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Dietary ecology is key to understanding the lifeways and evolutionary pathways of many animals, but determining the diets of long-extinct primates, including early hominins, is a considerable challenge. Although archeological evidence forms a pillar of our understanding of diet and subsistence in the more recent past, for early hominins, the most direct evidence is to be found in the fossils themselves. Here we review the suite of emerging biochemical paleodietary tools based on stable isotope and trace element archives within fossil calcified tissues. We critically assess the contribution of these tools to advancing our understanding of australopith, early Homo, and Neanderthal diets, and placed within the context of contributions of morphological and microwear tools. Perhaps the most significant outcomes to date are the demonstration of high trophic-level diets among Neanderthals in Glacial Europe, and the persistent inclusion of significant amounts of C4 grass-related foods in the diets of both the South African australopiths and Homo in the Pliocene and Pleistocene. These results raise new questions that require improved contextual understanding of these tools from modern ecosystems, but they also clearly show a good deal of promise as quantitative indicators of hominin diets that nicely complement morphological and microwear tools.
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Contributions of Biogeochemistry to Understanding
Hominin Dietary Ecology
Julia Lee-Thorp
1*
and Matt Sponheimer
2
1
Archaeological Sciences, University of Bradford, Bradford BD1 7DP, UK
2
Department of Anthropology, University of Colorado at Boulder, Boulder, CO 80309
KEY WORDS fossil teeth; stable isotopes of carbon; nitrogen and oxygen; trace elements;
microwear; dental morphology; australopiths; Homo; Neanderthals
ABSTRACT Dietary ecology is one key to understand-
ing the biology, lifeways, and evolutionary pathways of
many animals. Determining the diets of long-extinct hom-
inins, however, is a considerable challenge. Although
archaeological evidence forms a pillar of our understand-
ing of diet and subsistence in the more recent past, for
early hominins, the most direct evidence is to be found in
the fossils themselves. Here we review the suite of emerg-
ing biochemical paleodietary tools based on stable isotope
and trace element archives within fossil calcified tissues.
We critically assess their contribution to advancing our
understanding of australopith, early Homo, and Neander-
thal diets within the broader context of non-biogeochemi-
cal techniques for dietary reconstruction, such as mor-
phology and dental microwear analysis. The most signifi-
cant outcomes to date are the demonstration of high
trophic-level diets among Neanderthals and Late Pleisto-
cene modern humans in Glacial Europe, and the persis-
tent inclusion of C
4
grass-related foods in the diets of
Plio–Pleistocene hominins in South Africa. Such studies
clearly show the promise of biogeochemical techniques for
testing hypotheses about the diets of early hominins.
Nevertheless, we argue that more contextual data from
modern ecosystem and experimental studies are needed if
we are to fully realize their potential. Yrbk Phys Anthro-
pol 49:131–148, 2006. V
V
C2006 Wiley-Liss, Inc.
It is widely recognized that the pursuit and consump-
tion of food exerts a major influence on the behavior,
ecology, and biology of all animals. Most large primates
spend a large proportion of their waking hours searching
for, consuming, and digesting food (e.g., Altmann and
Altmann, 1970; Teleki, 1981; Goodall, 1986; Whiten
et al., 1991), and diet underlies ecological niche distinc-
tions. Consequently, dietary adaptations can be consid-
ered as one of the key drivers determining the pathways
of hominin evolution. The nature of hominin diets has
been the subject of lively debate and not a little specula-
tion for many years (e.g., Dart, 1926, 1957; Robinson,
1954, 1956; Jolly, 1970), although in recent years the
topic has received somewhat less attention than bipedal-
ism and brain expansion (Teaford and Ungar, 2000). The
importance of dietary ecology is clear, but determining
the diets of extinct hominins remains a considerable
challenge. Most primates are generalists, so pinpointing
their diets and dietary differences is no simple matter
even among extant animals, where observational studies
continue to generate new information and surprises. For
instance, more detailed observations of gorillas in a vari-
ety of environments have shown that they are less
devoted to folivory than previously believed, and that
their diets overlap considerably with those of chimpan-
zees in many areas (Tutin and Fernandez, 1992). The
difference lies to a significant extent in their fallback
foods; in times of stress gorillas can better rely on foli-
age. So how best can we investigate the diets of species
that have been extinct for many thousands or millions of
years?
We can glean paleodietary information from many
sources. However, some of the conventional sources of
contextual evidence may be inappropriate, or at best pro-
vide very indirect, limited, or ambiguous information
about diet. Archeological evidence in the form of stone
tools, animal bone scatters and their spatial contexts is
the conventional source of information about past human
diet and subsistence. There are, however, severe limita-
tions in applications to the early fossil record, particu-
larly where stratified archeological evidence is rare.
Moreover, even where stratigraphy (or good spatial con-
text) exists, the nature of association between the animal
bones and human behavior is often controversial (e.g.,
Binford, 1981; Brain, 1981). There are significant inter-
pretive problems associated with most Pliocene and
Lower Pleistocene bone accumulations, where the sites
are essentially palimpsests and the assemblages may
have accumulated over hundreds to thousands of years.
Traces that survive best are scatters of bones and stone
tools which may indicate procurement strategies and
butchery of vertebrate animal foods (e.g., Binford, 1981;
Brain, 1981; Blumenschine, 1987; Stiner, 1994; Marean
and Assefa, 1999; Speth and Tchernov, 2001). Yet, even
where these traces occur, the information they provide
can be ambiguous. For instance, the function of stone
Grant sponsors: National Research Foundation (South Africa),
National Science Foundation (USA), University of Bradford, Univer-
sity of Cape Town, University of Colorado at Boulder, the Leakey
Foundation, the Palaeoanthropology Scientific Trust.
*Correspondence to: Julia Lee-Thorp, Department of Archaeologi-
cal Science, University of Bradford, Richmond Road, Bradford BD1
7DP, UK. E-mail: j.a.lee-thorp@bradford.ac.uk
DOI 10.1002/ajpa.20519
Published online in Wiley InterScience (www.interscience.wiley.com).
V
V
C2006 WILEY-LISS, INC.
YEARBOOK OF PHYSICAL ANTHROPOLOGY 49:131–148 (2006)
tools and the identities of their manufacturers (i.e.,
whether early Homo or australopith) is often uncertain
(Brain, 1981). At present, the earliest known stone tools
and cut-marked bones are from Gona and Bouri in
Ethiopia, dated to *2.5 Ma (Semaw et al., 1997; de
Heinzelin et al., 1999; Dominguez-Rodrigo et al., 2005),
while the first potential hominins (Leakey et al., 2001;
Senut et al., 2001; Brunet et al., 2002; White et al.,
2006) precede these earliest archeological traces by mil-
lions of years. Thus archeological traces can tell us noth-
ing about the diets of our lineage for most of its history.
Finally, the prominence of bones and stone tools in the
record inevitably focuses attention on animal foods,
whereas plant foods make up the bulk of most primate
diets (Milton, 2002) and are likely to have been just as
important for early hominins. Overall, technological
attributes and spatial distributions of Oldowan and
Acheulian stone tools may tell us more about the cogni-
tive and fine-motor capabilities of their makers (Ambrose,
2001) and their use of the landscape (Isaac, 1981; Fe
`blot
Augustins, 1997) than they do about their dietary ecology.
As a result, paleoanthropologists have had to develop
other sources of palaeodietary information to fill these
gaps. Many are focused largely on teeth—dental mor-
phology and allometry, dental microwear, and trace ele-
ment and stable isotope analysis. These techniques have
advantages and limitations that are peculiar to each
approach. Morphology and allometry, for instance, pro-
vide general indications about the capability of a species
to process foods with certain mechanical properties, rely-
ing heavily on comparisons with living primates (Kay,
1975a, b, 1985). Dental microwear and chemical tools
also rely on comparisons with modern systems for inter-
pretation, but they are more immediate and direct indi-
cators of palaeodiet. Microwear, in turn, is largely lim-
ited to telling us about the mechanical properties or con-
sistency of foods eaten (Walker, 1981; Teaford, 1988a;
Teaford and Ungar, 2000). The information available
from chemical analyses in the form of stable light isotope
and trace element patterns in bones and teeth is limited
to certain broad dietary classes. Postmortem taphonomy
and diagenesis remains an ever-present problem that
can compromise or destroy dietary information for both
microwear and chemical approaches (Teaford, 1988b;
Sillen, 1989; Koch et al., 1997; Kohn et al., 1999; Lee-
Thorp, 2000; Pe
´rez-Pe
´rez et al., 2003; Lee-Thorp and
Sponheimer, 2005).
Given the distinct limitations for each approach,
ideally, they should form a complementary suite. Since
we cannot observe what early humans were eating,
inferences about early human diets are perforce indirect.
Several comprehensive reviews of dental allometry, mor-
phology, and microwear exist in the literature (Kay,
1985; Ungar, 1998; Teaford and Ungar, 2000; Teaford
et al., 2002). In this article, we provide brief overviews
of these approaches to give sufficient contextual informa-
tion to gauge the contributions of biogeochemical tools to
hominin diets. We concentrate largely on applications to
dietary ecology of the australopiths and Neanderthals,
simply because this is where we have most biogeochemi-
cal data.
DENTAL ALLOMETRY AND MORPHOLOGY
The function of teeth is to process foods, and they are
abundant in the fossil record; hence the relative size and
shape of teeth has been an important source of informa-
tion for many years. Robinson (1954, 1956) observed that
the \robust"australopith, Paranthropus robustus, had
absolutely smaller incisors and larger molars than did the
gracile australopith, Australopithecus africanus, and he
deduced that these differences reflected functional spe-
cializations. Specifically, Robinson argued that Paranth-
ropus had an herbivorous diet that required grinding
large quantities of tough plant foods, while A. africanus
had a more omnivorous diet that required relatively more
incisal preparation of meat and other foods (Robinson,
1956). This work was influential and set the stage not
only for subsequent allometric and morphological studies
of teeth, but also for hypothesis testing of the dietary pro-
clivities and differences between the South African aus-
tralopiths (e.g., Grine, 1981, 1986; Grine and Kay, 1988;
Scott et al., 2005; Sponheimer et al., 2005a).
While continuing to consider the functional implica-
tions of relative tooth size of both anterior and posterior
teeth in primates, subsequent studies have attempted to
deal with a central problem. That is, since basal meta-
bolic rate and molar occusal surfaces are generally
scaled in a similar way to body size (by *0.75), molar
size should be positively scaled to body size, because
larger surfaces can process greater amounts of food (Pil-
beam and Gould, 1974). Therefore, tooth size (particu-
larly molar occlusal area) must be considered in relation
to body size. However, this information is often unavail-
able or poorly known for the majority of fossil primates,
including hominins. A related problem is that certain
foods need a great deal more chewing or preparation
than others. In an attempt to control this problem, Kay
(1975a) compared primate taxa with similar diets. He
showed that primate posterior tooth surface area varied
isometrically, rather than allometrically, with body size
in primate taxa with frugivorous, folivorous, and insec-
tivorous diets, respectively. The implication is that posi-
tive allometry amongst the larger and smaller australo-
piths probably does denote different foods (Kay, 1975b),
as Robinson had originally proposed.
Reasonable estimates for body weights of the three
\gracile"australopiths—A. anamensis,A. afarensis, and
A. africanus—have allowed an assessment of the scaling
of incisors against body size (Kay, 1975b, 1985; Ungar
and Grine, 1991; Teaford and Ungar, 2000). Their rela-
tive sizes are very similar, and they fall close to the
regression line for a number of primates. These results
suggest that the gracile australopiths tended to eat foods
that required moderate amounts of incisal preparation
(Teaford and Ungar, 2000).
One of the distinguishing features of the australopiths
is their large and relatively flat molars (Robinson, 1956;
Wolpoff, 1973; Wood and Abbott, 1983; Kay, 1985; Tea-
ford et al., 2002). \Megadontia quotients"(relative size
of molars scaled against body size) for australopiths
increased over time from A. anamensis to Paranthropus,
suggesting changes in the physical properties of their
foods (e.g., hardness, size, and shape) to those that
required a good deal of force (Demes and Creel, 1988).
Another approach is to compare molar tooth areas of the
M1 and M3, since this ratio is inversely correlated with
percentage of leaves, flowers, and shoots in the diets of
modern primates (Lucas and Peters, 2000; Teaford et al.,
2002). The earlier australopiths, including Ardipithecus,
have clearly higher M1:M3 ratios than Paranthropus,
suggesting perhaps lower consumption of leaves, flowers,
and shoots, and conversely greater degrees of frugivory
(Teaford and Ungar, 2000).
132 J. LEE-THORP AND M. SPONHEIMER
American Journal of Physical Anthropology—DOI 10.1002/ajpa
Tooth size alone is insufficient to address questions
about changing amounts of fruit (or other foods) in the
diets of early hominins, shape must also be considered
(Wood, 1981). Changes in tooth morphology tend to
reflect changes in properties of typical foods, such as
their toughness (Ungar, 1998). Food is orally prepared
by the shearing, crushing, and grinding actions of teeth,
and these functions have different morphological corre-
lates (Strait, 1997; Lucas and Peters, 2000). Shearing
requires blades or crests, while crushing and grinding
require occlusion of two relatively flat or smooth surfaces
in opposition. Hence, the relative importance of these
actions, which are related to the properties of typical
foods, should be reflected in tooth morphology, or rather,
in the capabilities of tooth forms to accomplish these
actions (Strait, 1997). Hard and brittle foods, for exam-
ple, require crushing between flat planar surfaces
whereas tough, pliant foods require shearing by recipro-
cally concave, highly crested teeth. The shearing poten-
tial of molar teeth can be assessed by means of a
\shearing quotient"based on observations that extant
folivorous primates exhibit higher shearing quotients
than brittle or soft fruit feeders, which are higher in
turn than hard-object feeders (Kay, 1985). In general,
australopiths had relatively flat, blunt molars and lacked
prominent shearing crests (Grine, 1981; Kay, 1985; Tea-
ford et al., 2002), suggesting that they were more capa-
ble of processing soft or brittle, rather than tough, pliant
foods. Following this reasoning, it has also been sug-
gested that the early australopiths may have lacked the
capabilities for orally processing meat, while early Homo,
which had relatively greater occlusal relief, might have
had greater success processing tough, elastic foods such as
meat (Lucas and Peters, 2000; Ungar, 2004). Nonetheless,
variability undoubtedly exists within the australopiths, as
A. africanus and A. afarensis have greater occlusal relief
compared to P. robustus, again suggesting dietary differ-
ences between these species (Teaford et al., 2002).
In spite of this improved understanding of the func-
tional drivers for dental morphology and allometry, the
functional relationships between form and diet remain
unclear (Grine et al., 2006). Moreover, ultimately these
approaches imply dental capabilities rather than evi-
dence of diet per se. Indeed, morphology is an ambiguous
dietary predictor and studies have in many cases yielded
conflicting results. It has been suggested, for instance,
that A. africanus was anything from primarily herbivo-
rous, omnivorous, to faunivorous on the basis of tooth
morphology (Robinson, 1954; Jolly, 1970; Wolpoff, 1973;
Szalay, 1975; Kay, 1985). The central problem is that
dental morphology reflects both phylogenetic history and
dietary adaptations. Dental adaptations reflect dietary
drivers over geological or evolutionary timescales and
they are not necessarily concordant with the actual
behavior of any given individual. For instance, the rela-
tively large incisors and bunodont molars of modern
Papio baboons suggest a frugivorous diet (Hylander,
1975; Ungar, 1998; Fleagle, 1999), and yet many Papio
populations consume large quantities of grass (Altmann
and Altmann, 1970; Dunbar, 1983; Strum, 1987) for
which they have no apparent dental capabilities. Fur-
thermore, dietary behavior can be altered over time and
space, and the facility for change is particularly evident
in taxa which are dietary generalists. Pointing to these
problems, Ungar (2004) proposed that dental morphology
may be a better predictor of fallback dietary behavior or
dietary limitations than of more typical trophic behavior.
PROCESSING DAMAGE AND MICROWEAR
Wear-related techniques can address some of these limi-
tations. The results of gross wear pattern studies, how-
ever, have been inconclusive, resulting in opposing conclu-
sions about the variability and distinctiveness between
the South African australopiths, for instance (Robinson,
1956; Wallace, 1973, 1975; Wolpoff, 1973). Antemortem
chipping occurred in both taxa (Wallace, 1973, 1975) but
the dietary implications were never satisfactorily re-
solved. Amongst Neanderthals, rounded labial wear of
incisors coupled with frequent damage in the form of chip-
ping, microfractures, and striations is thought to be asso-
ciated with use of the anterior dentition as a tool rather
than with dietary wear (e.g. Klein, 1999).
Dietary microwear patterning, by contrast, has received
a great deal of attention over the last two decades. Oral
processing of food leaves microscopic damage on tooth
enamel surfaces, which is ultimately related to the me-
chanical properties of foods and to the presence of exoge-
nous grit. Thus, unlike dental allometry and morphology
which reveal something about the foods that challenge an
individual’s ancestors, dental microwear reflects its actual
experience. In fact, the immediacy is such that it reflects
food processing over the previous few days to weeks at the
most, as microwear is quickly obliterated (Teaford and
Oyen, 1989a). In short, dental microwear can distinguish
among dietary categories when they correspond to differ-
ences in physical characteristics of foods (El Zataari et al.,
2005), and when the influence of taphonomic factors is
excluded (Teaford, 1988b).
A particular advantage is that microwear patterns may
be able to detect subtle dietary differences amongst
related primate species under certain circumstances (e.g.,
Walker, 1976; Teaford, 1985, 1988a; Teaford et al., 2002).
Most studies have concentrated on patterns of small pits
and scratches resulting from chewing and crushing, and
both extant and extinct primates have been extensively
studied. For instance, primates that make frequent use of
their front teeth tend to have high densities of microwear
striations on their incisors (Ryan, 1981; Ungar and Grine,
1991). Folivores show high incidences of long narrow
scratches on their molar occlusal surfaces, whereas frugi-
vores have relatively more pits. Among frugivores, hard-
object feeders have higher pit incidences than soft-fruit
eaters. Hence, hard fruit- and seed-eaters, such as manga-
beys (Lophocebus albigena and Cebus apella), show dis-
tinct microwear patterns compared to leaf-eaters, like
mountain gorillas (Gorilla gorilla beringei) (Grine and
Kay, 1988; Ungar, 1998). These and other relationships
between microwear and feeding behaviors in living pri-
mates have been used to infer diet in fossil forms.
Observer differences and low repeatability have been
major disadvantages in microwear studies (Teaford and
Oyen, 1989b; Grine et al., 2002), and an area of active
and ongoing development is to quantify patterns of mi-
croscopic pitting and scratching damage in as objective
and repeatable a manner as possible (e.g., Ungar, 2004;
Scott et al., 2005). Micrographs of small sections of tooth
facets are obtained using scanning electron microscopy
of high-precision molds, at high magnification (5003). A
major advance was the combination of scanning confocal
microscopy methods (Boyde and Fortelius, 1991) with
fractal analysis to analyze tooth topography (Ungar
et al., 2003). Current techniques use automated image
processing of scanned micrographs using a software
package (Ungar, 1995; El Zataari et al., 2005) to quantify
133BIOGEOCHEMISTRY AND HOMININ DIETS
American Journal of Physical Anthropology—DOI 10.1002/ajpa
the variables—percentage of pits, scratch breadth, pit
breadth, and pit length. Scale-sensitive fractal analysis
has been recently applied to a hominin study to better
characterize the complexity and anisotropy of three-
dimensional microwear damage (Scott et al., 2005).
Microwear analyses have been frequently applied to
diets of fossil primates, including Miocene Dryopithe-
cines (Ungar, 1996), and applications to early hominin
diets are ongoing. An early application to the South Afri-
can australopiths provided an independent test of Robin-
son’s hypothesis for dietary distinctions between the
South African robust and gracile australopiths (Rob-
inson, 1954, 1956). Grine (1981, 1986), and Grine and
Kay (1988) demonstrated that Paranthropus molars
showed more pitting than those of A. africanus, while
the scratches in the latter are longer, narrower and
more directed (or anisotropic) (Fig. 1a). These authors
deduced that while Paranthropus concentrated on small,
hard objects, A. africanus ate softer foods more fre-
quently, such as fruits and leaves. Microwear features
on A. africanus incisors show higher densities on all sur-
faces compared to Paranthropus (Ungar and Grine,
1991), suggesting that the former processed more foods
with the anterior teeth. The results are consistent with
craniodental measurements which suggest that they
used a great deal of force to process hard foods (e.g.,
Demes and Creel, 1988). Subsequent assessments of
molar microwear using automated confocal 3D image mi-
croscopy and fractal image analysis have been largely
consistent with the earlier studies, although they have
tended to emphasize also inter-individual dietary vari-
ability and overlap between these two species (Fig. 1b)
(Scott et al., 2005).
Most recently, Grine et al. (2006) showed that the
molar microwear on the enamel of A. afarensis was most
similar to that of gorillas and dissimilar to hard object
feeders (Fig. 2), suggesting an unexpected reliance on
terrestrial herbaceous vegetation rather than small hard
objects, as suggested by their dental morphology and
thick enamel. They also noted that Australopithecus
microwear patterns did not change with shifting envi-
ronments over a period of some 400 Ka. An earlier quali-
tative microwear study on the anterior teeth of A. afar-
ensis (Puech et al., 1983) had also suggested that a
mosaic of gorilla-like fine wear striae and baboon-like
pits and microflakes implied use of incisors to strip
gritty plant parts, such as seeds, roots, and rhizomes
(Ryan and Johansen, 1989). Other than this, little micro-
wear data is available for the earlier australopiths, and
none for A. anamensis and Ardipithecus ramidus,
although a report on the microwear of the former species
is forthcoming (P. Ungar, personal communication).
There has also been little emphasis on dental micro-
wear in later hominins. This is partly a result of the
unknown influence of cultural factors in processing of
Fig. 1. Occlusal molar microwear differences and similarities between A. africanus (filled circles) and Paranthropus (open
circles). (a) A bivariate plot of microwear feature width versus feature length (in lm) on M
2
protoconal facets using scanning elec-
tron microscopy shows that the former has more scratches and the latter more pit features (data from Grine, 1986: Table 9). (b)A
bivariate plot of anisotropy (epLsar
1.8
) and complexity [log
10
(Asfc)], calculated from fractal analysis of occlusal molar topography,
suggests that Paranthropus features show less anisotropy (i.e. less directionally dependent microwear) and greater complexity, but
also that there is some overlap between patterns of the two taxa (redrawn from Scott et al., 2005).
Fig. 2. A comparison of the two most distinguishing micro-
wear features (scratch width and % pitting) for Australopithecus
afarensis (or Praeanthropus afarensis) against similar data for a
range of extant primates shows greatest similarity with Gorilla
gorilla and not with hard object feeders (Cebus apella and Lopho-
cebus albigena) as might have been predicted from morphology
and enamel thickness (data from Grine et al., 2006: Table 7).
134 J. LEE-THORP AND M. SPONHEIMER
American Journal of Physical Anthropology—DOI 10.1002/ajpa
foods, as well as the lack of appropriate comparisons.
Primate comparisons are a central pillar of microwear
(and morphological) applications to hominin diets, but
they are less relevant to more recent populations, and
comparative studies are relatively rare. One exception is
the study of Pe
´rez-Pe
´rez et al. (2003) which suggested
that the microwear feature density, length, and orienta-
tion on Middle Pleistocene hominin molar buccal sur-
faces were consistent with more abrasive diets than
those of Late Pleistocene individuals. They suggested
that microwear density appeared to increase during cold
intervals and argued that this resulted from hominins
eating more abrasive plant foods, such as roots and
bulbs. A corollary is that Neanderthals ate more nonab-
rasive foods during warmer periods, and the authors
argue that the most likely item was animal meat. This is
a somewhat counter-intuititive outcome when one con-
siders that animal foods were likely to be the most acces-
sible items under glacial conditions. A forthcoming study
on molar microwear of Neanderthals should resolve this
argument (S. El-Zataari, personal communication).
CHEMICAL DIETARY TOOLS
The underlying rationale of these techniques is that
the chemical composition of a mammal’s tissues, includ-
ing bones and teeth, reflects that of its diet, following
the old adage, \you are what you eat". Thus, they can
provide direct chemical means for investigating paleo-
diets. This is the case as long as several crucial condi-
tions are met. One is that various food sources can be
distinguished by means of isotopic or chemical composi-
tion differences, which is not always the case. The path-
ways of these natural abundance tracers into tissues
must also be predictable and understood. Finally, the
original chemical composition, or at least something
close to it, must survive. Thus, the over-arching con-
straints for applying these tracers are related to our
understanding of the pathways of essential elements and
isotopes in ecosystems, and to preservation issues. Stud-
ies of isotope and trace elemental behavior in modern
ecosystems are large-scale, ongoing, undertakings (e.g.,
Burton et al., 1999; Codron et al., 2005; Sponheimer
et al., 2005b). Efforts to address problems of preserva-
tion have included a shift to tooth enamel as sample ma-
terial where it is feasible and the development of reliable
protocols for identifying purity and assessing whether
the dietary signals are real or not.
Chemistry was first used to address questions related
to diet in the more recent archeological past to detect
use of maize (e.g., Vogel and van der Merwe, 1977; van
der Merwe and Vogel, 1978), pastoralism (Ambrose,
1986), marine food use (Tauber, 1981), and trophic levels
and dietary change (Schoeninger, 1979; Sillen, 1981).
Subsequently, a good deal of effort has been devoted to
pushing these tools further back in time. Over the last
decade or so, several studies have emerged that have
provided new insights into dietary behavior of early and
later hominins. The earlier pioneering stable isotope
work concentrated exclusively on bone collagen, with the
first applications to early hominin diets, based on tooth
enamel, appearing later (Lee-Thorp, 1989; Lee-Thorp
et al., 1994). Stable isotopic studies of the diets of Late
Pleistocene hominins—Neanderthals and modern
humans—have so far relied on the conventional bone col-
lagen-based methods. Similarly, trace element studies
focused for some time on bone, and only recently have
applications explored tooth enamel as sample material.
The discussion below briefly outlines the principles of
stable light isotope and trace element pathways in eco-
systems and follows first the work on Neanderthals
using bone collagen, and next the isotope and trace ele-
ment work on earlier hominins based on analyses of
enamel and bone mineral. The emphasis on European
Neanderthals and South African australopiths is a
reflection of the limited degree to which stable isotopes
and trace elements have been used to investigate the
diets of Plio–Pleistocene hominins.
Stable light isotopes in ecosystems
A simplified, diagrammatic illustration of the stable
isotope pathways described in the following paragraphs
is shown in Figure 3.
During photosynthesis plants take in CO
2
and convert
it to sugars. This process discriminates strongly against
13
CO
2
but to different degrees depending on the pathway
(Smith and Epstein, 1971) and on environmental condi-
tions to a smaller extent. Plants following the C
3
pathway
(all trees, shrubs and herbs, and temperate or shade-
adapted grasses) are strongly depleted in
13
C relative to
atmospheric CO
2
, and consequently have distinctly lower
d
13
C
1
values compared to C
4
plants (mainly tropical
grasses). Environmental influences acting on C
3
plants
include the \canopy effect"in dense forests (leading to fur-
ther depletion in
13
C) (Vogel, 1978; van der Merwe and
Medina, 1989) and aridity/temperature effects (leading to
1
By convention, stable isotope ratios are expressed as dvalues rel-
ative to an international standard in parts per thousand (per mil),
as follows in an example for carbon isotopes: d
13
C(%)¼(R
sample
/
R
standard
–1)31,000 where R¼
13
C/
12
C and the international
standard is Vienna Peedee Belemnite (VPDB).
Standards for nitrogen (
15
N/
14
N) and oxygen (
18
O/
16
O) isotopes
are atmospheric nitrogen (AIR), and VPBD or Standard Mean
Ocean Water (SMOW), respectively.
Fig. 3. Schematic representation showing the patterning of
stable carbon (d
13
C) and nitrogen (d
15
N) isotopes in typical food-
webs. Global mean d
13
C values are given for trophic steps in
the carbon cycle (middle panel), while mean differences are
given for steps in the nitrogen cycle (right panel). This is
because soil d
15
N values depend on the balance of nitrogen fixa-
tion and denitrification, which is affected by a host of environ-
mental factors. Two tissues (collagen and apatite) are shown for
herbivores and carnivores.
135BIOGEOCHEMISTRY AND HOMININ DIETS
American Journal of Physical Anthropology—DOI 10.1002/ajpa
enrichment in
13
C under more arid and/or warm condi-
tions and vice versa) (for a review see Tieszen, 1991). A
third photosynthetic pathway, the Crassulacean Acid Me-
tabolism (CAM) pathway, effectively utilizes both path-
ways with resulting d
13
C values that vary extensively
depending on whether they are \obligate"CAM or not and
upon environmental conditions (Winter and Smith, 1996).
CAM plants are primarily succulents like euphorbias that
are rare outside of desert environments, and are moreover
rarely used by animals (but see Codron et al., 2006 for use
by baboons). They are not considered as important compo-
nents of the environments inhabited by Plio–Pleistocene
hominins (Reed, 1997; Peters and Vogel, 2005).
Nitrogen enters the terrestrial foodweb via N
2
-fixing
bacteria in soils or plants to form nitrates or ammonium
ions which are utilized by plants. The net effect of bio-
logical nitrogen fixing and subsequent denitrification
during decay of organic matter is slight enrichment in
15
N in plants and soils compared to atmospheric N
2
but
the balance is affected by environmental conditions such
as aridity (Heaton, 1987; Sealy et al., 1987; Handley and
Raven, 1992; Amundson et al., 2003), although other
effects such as leaching (high precipitation) and anoxia
can also contribute.
Isotopic variability in plants is reflected in the bones
and teeth of animals that consume them. Here under-
standing of the bio- and physico-chemical routes from food
to tissue fixation is required, since diet-tissue fractiona-
tion varies according to the tissue and its chemistry. Iso-
tope ratios of carbon (
13
C/
12
C) and nitrogen (
15
N/
14
N) can
be studied in collagen, which is the main organic compo-
nent of bone and dentine. The mineral phase of bone and
enamel, crystalline calcium phosphate structures known
as biological apatites, yield
13
C/
12
C and
18
O/
16
O ratios
from carbonate ions or
18
O/
16
O alone from phosphate ions.
Both the structural and the isotope chemistry between
diet and the organic or inorganic (mineral) compartments
of skeletal tissues differ. Further, the timespan of dietary
behavior reflected differs depending on whether bone or
tooth tissues are analyzed; bone isotope values tend to
reflect long-term averages (at least 10 years or more)
whereas tooth isotope values reflect dietary behavior at
the time of deposition since both enamel and dentine are
incremental tissues. Where skeletal tissues are preserved
at all, enamel in particular survives remarkably well for
millions of years, apparently with only subtle alteration.
Collagen has a much shorter \shelf-life"since it denatures
and dissolves away far more quickly than the mineral,
where the latter is preserved. On the other hand, where it
does survive, it is relatively straightforward to obtain
demonstrably intact collagen for analysis. A number of
safeguards are routinely employed to demonstrate the
quality of the collagen (Ambrose, 1990). Hence, the sample
tissue chosen is important because this choice (often
imposed by circumstances) directly affects the isotope
tools and the type of information available, the age limits
for the study, and the measures that must be taken to
guard against diagenesis.
Stable isotopes in bone collagen
The difference (D) between diet and collagen d
13
Cis
about +5%, but controlled feeding studies have shown
that the relationship is largely between dietary protein
and collagen because dietary amino acids are preferen-
tially utilized for collagen tissue construction, while car-
bon from dietary carbohydrate and lipids makes a lesser
contribution (Ambrose and Norr, 1993; Tieszen and
Fagre, 1993). A stepwise trophic shift of +3–5%in d
15
N
from plants to herbivores, and from herbivores to carni-
vores has been widely documented in marine and terres-
trial foodwebs (Minigawa and Wada, 1984; Schoeninger
and DeNiro, 1984; Sealy et al., 1987). A significant out-
come of the routing of dietary protein to tissue proteins
is that d
13
C in bone collagen (and d
15
N by default) is \bi-
ased"towards the high protein component of an individ-
ual’s diet. Consequently, animal foods will be overrepre-
sented in bone collagen at the expense of low-protein
(vegetable) foods, and this bias must be considered when
interpreting collagen stable isotope data.
Progress in extracting good quality collagen from older
material has demonstrated that under the right condi-
tions, bone collagen can survive for up to 200,000 years
(Ambrose, 1998; Jones et al., 2001). This has made it
possible analyze the bone collagen of Late Pleistocene
hominins in certain cases. At these time depths, strict
quality controls that demonstrate collagen preservation
are essential because degradation is known to alter colla-
gen stable isotope ratios significantly (Ambrose, 1990).
Neanderthal diets. Bocherens et al. (1991) performed
the first stable isotope analysis of a single Neanderthal
individual and associated fauna from 40,000-year-old
bones at the site of Marillac in France. Although the
quality control methods relied on amino acid profiles
that might not be considered adequate today, subsequent
analyses from this site (Fizet et al., 1995) have shown
the original observations to be robust. The study paved
the way for subsequent analyses of Neanderthals from
Marillac (Fizet et al., 1995), Scladina Cave, Awirs Cave,
and Betche-al-Roche Cave in Belgium (Bocherens et al.,
1997, 2001), and Vindija Cave in Croatia (Richards
et al., 2000).
All native European plants are C
3
, and consequently
have similar d
13
C values with the exception of plants in
densely wooded environments that are more depleted in
13
C due to the canopy effect (Vogel, 1978; van der Merwe
and Medina, 1989). Thus, d
13
C composition of bone colla-
gen reveals little about the diets of Neanderthals, except
that they likely utilized few food resources from closed,
densely forested environments (Bocherens et al., 1999;
Richards et al., 2000). The d
15
N composition of Neander-
thal bone collagen is more revealing. Although nitrogen
isotope distributions in foodwebs are often complicated
due to heterogeneity in plant d
15
N and the disparate
physiological adaptations and requirements of different
animals (Ambrose, 1991; Sponheimer et al., 2003), the
general pattern of stepwise shifts in d
15
N of about +3–
4%is robust (Fig. 3). Thus, d
15
N analysis of Neanderthal
bone collagen can address the question of trophic level
and hence of meat consumption. This is particularly rele-
vant as the degree of carnivory and manner of carcass
acquisition (hunting or scavenging) amongst Neander-
thals has been the subject of debate (e.g., Binford, 1981;
Stiner, 1994; Marean and Assefa, 1999; Speth and Tcher-
nov, 2001).
All published isotopic studies have shown that Nean-
derthals have much higher d
15
N than that of contempo-
raneous (or near-contemporary) herbivores such as horse
(Equus caballus), reindeer (Rangifer tarandus), and bi-
son (Bison priscus) and similar to that of carnivorous
wolves (Canis lupus), hyenas (Crocuta spelaea), and
lions (Panthera spelaea) (Bocherens et al., 1991, 1997,
2001, 2005; Fizet et al., 1; Richards et al., 2000). Overall,
136 J. LEE-THORP AND M. SPONHEIMER
American Journal of Physical Anthropology—DOI 10.1002/ajpa
Neanderthal d
15
N is not only significantly higher than
herbivore d
15
N, but also slightly higher than carnivores
(Fig. 4) (Sponheimer and Lee-Thorp, 2006b). Even given
the bias towards animal foods in bone collagen, these
data suggest that Neanderthals were significantly car-
nivorous, and that little of their dietary protein came
from plant foods (Richards et al., 2000, 2001; Bocherens
et al., 2005). These authors have argued that enrichment
in
15
N compared to (other) carnivores could be taken as
an indication of dependence on herbivores with relatively
high d
15
N, such as mammoths (Mammuthus primige-
nius), or even the consumption of omnivorous bears
(Ursus spp.)(Richards et al., 2000; Bocherens et al.,
2001). Bocherens et al. (2005) used a mixing/resource
partitioning model developed in modern ecosystem stud-
ies (Phillips, 2001; Phillips and Gregg, 2003) to calculate
on the basis of statistical probability that a major compo-
nent of Neanderthal diet was mammoth. However, a
number of problems underlie the use of this statistical
model, not the least of which is that values for all
resources must be known.
It has not yet been possible to compare directly the
stable isotope composition of Neanderthals and Upper
Paleolithic Homo sapiens (UPHs) from similar periods
and places. However Richards et al. (2001) were able to
compare data from nine near-contemporaries from the
mid-Upper Paleolithic (*28–20 Ka) at Brno-Francouz-
ska and Dolni Vestonice (Czech Republic), Kostenki,
Mal’ta, and Sunghir (Russia), and Paviland (Great Brit-
ain) with data from the five Neanderthals that had been
published at the time. They observed that the modern
humans were even more elevated in d
15
N, suggesting, if
one follows the same arguments applied to Neander-
thals, that these modern humans were also highly de-
pendent on animal foods. In this case, however, they sug-
gested contributions from freshwater aquatic resources
such as fish and waterfowl, which can be more enriched
in
15
N than terrestrial resources (Dufour et al., 1999)
and that this implied diversification of the resource base
(Richards et al., 2001). This suggestion was unexpected,
as there is little archeological evidence for exploitation of
such foods at this time. With the subsequent addition of
several new Neanderthal and mid-Upper Paleolithic
human analyses (Bocherens et al., 2001; Pettitt et al.,
2003); however, there is no longer any statistically sig-
nificant difference in the d
15
N of Upper Paleolithic
humans and Neanderthals (Sponheimer and Lee-Thorp,
2006b) (Fig. 4).
Interpretation of these data is not straightforward and
there remain a number of unanswered questions. For
instance, why are both hominins so enriched in
15
N com-
pared to associated carnivores? The consumption of her-
bivores with unusually high d
15
N such as mammoths, or
aquatic resources, offers one possible, but nevertheless
rather unsatisfactory explanation. There may be an al-
ternative physiological explanation for their extremely
high d
15
N values. Controlled feeding studies have shown
that when herbivores are fed diets with protein contents
much greater than their nutritional requirements, their
diet-tissue spacing (D, denoting the isotopic difference
between dietary and tissue values) exceeds the average
of +3–4%(Sponheimer et al., 2003). Hence, if the con-
sumption of animal-rich high-protein diets in the pre-
vailing glacial environment led to Neanderthals’ exceed-
ing their protein requirements, their Dmight well
exceed +3–4%and increase their d
15
N compared to other
taxa. The anomalously high d
15
N of mammoths and low
d
15
N of cave bears (Bocherens et al., 1997; Ambrose,
1998) also hints at the importance of unknown physio-
logical adaptations in determining an organism’s nitro-
gen isotope composition. These studies of glacial-age
Neanderthals and modern humans in Europe illustrate
the complexity in interpreting d
15
N data in a paleo-eco-
system for which we have incomplete information and no
modern analogue.
It is worth noting that even if the Neanderthals did
have an unusually increased diet-tissue spacing due to a
high-protein intake, it might erase their distinctiveness
from other carnivores but would certainly not make
them look herbivorous. The d
15
N data leave little doubt
that Neanderthals and mid-upper Pleistocene modern
humans consumed large quantities of animal foods.
Stable isotopes in enamel apatite
Bone collagen is rarely preserved beyond the Late
Pleistocene (Jones et al., 2001), so this avenue is not an
option for analysis of older hominin material. However,
the carbon isotopes in the mineral component can also
be used as dietary proxies (Sullivan and Krueger, 1981;
Lee-Thorp and van der Merwe, 1987). Although bone
mineral clearly persists beyond bone collagen, it is inevi-
tably altered postmortem, often (but not always) result-
ing in the loss of the biogenic dietary signal (Lee-Thorp,
2000; Lee-Thorp and Sponheimer, 2003). This is due to
bone’s high organic content, porosity, and small crystal
size (LeGeros, 1991; Elliot, 1994), which make it suscep-
tible to dissolution/reprecipitation phenomena that facili-
tate the incorporation of exogenous carbonate ions. Thus
paleodietary studies based on bioapatite were forestalled
until it could be shown that dental enamel from ancient
fauna with well-understood diets reliably retained bio-
genic isotope compositions. This was accomplished by
demonstrating that known fossil grazers had d
13
C values
indicative of C
4
-grass diets, while known fossil browsers
Fig. 4. Neanderthal bone collagen d
15
N data from the sites
of Marilac, Scladina, Vindija, Engis, and Spy shown in relation
to herbivores and carnivores from the same sites (combined),
and compared against data for mid-Upper Paleolithic humans
(labeled H. sapiens for brevity). Mean values are shown as
boxes along with standard deviations and the number of indi-
viduals in each case. Neanderthal data are summarized from
Bocherens et al. (1991, 1999, 2001), Fizet et al. (1995), and
Richards et al., (2000), while the Upper Paleolithic human data
is from Richards et al. (2001) and Pettitt et al. (2003).
137BIOGEOCHEMISTRY AND HOMININ DIETS
American Journal of Physical Anthropology—DOI 10.1002/ajpa
had d
13
C values indicative of browsing diets (Lee-Thorp
and van der Merwe, 1987). Numerous empirical and the-
oretical studies have substantiated this finding (e.g.,
Cerling et al., 1997; Sponheimer and Lee-Thorp, 1999b;
Zazzo et al., 2000), which is hardly surprising given that
enamel is denser, has a very low organic content and is
more crystalline (LeGeros, 1991; Elliott, 1994) which
renders it effectively more inert and \pre-fossilized."
Therefore, only tooth enamel has been used for stable
isotope analysis of hominin and non-hominin specimens
that are millions of years old. Although at first relatively
large samples (*200 mg) were needed, rendering this a
destructive method of analysis, subsequent advances in
mass spectrometry have reduced the required sample to
a few milligrams (Lee-Thorp et al., 1997; Sponheimer,
1999). As a result, it has become possible to remove
small samples with minimal, barely observable damage,
and consequently larger numbers of analyses became
possible. It is worth noting that different pretreatment
protocols designed to eliminate contamination (Koch
et al., 1997; Lee-Thorp et al., 1997; Sponheimer, 1999)
can lead to small but significant differences in a sample’s
stable isotope composition (especially for oxygen), and
therefore one must compare stable isotope values for
teeth analyzed following different protocols with caution.
Apatite carbonate forms from blood bicarbonate, and
isotopic fractionation is tightly controlled by physico-
chemical processes during apatite formation. The rela-
tionship between dietary, breath CO
2
(which is equili-
brated with blood bicarbonate), and enamel apatite d
13
C
has been well-studied (Passey et al., 2005). Overall, the
diet to enamel shift averages about 13%for most large
mammals (Fig. 3) (Lee-Thorp et al., 1989; Passey et al.,
2005). Nevertheless, some variability has been docu-
mented, for instance measurements on small rodents on
controlled diets indicate a diet-apatite spacing of just
less than 10%(Ambrose and Norr, 1993; Tieszen and
Fagre, 1993), while studies of some large ruminants
indicate values of up to +14%(Cerling and Harris,
1999). This variation likely reflects mass balance differ-
ences related to metabolism and/or dietary physiology.
Unlike collagen, apatite reflects the d
13
C of the bulk
diet, and not just the protein component (Krueger and
Sullivan, 1984; Lee-Thorp et al., 1989; Ambrose and
Norr, 1993; Tieszen and Fagre, 1993). Thus, apatite and
bone collagen d
13
C provide different perspectives on an
individual’s diet, and indeed analysis of both components
would provide the most complete picture. Most impor-
tant, for our purposes, is that enamel apatite provides a
good average dietary signal that equally reflects the con-
sumption of vegetable and animal foods.
Australopith and early Homo diets. Isotopic dietary
studies of early hominins are founded primarily upon
the distinct d
13
C composition of C
3
and C
4
plants, which
in African savanna environments reflect carbon sources
from trees, bushes, shrubs, and forbs for the former, and
tropical grasses and some sedges for the latter. In the
early 1990s, it was widely believed that A. africanus had
a diet that consisted primarily of fleshy fruits and
leaves, much like the modern chimpanzee, while
P. robustus consumed more small, hard foods such as
nuts (Grine, 1981; Grine and Kay, 1988; Ungar and
Grine, 1991). As these are all C
3
foods, it could then be
predicted that A. africanus and P. robustus should have
d
13
C values indistinguishable from those of C
3
browsers
and frugivores.
This turned out not to be the case. A total of 40 cer-
tain hominin specimens from the sites Makapansgat,
Sterkfontein, Kromdraai, and Swartkrans have now
been analyzed. The data demonstrate unequivocally that
the d
13
C of both australopiths is very distinct from that
of C
3
-consuming coevals (P<0.0001), but that A. africa-
nus and P. robustus cannot be distinguished from each
other (Sponheimer and Lee-Thorp, 1999a; Lee-Thorp
et al., 1994, 2000; van der Merwe et al., 2003; Spon-
heimer et al., 2005b) (Fig. 5). The distinction between
the hominins and other fauna cannot be ascribed to dia-
genesis, as there is no evidence that browser or grazer
d
13
C has been altered, and diagenesis should affect all
fauna alike. If we take the mean d
13
CofC
4
and C
3
con-
suming herbivores as indicative of pure C
4
and C
3
diets
respectively, it would indicate that both Australopithecus
and Paranthropus obtained about 30% or more of their
carbon from C
4
sources. Thus, both taxa were eating
considerable quantities of C
4
resources, and these
resources must have consisted of grasses, sedges, or ani-
mals that ate these plants.
Fig. 5. Enamel d
13
C data for Australopithecus africanus,
Paranthropus robustus, and Homo specimens from the sites of
Makapansgat, Sterkfontein, and Swartkrans compared with C
3
plant consumers (browsers) and C
4
plant consumers (grazers);
all data are shown as means (boxes), standard deviations, and
numbers (n) of individuals except for the three Swartkrans
Homo values which are shown as stars. Data are from Lee-
Thorp et al. (1994, 2000) for Swartkrans, Sponheimer, and Lee-
Thorp (1999a) for Makapansgat, van der Merwe et al. (2003) for
Sterkfontein, and Sponheimer et al. (2005a) for the remaining
Sterkfontein data.
138 J. LEE-THORP AND M. SPONHEIMER
American Journal of Physical Anthropology—DOI 10.1002/ajpa
This result was unexpected, since extant apes consume
minimal C
4
resources if at all (McGrew et al., 1981, 1982;
Goodall, 1986). Even in more open environments where
C
4
foods are readily available, d
13
C analyses of chimpan-
zees do not indicate any C
4
consumption (Schoeninger
et al., 1999; Carter, 2001; Sponheimer et al., 2006). Thus,
the d
13
C data suggests a fundamental niche difference
between the australopiths and extant apes. Furthermore,
this association with C
4
resources persists through dia-
chronic environmental trends from relatively closed habi-
tats in the Pliocene at the sites of Makapansgat (*3 Ma)
and Sterkfontein Member 4 (*2.5 Ma) through to the
later, open environments of Swartkrans Member 1 (*1.5–
1.8 Ma) (Fig. 5). The hominin d
13
C data are also more vari-
able than virtually all modern and fossil taxa that have
been analyzed in South Africa (Lee-Thorp et al., 1994,
2000; Sponheimer and Lee-Thorp, 1999a, 2001, 2003;
Codron, 2003; van der Merwe et al., 2003). This suggests
that australopiths were opportunistic primates with wide
habitat tolerances, an observation which is consistent
with Wood and Strait’s (2004) suggestion that these early
hominins were eurytopic (dietary generalists) rather than
ecological specialists.
How do these data compare with early Homo? Based
on the prediction that if Homo consumed more animal
foods (as is widely held), their d
13
C should be more posi-
tive compared to P. robustus from the same Swartkrans
Member 1 deposits, data from three early Homo speci-
mens were compared with the australopith data (Lee-
Thorp et al., 2000). Again this turned out not to be the
case; Homo d
13
C was very similar to that of the australo-
piths (Fig. 5), and the results must be interpreted in the
same way. Roughly 25% of their dietary carbon came
from C
4
sources that included C
4
plants, C
4
animal prod-
ucts, or some combination of these. However, only three
Homo specimens from one site have been analyzed and
published so far, and thus comparisons with the more
numerous australopith data must be viewed with cau-
tion. Unpublished d
13
C data from East Africa show a
strong difference between Paranthropus and Homo;in
this case the former is strongly enriched in
13
C, while
values for the latter resemble those for the Swartkrans
individuals (van der Merwe, personal communciation).
This leaves us with the question about what exactly
these C
4
resources were? The answer to this question is
significant, because the outcome has a variety of physio-
logical, social, and behavioral implications. For instance,
if australopiths had a grass-based (graminivorous) diet
similar to the modern gelada baboon (Theropithecus
gelada), it would suggest that their diets were less nutri-
ent rich than those of modern apes, placing limitations on
brain expansion and sociality (Aiello and Wheeler, 1995;
Milton, 1999). The converse that australopiths ate diets
rich in animal foods would indicate a leap in dietary qual-
ity over modern apes (Milton, 1999). At the time Lee-
Thorp et al. (1994, 2000) argued that savanna grasses are
unlikely staple food sources for hominins and that con-
sumption of C
4
-consuming insects and vertebrates was a
more plausible explanation. This argument was based
partly on the lack of dental and digestive \equipment"to
deal with grasses per se, and partly on the limited sea-
sonal availability and difficulties of harvesting grass
seeds, which are denser, if tiny, food packages.
This list of possibilities has been reconsidered (e.g.,
Peters and Vogel, 2005; Sponheimer and Lee-Thorp,
2006b). Recently edible sedges have received attention as
potential C
4
foods for hominins (Conklin-Brittain et al.,
2002), argued to have been part of a strategy focused on
wetlands. Sedges are common in these habitats and in
some cases can represent reasonably high quality foods,
for which there was likely little competition (Conklin-
Brittain et al., 2002). However, the distribution of C
4
sedges has different climate or environmental controls
compared to C
4
grasses (Stock et al., 2004), and it cannot
be assumed that most sedges utilize the C
4
pathway even
in African savannas. Only 35% of sedges in South Africa
overall are C
4
(Stock et al., 2004), and a study of sedges
in riverine habitats similar to those inhabited by austral-
opiths found <30% abundance (Sponheimer et al., 2005a),
with very few being edible. Unless the distribution of
sedges was markedly different during the Pliocene, and/
or the australopiths sought out large quantities of C
4
sedges, sedge consumption could not produce the
observed 35–40% C
4
contribution to hominin diets. Thus,
a sedge specialization is unlikely in South Africa,
although that does not rule out some contribution. In con-
trast, some habitats in East Africa where C
4
sedges, such
as the Olduvai Gorge wetlands, are far more common
(Hesla et al., 1982; DeoCampo et al., 2002) likely provided
richer edible C
4
sedge opportunities. The very positive
d
13
C values obtained for P. boisei would be consistent
with heavy utilization of C
4
sedges.
The other possibility considered in Lee-Thorp et al.
(2000)—that of animal foods—has also been more closely
examined. It was envisioned at the outset as a broad cat-
egory comprising insects, lizards, rodents, hyraxes, eggs,
and small antelopes (as suggested originally by Dart
(1926) for the Taung hominin), rather than necessarily
flesh from large vertebrate mammals. It was assumed
that a majority of such animal foods would be enriched
in
13
C, as the bulk of the biomass in savanna environ-
ment derives from C
4
sources. A recent analysis of pred-
ators from all size classes in the Kruger National Park,
South Africa, has shown this to indeed be the case
(Codron, Sponheimer, Lee-Thorp, unpubl. data). These
foods can be acquired by gathering. Baboons are known
to eat grass-eating grasshoppers (Acrididae) (Hamilton,
1987), and grass-eating termites represent another plau-
sible source, particularly since bone tool wear studies
have suggested that they were used for excavating ter-
mite mounds (Backwell and d’Errico, 2001). Savanna ter-
mites are widely distributed and range from C
3
to pure
C
4
consumers, but most consume significant proportions
of C
4
plants, and termites in the Kruger National Park
ate 35% C
4
vegetation on average (Sponheimer et al.,
2005a). Again, it’s unlikely that termite consumption
alone was the source of the strong C
4
signal in australo-
piths because it would require a diet of nearly 100% ter-
mites, or at least, a very large amount of grass-specialist
termites. Thus, termite consumption plausibly contrib-
uted to the d
13
C values of australopiths, but other C
4
resources were almost certainly consumed as well.
Clearly, carbon isotope ratios alone cannot address the
question of the source of C
4
carbon in australopith diets,
or indeed that of the slightly larger C
3
component. One
other possible source of information may come from d
18
O
in enamel apatite. Oxygen isotopes are not usually con-
sidered as dietary but rather as climate indicators, since
the primary input in ecosystems is from environmental
drinking water, which is subject to a range of strong cli-
mate influences (e.g., vapour source, storm paths, tem-
perature, and altitude) (Dansgaard, 1964).
Recent studies have shown that d
18
O from apatite car-
bonate or phosphate can also be influenced by dietary
139BIOGEOCHEMISTRY AND HOMININ DIETS
American Journal of Physical Anthropology—DOI 10.1002/ajpa
ecology (Bocherens et al., 1996; Kohn, 1996; Kohn et al.,
1996; Sponheimer and Lee-Thorp, 1999b). In herbivores
this occurs largely because of the input of oxygen from
plant water and carbohydrates in leaves that are
enriched in
18
O as a result of evapo-transpiration isotope
effects. Consequently, animals such as giraffes that rely
less on free drinking water and feed in the upper canopy
(Cerling et al., 1997) have higher d
18
O values than obli-
gate drinkers in the same environment. Distribution of
d
18
O in bioapatites, unexpectedly, also reflects trophic
behavior. In southern Africa, the faunivores, Otocyon
megalotis,Crocuta crocuta, and Orycteropus afer, are sig-
nificantly depleted in
18
O compared to herbivores in two
modern ecosystems (Lee-Thorp and Sponheimer, 2005).
Low values for faunivores are likely linked to their high
lipid, high protein diets (Sponheimer and Lee-Thorp,
1999b). Suids and many primates also have relatively
lower d
18
O (Sponheimer and Lee-Thorp, 1999b; Carter,
2001).
Australopith d
18
O data from Makapansgat and
Swartkrans overlap with those of carnivores in the same
strata (Lee-Thorp, 2002; Lee-Thorp et al., 2003) (Fig. 6).
Although at first sight, this could be seen as reinforce-
ment of the animal-food hypothesis, it is not that simple.
The causes of the relatively low d
18
O values for many
primates and suids are obscure: they may be linked to
frugivory, the use of underground storage organs, or
water dependence, but given our present limited under-
standing of d
18
O patterning in foodwebs, this is merely
speculative. Clearly there is overlap in the inputs from
different sources and, fuller interpretation of these data
awaits more detailed ecosystem studies.
Despite these uncertainties, we should not lose sight
of a significant finding from these isotope data, namely
that australopiths increased their dietary breadth com-
pared to extant apes by consuming novel C
4
resources,
whatever these resources were. Thus, a fundamental dif-
ference between australopiths and extant apes might be
that when confronted with increasingly open areas, apes
continued to use the foods that are most abundant in for-
est environments (McGrew et al., 1982), whereas aus-
tralopiths began to exploit the novel C
4
resources.
Trace elements
The distribution of trace elements in foodwebs forms
the basis for another important chemical means for trac-
ing diets in the past. Mammals discriminate against the
alkaline earth metals, strontium (Sr) and barium (Ba),
with respect to calcium (Ca) in the digestive tract and
kidneys in a process known as biopurification of Ca
(Spencer et al., 1973; Elias et al., 1982). As a result, her-
bivore tissues have lower Sr/Ca
2
and Ba/Ca ratios than
the plants that they eat, and carnivores in turn have
lower Ba/Ca and Sr/Ca than the herbivores they con-
sume (Elias et al., 1982; Sealy and Sillen, 1988; Burton
et al., 1999). Since Sr and Ba are found in bones and
teeth, where they substitute for calcium in the calcium
phosphate apatite structure, they can in principle be
used to investigate trophic behavior of fossil fauna (Fig.
7). Other trace elements have been applied from time to
time, for instance zinc (Zn), but applications are severely
limited since so little is known about their distribution
in foodwebs and fixation in bone.
There are two major constraints in application of Sr
and Ba to paleodietary reconstruction. One is diagenesis.
Although early researchers were largely unaware of the
extent of the problem (e.g., Toots and Voorhies, 1965;
Fig. 6. Bivariate plot of d
13
C versus d
18
O for A. africanus
and selected fauna from Makapansgat Member 3, shown as
means (boxes) and standard deviations. The hominins (n¼4),
although variable in d
13
C, cluster with Hyena makapania in
both d
18
O and d
13
C.
2
Since Ca is a major element in skeletal tissues, with very high
concentrations, the Sr and Ba composition is usually expressed as a
ratio compared to Ca, ie. as Sr/Ca and Ba/Ca or as log Sr/Ca and log
Ba/Ca.
Fig. 7. The results of the classic trace element discrimina-
tion study of a terrestrial grazing ecosystem in North America.
Sr/Ca and Ba/Ca ratios are plotted on a logarithmic scale (y-
axis), and \soil"is used as shorthand for \soil moisture". This
study was designed to calculate biopurification factors for cal-
cium with respect to strontium and barium uptake. The plant:
vole:pine marten curves nicely illustrate systematic reduction in
Sr/Ca and Ba/Ca in this foodweb, with stronger discrimination
against Ba. This study was subsequently taken as representing
trophic relations everywhere. Data are redrawn from Elias
et al. (1982).
140 J. LEE-THORP AND M. SPONHEIMER
American Journal of Physical Anthropology—DOI 10.1002/ajpa
Wyckhoff and Doberenz, 1968; Brown, 1974; Schoe-
ninger, 1979), it was subsequently widely recognized
(e.g., Sillen, 1981, 1989). Traditionally, archeological and
paleontological trace element studies have been carried
out on bone. This is because infants lack the adult
capacity to discriminate against strontium and barium
(Lough et al., 1963; Sillen and Kavanagh, 1981), and
many teeth are formed in early development. A major
drawback of bone, however, is its susceptibility to post-
mortem chemical alteration (Sillen, 1989; Tuross et al.,
1989) that can quickly obliterate the biological Sr/Ca
signal.
To address the problem, Sillen (1981, 1992) developed
a\solubility profiling"technique based on the premise
that diagenetic apatite has differing solubility to biogenic
fossil apatite. In this technique, highly soluble and
poorly soluble diagenetic apatites are, in effect, stripped
away from the biogenic material and the solutes, not the
solid materials, are measured (Sillen, 1981, 1992). While
ingenious, this method is technically challenging and la-
borious, greatly limiting wider application, but more
importantly, several studies have shown that even when
it is applied, diagenetic strontium often cannot be eradi-
cated from bone and dentine (Budd et al., 2000; Hoppe
et al., 2003; Lee-Thorp and Sponheimer, 2003; Trickett
et al., 2003). This has led to recent attempts to investi-
gate paleoecology using elemental ratios in modern
enamel (Sponheimer et al., 2005a; Sponheimer and Lee-
Thorp, 2006a), which as a denser, far more crystalline
and ordered apatitic tissue (LeGeros, 1991; Elliott,
1994), is much more resistant to postmortem elemental
alteration than bone (Budd et al., 2000; Hoppe et al.,
2003; Lee-Thorp and Sponheimer, 2003; Sponheimer and
Lee-Thorp, 2006a). The problem of poor biopurification
in infants can be easily avoided by analyzing late devel-
oping teeth.
Perhaps a more immediate constraint in current trace
element studies is the requirement for understanding
their very complex pathways in foodwebs, which can
result in significant variation between habitats and
within a trophic level. The importance of local geology in
controlling absolute availability of alkaline earth ele-
ments has been known from the early stages of develop-
ment of the trace element method (Toots and Voorhies,
1965), if sometimes ignored. However, inherent variabili-
ty within trophic levels in ecosystems and indeed within
sympatric species has been largely unappreciated. For
many years trace element paleodietary studies were
based almost entirely on an \archetypal"grazing terres-
trial foodweb study in North America (Elias et al., 1982)
(Fig. 7), and only gradually has the necessity to study
many modern foodwebs, and in more detail, been appre-
ciated. For instance, sympatric browsing and grazing
herbivores can be readily distinguished by their Sr/Ca
and Ba/Ca ratios as can be carnivores and insectivores
(Sillen, 1988; Sponheimer et al., 2005a; Sponheimer and
Lee-Thorp, 2006a), yet the mechanisms that lead to such
differences are at present poorly understood. The key
lies in plant variability as plants, and plant parts (ie.
underground, stem, fruit, leaves) differ considerably in
their strontium distributions due to capillary action in
their vascular systems (Runia, 1987). However, stron-
tium and barium distributions in plants are still poorly
studied. Probably for this reason, coefficients of variation
(CV) for Sr/Ca for a single mammalian species in a sin-
gle location are typically 30–40% (Sillen, 1988; Price
et al., 1992; Sponheimer et al., 2005a). Hence, the natu-
ral variation in mammalian elemental compositions is
such that large numbers of samples are required to
adequately characterize dietary ecology. These problems
are compounded by non-linear relationships between die-
tary and tissue Sr/Ca (Burton and Wright, 1995).
Early hominin diets. The first significant attempt to
investigate the diets of Plio–Pleistocene hominins was
made by Sillen (1992). He found that the bones of Para-
nthropus at Swartkrans had similar Sr/Ca to carnivores
and lower Sr/Ca than primarily herbivorous taxa like
Papio and Procavia (Fig. 8a.) This, in conjunction with
observations from dental microwear (Grine and Kay,
1988) and stable isotopes (Lee-Thorp, 1989) led him to
conclude that Paranthropus was unlikely to be \purely
herbivorous". Subsequently, two bone specimens of early
Homo from Swartkrans were observed to have slightly
higher Sr/Ca than P. robustus (Sillen et al., 1995), a
result that was quite unexpected given the generally
accepted belief that early Homo was the first hominin to
include significant amounts of animal food in its diet
(e.g., Aiello and Wheeler, 1995). Therefore Sillen et al.
(1995) argued that early Homo consumed significant
quantities of strontium-rich underground storage organs,
Fig. 8. Trace element data for the South African hominins
from two studies. (a) shows Sr/Ca data for Paranthropus, Homo,
and a suite of fauna from Swartkrans based on bone analysis,
shown as means (Sr/Ca 31,000) and standard deviations (data
from Sillen, 1992). (b) shows enamel data for A. africanus and
Paranthropus and associated fauna from Makapansgat, Sterk-
fontein, and Swartkans shown as means and standard devia-
tions (data from Sponheimer et al., 2005b; Sponheimer and Lee-
Thorp, 2006a). The data from the three sites were combined
because of the similarity in geology and Sr/Ca ratios for modern
fauna from the Sterkfontein and Makapans Valleys.
141BIOGEOCHEMISTRY AND HOMININ DIETS
American Journal of Physical Anthropology—DOI 10.1002/ajpa
an argument that has since received support from other
quarters (O’Connell et al., 1999; Conklin-Brittain et al.,
2002). As intimated, however, the results from just two
specimens can have no statistical significance given the
inherent variability of the tool.
Concerned about diagenesis, we investigated Sr/Ca and
Ba/Ca ratios in enamel from late forming teeth of modern
and fossil fauna, including hominins from Makapansgat,
Sterkfontein, and Swartkrans (Sponheimer et al., 2005a).
Since these sites share a similar geology, the data from all
three could be combined. The results show that A. africa-
nus had significantly higher Sr/Ca than Paranthropus
and both taxa have higher Sr/Ca than contemporaneous
browsing herbivores and papionins (Fig. 8b). Thus, there
is no reason to believe that Paranthropus consumed
greater amounts of animal foods than contemporaneous
baboons as suggested by (Sillen, 1992). In addition, even if
the Sr/Ca of one or both of these australopith species was
low, it would still provide only limited support for omni-
vory, given our nascent understanding of Sr/Ca through-
out African foodwebs. For instance, diets rich in leaves (as
observed in browsers) also lead to low Sr/Ca, and while a
diet rich in leaves is unlikely for the australopiths given
their extremely low shearing crests (Kay, 1985; Ungar,
2004) and low d
18
O values (see above), we cannot rule out
the consumption of other low Sr/Ca foods. At present we
know very little about the Sr/Ca of different kinds of Afri-
can fruits, although we would expect many fruits to have
low Sr/Ca as has been shown to be the case with tomatoes
(Haghiri, 1964). Consequently, our limited knowledge of
Sr/Ca in plant foods and amongst African savanna mam-
mals, makes detailed dietary interpretation of this Sr/Ca
data difficult.
We have also applied multiple element analysis of
tooth enamel to investigate the diet of A. africanus
(Sponheimer and Lee-Thorp, 2006a). In combination, Ba/Ca
and Sr/Ba ratios suggest that this taxon was signifi-
cantly distinct compared to contemporaneous grazers,
browsers, and carnivores, which were in turn different
from each other (Fig. 9). The Australopithecus fossils are
characterized by high Sr/Ba that is quite distinct from
all other fossil specimens that have been analyzed, sug-
gesting the possibility that they consumed very different
foods than all of these groups, with unusually high Sr
and relatively low Ba concentrations (Fig. 9). One food
that could meet this requirement is grass seeds, another
is underground storage organs (roots, rhizomes, and
bulbs). The evidence for this is indirect, and based partly
on observations that three specimens of African mole rat
(Cryptomys hottentotus), a species which is known to
consume only underground roots and bulbs, had the
highest Sr/Ba of any animal we have studied. The possi-
bilities of both grass seed and underground storage
organ consumption, both of which have been suggested
as possible early hominin foods requires further consid-
eration.
Another potential explanation for the high Sr/Ca of
Australopithecus, and to a lesser extant Paranthropus,is
insectivory. Our modern pilot data show that a modern
insectivore (Orycteropus afer) has much higher Sr/Ca than
carnivores, again emphasizing that not all faunivores are
equivalent in Sr/Ca. Yet, these pilot data also show that
insectivores have high Ba/Ca, unlike the hominins, mak-
ing it less likely that the elevated hominin Sr/Ca results
from insectivory. At present we have analyzed far too few
insectivores to seriously address this possibility.
In summary, although there is clearly ecological pat-
terning to be found in the trace element ratios of early
hominins and associated fauna, interpretation of these
data remains problematic. The difficulty stems from the
lack of work on trace element distributions in modern
African ecosystems. No detailed studies have been pub-
lished that demonstrate the elemental distributions in
African plants and animals, although some promising
work has been carried out in North America (Burton
et al., 1999). The reason is two-fold. In the early days of
trace element studies, there was insufficient appreciation
for the variation that existed in plants and animals, and
therefore it was assumed that trace element ratios sim-
ply reflected trophic level. Later, as researchers became
disabused of this overly simplistic notion, concerns about
diagenesis greatly reduced the time and effort put into
trace element studies. Thus, soon after trace element
analysis was first applied to early hominins in 1992, it
lapsed into virtual disuse except for a few specialized
applications. Now that it has been demonstrated that
trace element compositions retain much of their fidelity
in enamel; studies investigating elemental distribution
in modern foodwebs are urgently required.
Neanderthal diets. Just one trace element application
to the diet of Neanderthals has been carried out based
on Sr/Ca and Ba/Ca ratios of a variety of faunal bones
and a single Neanderthal specimen from Saint Ce
´saire
(Balter et al., 2002). Recently, Balter and Simon (2006)
compared the Sr/Ca, Ba/Ca, d
13
C and d
15
N of the Saint
Ce
´saire individual to other fauna using partitioning
models (Phillips, 2001; Phillips and Gregg, 2003) similar
to that used by Bocherens et al. (2005). They concluded
that this individual ate virtually no plant food and that
its diet was dominated by bovids (71%) with smaller
amounts of horses, rhinos, and mammoths consumed.
Although this is an interesting approach, the results
must be treated with caution. First, only a single Nean-
derthal individual was analyzed, and given the inherent
natural variability of trace elements in ecosystems, very
little can be gleaned about the diets of Neanderthals in
general. Secondly, the study used bone rather than
Fig. 9. Bivariate logarithmic plot of Ba/Ca versus Sr/Ba (3
1,000) for combined fauna and hominins from Makapansgat,
Sterkfontein, and Swartkrans distinguishes Australopithecus
from Paranthropus, although they overlapped in Sr/Ca (Fig. 8).
These data suggest that Australopithecus may have consumed
foods with an unusual combination of high [Sr] and low [Ba]
(data from Sponheimer and Lee-Thorp, 2006a).
142 J. LEE-THORP AND M. SPONHEIMER
American Journal of Physical Anthropology—DOI 10.1002/ajpa
enamel and thus problems due to diagenesis cannot be
discounted. We also know little about geological variabil-
ity in the terrain that might have been used by this indi-
vidual, and geological differences could render the entire
faunal comparison and reconstruction invalid. It must be
said that application of resource partitioning models in
paleo-ecosystems is a risky undertaking. This is because
we cannot know the isotopic and more particularly the
trace element compositions of all potential dietary items,
and this is a requirement of the model which is statisti-
cally based. This is a very significant and inherent limi-
tation given that both plants (and plant parts) and mam-
mals vary widely in these compositions. Application of
trace elements to Neanderthal diets will need a great
deal more basic data to provide a framework that may
eventually inform the broader debate.
COMBINING DIETARY TOOLS
In the preceding sections we provided an overview of
what each of the various dietary tools can and cannot
tell us about hominin diets and gave some pointers to
their relative strengths and weaknesses. For instance,
although the nature of the information obtained from
morphology/allometry and microwear sources primarily
concerns the properties of foods, there are strong differ-
ences in the nature of the observations obtained. Dental
morphology and allometry essentially provides the
broader phylogenetic/historical framework for the prop-
erties of foods a species is capable of eating, while micro-
wear provides more direct information about the effects
of foods actually ingested by an individual. Information
at the level of the individual is important since it ena-
bles intragroup comparisons to be made. Amongst the
biochemical tools, isotope analysis provides quantitative
information at the individual level, facilitating intra-
group and intergroup statistical comparisons. This is not
the case for trace element methods, however, because
very high natural variability restricts available informa-
tion to general group-specific levels, and moreover, the
foodweb pathways are still very poorly understood.
How can we best summarize and combine all this evi-
dence? Or, what are the solid outcomes, where do these
approaches reinforce each other and where are they in
disagreement? In the case of Neanderthals the biochemi-
cal data can be compared mostly with archeological evi-
dence and the single microwear study published so far.
The d
15
N data suggest high trophic level diets for Euro-
pean Neanderthals in the last Glacial. Hence they have
been portrayed as effective top level predators with diets
consisting primarily of meat (Richards et al., 2000;
Bocherens et al., 2005). The d
15
N evidence is consistent
with widespread archeological evidence that suggests
that Neanderthals were efficient hunters, since large
quantities of animal flesh are extremely unlikely to have
been obtained by scavenging. As Richards et al. (2000)
and Bocherens et al. (2005) have argued, this pattern
places Neanderthals and their capabilities in a different
light, contradicting suggestions by some (e.g., Binford,
1981) that they lacked the planning resources required
for efficient hunting of large game as observed in the
Upper Paleolithic. In this case, the isotope evidence has
in effect provided a more radical solution than the arche-
ology in suggesting extreme meat-rich diets. Some prac-
titioners have further exploited the biochemical data,
using multi source mixing models to argue for heavy
reliance of the Saint-Ce
`saire I individual on woolly rhi-
noceros and mammoth based on it’s d
15
N and d
13
C
(Bocherens et al., 2005), while Balter and Simon (2006)
added trace element data in a similar exercise to argue
rather for 60% reliance on bovids. However, while the
conclusions may be seductive, use of such resource parti-
tioning models requires detailed knowledge of the iso-
topic and/or trace element composition of the entire paleo-
ecosystem that we simply do not have. This is a particular
concern for trace element composition given inherently
high variability and susceptibility of bone to diagenesis.
Leaving the trace element data aside, the rather more ro-
bust d
15
N data showing consistently high trophic diets for
Neanderthals would appear to be contradicted by the buc-
cal microwear study showing striation patterns and high
variability more consistent with processing of tough, abra-
sive plant foods and enhancement of abrasion damage in
colder periods (Perez-Perez et al., 2003). However, we also
need to consider the inherent limitations of each of these
approaches; for d
15
N the constraint lies in the bias
towards high protein foods while other explanations may
exist for buccal surface microwear data.
The range of paleodietary methods applied to the
South African hominins provides a good case study for
comparisons, and allows elimination of at least some pos-
sibilities. Some firm results have emerged. For one, the
d
13
C data clearly show that overall both australopith
taxa and early Homo consumed significant proportions of
C
4
or C
4
-derived foods. These results can only be
accounted for by consumption of C
4
grass, C
4
sedges, or
animals which ate these plants, but we cannot tell what
these possibilities are from these data alone. The low
d
18
O is consistent with consumptions of rhizomes or
other roots, as well as animal foods. The microwear data
discounts gelada-like graminivory, since the australo-
piths’ pitted molars (Grine, 1986; Grine and Kay, 1988)
are unlike those of modern geladas whose molar micro-
wear is dominated by scratches (Teaford, 1993). On the
other hand, two recent molar microwear studies of sa-
vanna Papio baboon populations noted a higher frequency
of pitting than was found in Theropithecus (Daegling and
Grine, 1999). These baboons consume moderate amounts
of savanna grasses on a seasonal basis. The trace element
data from australopith tooth enamel showed that Austral-
opithecus, and to a lesser extent Paranthropus,had
higher Sr/Ca ratios than contemporaneous carnivores,
browsers, and papionins. The unusual combination of
high Sr/Ca and low Ba/Ca in Australopithecus has only
been found in modern fauna that heavily utilize the
underground portions of grasses, such as warthogs (Pha-
cochoerus africanus) and African mole rats (Cryptomys
hottentotus) (Sponheimer et al., 2005b). These elemental
data are still preliminary, and certainly cannot be used to
state firmly that early hominins consumed grass rhi-
zomes. Nevertheless, they are entirely consistent with the
possibility and suggest avenues for future research.
Comparing the results from the various techniques
may also give us the opportunity to question some of the
assumptions on which we base interpretations of the
results. For instance, it has been suggested that hominid
dental anatomy was not well suited for the processing of
animal foods (Lucas and Peters, 2000; Teaford et al.,
2002; Ungar, 2004), while the chemical evidence points
towards some consumption of animal foods. It has per-
haps not been appreciated that these anatomical obser-
vations pertain only to a limited class of animal foods
(ie. flesh or meat-eating), while a great many animal
foods require little if any oral processing. Termites,
143BIOGEOCHEMISTRY AND HOMININ DIETS
American Journal of Physical Anthropology—DOI 10.1002/ajpa
grasshoppers, ants, grubs, eggs, and a variety of other
insects may be eaten whole. Soft tissues can also be con-
sumed without oral processing if they can be reduced to
a suitable size through extra-oral means. Moreover, in
some cases apparent disjunctions between dental mor-
phology and actual trophic behavior can result from the
dentition being adapted for other, more mechanically
challenging foods in an animal’s diet. For example, capu-
chin monkeys (Cebus apella) have large, bunodont denti-
tion with thick enamel adapted for consuming fruits and
hard nuts. Nonetheless, close to 25% of capuchin diets
can come from animal foods (Rosenberger and Kinzey,
1976; Fleagle, 1999). Similarly, Grine et al. (2006)
showed that A. afarensis microwear closely resembled
that of gorillas while their dental and enamel morphol-
ogy suggested other affinities. These observations are
consistent with Ungar’s (2004) argument that among
hominoids, differences in dental morphology primarily
reflect their multifarious fallback foods, rather than
their preferred foods during times of plenty.
As for the australopiths, stable isotopes suggest that
they broadened the ancestral ape resource base to
include C
4
foods which, coupled with bipedalism, allowed
them to pioneer increasingly open and seasonal environ-
ments. Yet, there are equifinality problems that are com-
mon in stable isotope and trace element studies. That is,
many different diets can lead to the same stable isotope
(or trace element) composition (Peters and Vogel, 2005).
Although some progress has been made using further
indicators, including d
18
O and trace elements, there is
little reason to believe that this problem can be circum-
vented entirely by relying on chemical means. In the
end, stable isotopes are one tool among many, all of
which provide a slightly different window into the diets
of our ancestors. Stable isotopes will prove most informa-
tive when pursued as part of a larger, integrated paleodi-
etary investigation.
All of these tools also require a great deal of active de-
velopment to improve our understanding of how they
work in ecosystems today. For instance, we still have
much to learn about of the stable isotope compositions of
modern plants and mammals, and how physiology affects
diet-tissue spacing. We must also continue to test com-
fortable assumptions. As a good example, earlier notions
of a simple stepwise trophic system from trace elements
that distinguishes, herbivores, omnivores, and carnivores
has been gradually refined after a series of modern eco-
system studies in different environments (Sillen, 1988;
Burton et al., 1999; Sponheimer and Lee-Thorp, Kruger
National Park Project, unpubl. data). Rather than a sim-
ple trophic level indicator, Sr/Ca and Ba/Ca ratios may
ultimately provide just as much information about plant
foods. Hopefully, such actualistic and experimental work
will serve to further refine the entire suite of paleodiet-
ary tools.
ACKNOWLEDGMENTS
The authors are grateful to their colleagues in the
Transvaal Museum and the University of the Witwaters-
rand for allowing them to pursue their analytical pro-
grammes. They thank Rebecca Ackermann, Thure Cerl-
ing, Daryl Codron, Darryl De Ruiter, Ben Passey, Kaye
Reed, Judith Sealy, Andrew Sillen, Andreas Spa
¨th, Fran-
cis Thackeray, Peter Ungar, and Nikolaas van der Merwe
for helpful discussions over many years.
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... range = -5.4 to -10.0). Although, as noted by Lee-Thorp and Sponheimer (2006) and Cerling et al. (2011), the d 13 C data for both australopith species are more variable than virtually all modern and extinct taxa that have been examined in South Africa, these data might still be brought to bear on the issue of the taxonomic homogeneity of the A. africanus hypodigm. To date, there has been no attempt to relate any of the carbon isotope data to individual specimens as they might relate to the proposed taxonomic groupings. ...
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... de hecho, en la figura 6 se observa que muchos humanos modernos tienen valores δ 15 N todavía más elevados que los Neandertales, lo que se puede interpretar como que los primeros eran al menos igual de dependientes de la carne animal que los segundos (Lee- Thorp y Sponheimer, 2006). Es por esto último por lo que es necesario reconsiderar el papel de la alimentación como factor decisivo en la sustitución de unos homininos por otros en el continente eurasiático. ...
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Durante la última década, los análisis arqueozoológicos que pretenden reconstruir los patrones de subsistencia paleolítica han encontrado aliados en la aplicación de nuevas técnicas: los análisis isotópicos y el estudio de micro-restos vegetales. Los análisis de isótopos estables del carbono y del nitrógeno en colágeno óseo dan información sobre el origen de la proteína consumida de forma constante durante varios años antes de la muerte de los individuos, así como sobre el peldaño trófico de la cadena alimentaria en que los especímenes de estudio se sitúan. El estudio de micro-restos vegetales (fitolitos y granos de almidón) conservados en cálculos dentales y útiles líticos da información sobre el probable consumo de diferentes tipos de plantas por los individuos estudiados. Son ya muchos los especímenes paleolíticos a los que se ha realizado análisis isotópicos para reconstruir la dieta, aunque menos sobre los que se ha aplicado el estudio de microrestos vegetales en cálculos dentales. Se pretende dar a conocer las bases y el potencial de estos dos tipos de técnicas en la reconstrucción de la subsistencia de Neandertales y humanos modernos paleolíticos, así como ilustrar su aplicación utilizando varios yacimientos sobre los que se ha realizado estas técnicas analíticas.
... The disadvantage of this approach is that it does not allow us to do much more than make species-level generalizations: we can say little about intersite variability in behavior and nothing at all as to how behavior might have changed in the face of changing climates and environments. Trace element analysis has provided a valuable alternative and has allowed researchers to make direct inferences about sitespecific variation (Codron et al. 2005;Lee-Thorp and Sponheimer 2006). However, it has, so far, been necessarily confined to observations about diet. ...
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... The latter point is well-supported by archaeological evidence, such as stone tools and cut marks on animal bone recovered from Lower Palaeolithic sites, e.g. Gona and Bouri in Ethiopia, which suggests that our ancestors began processing foods more than two million years ago (Lee-Thorp and Sponheimer 2006). The universality and prevalence of food processing in the present day is also undisputable: all societies in the world practise food processing, regardless of their geographic, ecological and cultural circumstances. ...
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This paper explores the idea that past and present food processing traditions, practiced by modern humans and our Homo ancestors, are tantamount to evolutionary niche construction. It examines how the introduction of simple processing techniques by our Homo ancestors, such as pulverizing and thermal processing (e.g. roasting, baking, boiling), may have triggered radical shifts in their dietary behaviours, which further promoted advances in associated ecological and technological knowledge, skills and tools. It is argued that the consequences of food processing niche construction, e.g. changing dietary selection, increasing diet breadth and improved access to essential nutrients, are of evolutionary significance because they can be linked to changes in the Homo brain and body, as well as increased longevity and disease prevention
... The latter point is well-supported by archaeological evidence, such as stone tools and cut marks on animal bone recovered from Lower Palaeolithic sites, e.g. Gona and Bouri in Ethiopia, which suggests that our ancestors began processing foods more than two million years ago (Lee-Thorp and Sponheimer 2006). The universality and prevalence of food processing in the present day is also undisputable: all societies in the world practise food processing, regardless of their geographic, ecological and cultural circumstances. ...
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... Carbon isotope values of Au. africanus tooth enamel suggest that some 35-40% of the diet of this species consisted of C 4 plants, whereas the predominant component (ca., 65%) was C 3 -based (Sponheimer and Lee-Thorp, 1999a;Lee-Thorp and Sponheimer, 2006). Thus, while Au. ...
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... Perhaps the two most obvious adaptations to emergence of more open landscapes are to be found in locomotor behavior (bipedalism ) and in dietary ecology. Bipedalism is an important defining characteristic of hominins, and although no dietary information is available for very early hominin taxa, it has been suggested that participation in C 4 foodwebs is a consistent feature of later Pliocene hominins, at least (Lee-Thorp et al., 2003; Sponheimer et al., 2005; Lee-Thorp and Sponheimer, 2006). Today, C 4 grasses are a dominant component of many African ecosystems (Sage and Monson, 1999), where they are associated with high solar radiation and warm temperatures during the growing season. ...
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Accumulating isotopic evidence from fossil hominin tooth enamel has provided unexpected insights into early hominin dietary ecology. Among the South African australopiths, these data demonstrate significant contributions to the diet of carbon originally fixed by C(4) photosynthesis, consisting of C(4) tropical/savannah grasses and certain sedges, and/or animals eating C(4) foods. Moreover, high-resolution analysis of tooth enamel reveals strong intra-tooth variability in many cases, suggesting seasonal-scale dietary shifts. This pattern is quite unlike that seen in any great apes, even 'savannah' chimpanzees. The overall proportions of C(4) input persisted for well over a million years, even while environments shifted from relatively closed (ca 3 Ma) to open conditions after ca 1.8 Ma. Data from East Africa suggest a more extreme scenario, where results for Paranthropus boisei indicate a diet dominated (approx. 80%) by C(4) plants, in spite of indications from their powerful 'nutcracker' morphology for diets of hard objects. We argue that such evidence for engagement with C(4) food resources may mark a fundamental transition in the evolution of hominin lineages, and that the pattern had antecedents prior to the emergence of Australopithecus africanus. Since new isotopic evidence from Aramis suggests that it was not present in Ardipithecus ramidus at 4.4 Ma, we suggest that the origins lie in the period between 3 and 4 Myr ago.
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EVOLUTIONARY ANALYSIS OF CONTEMPORARY HUMAN DIETARY preferences is an aggregate science, consisting of several distinct approaches. These include: (1) analysis of early hominid diets; (2) the study of the diets of non-human primate species and possible regulating principles underlying them; and (3) theories concerned with patterns of foraging by animal species in general.