decomposition: the case of aspartic-acid racemization kinetics. Philos Trans R Soc Lond B Biol Sci 1999 Jan 29;354(1379):51-64 (Fossil Fuels and Environmental Geochemistry (Postgraduate Institute), NRG, University of Newcastle-upon-Tyne, UK. ( email@example.com )
MW, Meyer VR, Ramseyer S, The kinetics of diastereomeric amino acids with o-phthaldialdehyde,
Chirality 1991;3(6):471-5 PMID: 1812958, UI: 92256092 (Institute of
Organic Chemistry, University of Bern, Switzerland)
H. Brown, Amino Acid Dating, Origins 12(1):8-25 (1985). ( Link
Minnesota State University, Racemization essay, accessed December 2, 2007 ( Link )
Dennis O'Neil, "Chronometric Techniques - Part 1," Palomar.edu, June 7, 2007 ( Link )
Regarding the relative nature of amino acid racemization dating - i.e., the requirement for calibration against another dating method for a local area:
"D/L aspartic acid ratios cannot be converted into an age estimate unless a suitable known age reference sample is available for calibration of the aspartic acid racemization rate, e.g., kasp value (Bada 1985; Bada et al. 1979). In the case of the California paleoindian skeletons, the original racemization ages were derived using the Laguna skeleton dated by conventional radiocarbon method (Beta-counting) . . . "
Jeffrey L. Bada, Aspartic Acid Racemization Ages of California Paleoindian Skeletons, American Antiquity, Vol. 50, No. 3 (Jul., 1985), pp. 645-647. ( Link)
Amino-acid ratios can be used for either relative or absolute dating. Absolute dating requires calibration with radiometric techniques, such as radiocarbon dates, and knowledge of the temperature history of the fossil. Once such information is established for a region, amino-acid dating may be used with confidence. However, amino-acid time calibration cannot be extended beyond the area of study due to regional differences in temperature history.
In those articles I show that after 'calibrating' the amino acid racemization reactions using a radiocarbon dated bone, it is then possible to date other bones from the same site, which are either too old or too small for radiocarbon dating. The only assumption in this approach is that the average temperature experienced by the calibration sample is representative of the average temperature experienced by the other sample. Ages thus deduced are in good agreement with radiocarbon ages determined on the same samples.
Carroll uses amino acids with C-14 dating to come up with a calibration curve.
To overcome the problem of inherent uncertainty in the temperature history of sub-fossil bone Bada and colleagues (Bada and Protsch 1973; Bada et al. 1974) developed a .calibration" method for dating bones using aspartic acid racemization. A bone from a site was chosen as a .calibration" sample and both a radiocarbon date and a D/L aspartic acid ratio were determined. These values were substituted into equation ( 2.4) on page 15 and it was solved for k. The result was an in situ kasp value for the site. After substituting in this k asp value equation (2.4) on page 15 was used to determine the age of other samples from the site for which only D/L aspartic acid values had been determined. The major assumption required with this approach is that the average temperature experienced by the .calibration" sample is representative of the average temperature experienced by other samples from the deposit.
More recently researchers have developed calibration curves using a number of age estimations by independent dating methods (e. g. radiocarbon) and considerable effort has gone into transforming data in various ways to achieve linearity in the relationship between D/L ratio and age. Goodfriend et al., (1992) used a cubic transformation of D/L data for aspartic acid to achieve linearity. Later, power function transformations were used for D/L ratios in both mollusc and ostrich shells (Goodfriend and Hare 1995; Goodfriend 1996). Such transformations allow a strong correlation with time but do not explain the observed kinetics.
By determination of the amount of racemization of aspartic acid in bones from a particular location which have been dated by the radiocarbon technique, it is possible to calculate the in situ first-order rate constant for interconversion of the L- and D enantiomers of aspartic acid. Once this "calibration" has been calculated, the reaction can be used to date other bones from the deposit that are either too old to be dated by radiocarbon or that are too small for radiocarbon dating. The only assumption required with this approach is that the average temperature experienced by the "calibration" sample is representative of the average temperature experienced by older samples.
This study explores time-averaging (temporal mixing) at very high sampling resolution: that of adjacent shells collected from the same stratum. Nine samples of the bivalve Chione fluctifraga were collected from four Holocene cheniers (beach ridges) on the Colorado Delta (Gulf of California) and 165 shells were dated using radiocarbon-calibrated amino-acid racemization (D-alloisoleucine/L-isoleucine).
There is a book by a vertebrate paleontologist on dating methods pertinent to vertebrate paleontologists. It says little about amino acid racemization, but simply dismisses it with the comment that it is of little value to vertebrate paleontology because of its heavy dependence on calibration by carbon 14.
- Leonard Brand, paleontologist, LLU, personal letter, December 2007
"Two approaches to calibrating 14C and AAR are used. Interval calibration involves multiple AAR analyses (>10) of Mulinia from previously 14C dated core intervals. Both linear and non-linear regressions of D/L Asp against 14C age yield comparable R-squared values (0.91), but the intercept value has not yet been determined by analysis of modern samples. Direct calibration, currently in progress for 8 samples, involves both AAR and 14C analysis of separate valves from articulated Mulinia individuals. Because direct calibration results are not influenced by time-averaging, they should provide insights into the reliability of the interval calibration.
Use of AAR data to assess time-averaging not only requires a calibration curve but also an understanding of all factors that cause a spread in D/L values for a given core interval. For intervals with >10 analyses, the coefficient of variation (CV) for D/L Asp is between 3 and 10%, with only two intervals having CV's >7%. These ranges may be interpreted as "normal scatter" around an analytical mid-point, with all samples being essentially the same age, however, time-averaging (as represented by larger CV's) seems most pronounced within a region of slow or interrupted deposition at ~1150 cm core depth, between 2800 and 5600 cal yrs BP." [emphasis added] ( Link)
EDWARDS, A. L. 1 , WEHMILLER, J.1, LOCKWOOD, R.2, KAUFMAN, D.3, BRIGHT, J. 3, CRONIN, T.4, and WILLARD, D.4, HOLOCENE AMINOCHRONOLOGY AND TIME-AVERAGING FOR CHESAPEAKE BAY MULINIA, 2005 Salt Lake City Annual Meeting (October 16â€“19, 2005)
"Before using AAR ratios in fossils for dating, several tests need to be completed to ensure that the racemization reaction meets the criteria for the first order linear reversible or parabolic kenetics needed for dating (Fig. 4). The two pronged approach using both modern kinetic studies and calibrated tests on fossils applied to develop AAR dating for ostrich egg shells is an excellent example.
In high temperature kinetic experiments, the fossil species to be dated is heated at several different temperatures for various times. After using the Arrhenius equations (Eq 6) to determine a rate constant for each temperature tested ( e.g., Fig. 10a), the rate constants are plotted versus temperature (e.g., Fig. 10b) and extrapolated to Earth surface temperatures. If this method is used in isolation, then the curve must be assumed to extrapolate linearly to lower temperatures, an assumption that cannot be guaranteed without calibration at low temperatures (Blackwell, 1987; Rutter & Blackwell, 1995).
Calibration tests use several fossils from several diverse sites that have been accurately and precisely dated by another technique, such as C-14, etc. . ." [emphasis added]
William M. Last & John P. Smol, Tracking Environmental Change Using Lake Sediments, Published 2001, Springer, ISBN 0792364821 ( Link)
"With suitable calibration, racemization data can also be used to construct a history of temperature for the samples in question. Understanding diagenetic amino acid racemization (AAR) kinetics requires a combination of laboratory kinetic experimentation and testing of kinetic models with natural field samples that have independent chronostratigraphic control. These models must also incorporate information on the temperature dependence ("apparent" or "bulk" activation energy) as derived from either elevated temperature laboratory experiments or data from field samples with known ages and diagenetic temperatures. Over the past two decades, several well-calibrated datasets and a variety of kinetic models have become available: foraminifera results provide calibration for low temperature kinetics ( e.g., Muller, 1984) and paired radiocarbon-AAR results provide calibration at higher surface temperatures (e.g., Miller et al., 1997)." [emphasis added]
Wehmiller, J. F., Amino acid racemization kinetic modeling and the late Quaternary paleoclimate of the North Carolina coastal plain, American Geophysical Union, Fall Meeting 2004, abstract #OS43A-0535 ( Link)
"AAR is not a numerical dating method, per se; however, it can be used for a variety of chronological and palaeotemperature applications. Provided there is some independent age control, AAR can be used to extend or to improve upon the chronology, or to reconstruct the temperature history at a site."
B. J. JOHNSON, G. H. MILLER (1997), ARCHAEOLOGICAL APPLICATIONS OF AMINO ACID RACEMIZATION*, Archaeometry 39 (2), 265â€“287. ( Link)
"The increase in the proportion of D-amino acids (a function of time and temperature) can be used as a tool for estimating age. Attempts to provide absolute dates calibrate the amount of racemization using samples of known age and then use these predict the age of samples with known D/L values but of unknown age. A recent paper by Kaufman (in press Geology) estimates that the compound accuracy of this approach is +/- 20%." [accessed 11/29/07] ( Link)
"Although the finding of this dating method was meaningful, this dating method is considered controversial. The rate of racemization is dependent on temperature, or the thermal history of the fossil. The rate of racemization increases at warmer sites than at cooler sites. Samples from areas of different latitude tend to have greater age range differences. To obtain accurate dates, the temperature has to be constant for thousands of years. The speed of racemization slows down if the sample materials gets cold. The study carried out with bone revealed that unassured temperature of plus or minus 2 degree will cause an plus or minus 50% error of the age.
Amino acid dating cannot obtain the age of the material purely from the data itself. The rate of racemization can not be standardized by itself because it is too changeable. Thus, because of the rate problem, this dating technique must rely on other dating techniques to standardize its findings. As a matter of fact, the ages obtained from racemization dating must rely on other techniques such as Carbon 14, and if the dating of Carbon 14 is not accurate, racemization dating can never be certain.
Materials can easily be contaminated. Sample material can lose or gain amino acids by leaching, diagenetic formation of amino acids, bacterial contamination, and/or contaminated during collection or preparation. If the materials are contaminated by water, their racemic clocks will be ruined. Even though there must be some moisture for the occurrence of racemization, continual inflow of moisture can cause many kinds of contamination. For example, if pH of the moisture is higher, the racemization process would be very rapid, and that changes the age of the sample." [Bibliography with almost all references from 2000] ( Link)
"The potential variation in the racemization rate has led some paleoanthropologists to consider this dating technique relative rather than chronometric. It is, perhaps, best considered to be a calibrated relative dating technique which puts it somewhere between relative and chronometric methods." [accessed 11/29/07] ( Link)
"If the racemization rate for a particular system in any given material is known then AAR can be used to estimate the thermal history of any cross-dated samples. However, good independent age controls such as 14C dated samples and a reliable kinetic model for racemization rates are needed (Johnson and Miller 1997)."
Judith Robins, Martin Jones and Elizabeth Matisoo-Smith, Amino Acid Racemization Dating in New Zealand: An Overview and Bibliography, Auckland University, Private Bag 92019, March 20, 2001 ( Link)
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