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Research Letter Dental microwear of Plio-Pleistocene bovids and hominins
Page 1 of 5

© 2016. The Author(s). 
Published under a Creative 
Commons Attribution Licence.

Dental microwear differences between eastern and 
southern African fossil bovids and homininsAUTHORS: 

Peter S. Ungar1

Jessica R. Scott2

Christine M. Steininger3,4

AFFILIATIONS:
1Department of Anthropology, 
University of Arkansas, 
Fayetteville, Arkansas, USA
2Department of Sociology 
and Anthropology, University 
of Arkansas, Little Rock, 
Arkansas, USA
3Evolutionary Studies Institute, 
School of Geosciences, 
University of the Witwatersrand, 
Johannesburg, South Africa
4Centre of Excellence in 
Palaeosciences, University of the 
Witwatersrand, Johannesburg, 
South Africa

CORRESPONDENCE TO: 
Peter Ungar

EMAIL: 
pungar@uark.edu 

POSTAL ADDRESS: 
Department of Anthropology, 
University of Arkansas, 
Old Main 330, Fayetteville, 
Arkansas 72701, USA

DATES: 
Received: 11 Oct. 2015

Revised: 18 Dec. 2015

Accepted: 28 Dec. 2015

KEYWORDS: 
grit; diet; habitat; fossil 
ruminants; tooth wear

HOW TO CITE: 
Ungar PS, Scott JR, Steininger 
CM. Dental microwear 
differences between eastern 
and southern African fossil 
bovids and hominins. S Afr 
J Sci. 2016;112(3/4), Art. 
#2015-0393, 5 pages. 
http://dx.doi.org/10.17159/
sajs.2016/20150393 

Dental microwear has proven to be a valuable tool for reconstructing diets of fossil vertebrates. However, 
recent studies have suggested that the pattern of microscopic scratches and pits on teeth may be more 
reflective of environmental grit than of food preferences. Could differences in dental microwear between 
early hominins, for example, therefore be a result of dust level rather than of diet? We investigated this 
possibility using a palaeocommunity approach. We compared microwear texture differences between 
eastern and southern African Hominini, along with Plio-Pleistocene specimens representing two tribes of 
bovids, Alcelaphini and Antilopini, from the same deposits as the early hominins. If exogenous grit swamps 
diet signals, we would expect community-wide microwear patterns separating samples by region. Results 
indicate that each of the three tribes shows a different pattern of variation of microwear textures between 
eastern and southern Africa. These results imply that differences in microwear reflect diet rather than grit 
load, and that microwear can provide valuable information not just about environmental dust level, but about 
food preferences of fossil vertebrates.

Dental microwear is an important tool for reconstructing diets of fossil vertebrates, from Palaeozoic conodonts1 to 
Plio-Pleistocene hominins2. Microwear researchers have noted consistent and predictable relationships between 
pattern and behaviour in extant taxa from fishes3 to humans4; and these relationships have been used as a baseline 
to infer the diet of extinct species from their teeth. The basic assumption for mammalian cheek teeth has been 
that hard foods are crushed, causing pitting as opposing surfaces are pressed together, whereas tough foods 
are sheared, causing scratches as abrasives are drawn along opposing surfaces that slide past one another.5 For 
example, primates that eat hard nuts and palm fronds tend to have more microscopic dental pits than primates 
that eat tough leaves.6 This diet–microwear pattern association has been used to infer feeding behaviours of many 
fossil species, including early hominins.7

However, a recent study8 has called into question the efficacy of microwear as a proxy for diet, suggesting that 
experimental validation is needed to affirm relationships between pattern and foods eaten. For example, in an in 
vitro wear simulation study, Lucas and coauthors9 found that while quartz dust on foods can easily wear tooth 
enamel, phytoliths within them might not. This finding has led some to suggest that grit in the environment may be 
more important to wear pattern than factors intrinsic to items eaten.10 In fact, Strait et al.8 argued that microwear 
patterns for early hominins may reflect the dustiness of the environment and, ‘say little about the nature of the foods 
themselves’8(p.348). The argument follows that the more striated and less pitted microwear seen for Plio-Pleistocene 
hominins from eastern Africa than those from southern Africa7 may have more to do with where they lived than 
what they ate. This possibility has important implications not only for studies of early hominins, but also for the 
countless other fossil vertebrates for which microwear has been documented and related to diet.11 

Strait et al.8 suggested that quartz dust might cause heavy microwear pitting, and Williams12 opined that exogenous 
grit could lead to especially complex surface textures. These suggestions do not explain the lack of such pitting on 
Paranthropus boisei teeth, which have been suggested to evince extreme macrowear indicative of a gritty, abrasive 
environment.10 But they do raise the question: Is there a consistent relationship between environmental-grit level 
and microwear? While it is clear that soil quartz levels can play an important role in tooth wear13,14, studies of 
mammals living in different settings today have failed to find that grit obscures diet-related microwear signals15.

But what about the differences between Plio-Pleistocene hominins from eastern and southern Africa? If diet signals 
are ‘swamped’ by grit, it should be the case not only for early hominins, but also for other taxa. We predicted that, 
if environmental grit load explains the variation, other large-bodied, terrestrial mammals in the deposits with early 
hominins should show similar differences in microwear pattern between southern and eastern African samples.

We compared dental microwear textures of alcelaphin and antilopin fossil bovids, along with published data 
for hominins16-20 found at the same sites. The bovid data were originally presented in Scott21 and Steininger22 
(see Appendix 1 in the supplementary material). These tribes were selected because they are common at Plio-
Pleistocene fossil sites in both eastern and southern Africa, and because extant representatives have very different 
dietary patterns.23,24 Extant alcelaphins are predominantly grazers, although some consume browse when grass 
is scare. Antilopins, in contrast, include the whole gamut from obligate grazers to obligate browsers; and these 
differences are clearly reflected in dental microwear texture patterns (Supplementary table 1).

Original specimens were cleaned with alcohol-soaked cotton swabs, and microwear impressions were taken 
on first or second molar teeth using President’s Jet regular body polyvinyl-siloxane dental impression material 
(Coltène-Whaledent Inc, Cuyahoga Falls, OH, USA). Replicas were poured using Epotek 301 high-resolution epoxy 
and hardener (Epoxy Technologies, Billerica, MA, USA) and examined for post-mortem damage. Those specimens 
preserving ante-mortem microwear were scanned using the Sensofar plμ standard white-light confocal profilometer 
at the University of Arkansas to obtain point clouds representing four adjoining fields. The lateral (x, y) sampling 
interval was 0.18 μm, vertical (z) resolution was 0.005 μm and field of view for each scan was 138x102 μm. 

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Observable artifacts, such as dust, were deleted electronically and the 
point clouds were imported into ToothFrax (Surfract Corp, www.surfract.
com) to determine area-scale fractal complexity (Asfc) and length-scale 
anisotropy of relief (epLsar). Surfaces with pits of varying sizes tend to 
have high Asfc values, whereas those dominated by aligned scratches 
have higher epLsar values. These variables were chosen because 
previous studies have shown that browsing bovids have higher average 
Asfc values whereas grazers have higher epLsar values.25-27 In fact, 
these attributes together effectively parse extant bovids into Gagnon 
and Chew’s28 fine-scale diet categories29: (1) obligate grazers (>90% 
monocots); (2) variable grazers (60–90% monocots); (3) browser-grazer 
intermediates (30–70% monocots and dicots, including some fruit); 
(4) generalists (>20% of each of the three food types); (5) browsers 
(>70% dicots only, part fruit); and (6) frugivores (>70% fruits). 

Median values of the four scans of each specimen were calculated, 
and the final data set was rank-transformed to mitigate violation of 
assumptions inherent to parametric study (see Scott et al.30 for details). 
A two-factor multivariate analysis of variance (MANOVA) model was 
used to analyse the data, with location (eastern versus southern Africa) 
and tribe (Antilopini, Alcelaphini and Hominini) as the factors, and Asfc 
and epLsar as the variables.

Results showed a significant interaction between location and tribe, 
indicating that the pattern of differences between eastern and southern 
African specimens varied between alcelaphins, antilopins and hominins. 
There was no significant difference in microwear texture between 
southern and eastern African alcelaphins (Tables 1 and 2; Figures 1 
and 2). On the other hand, there was significant variation by location 
for both the antilopins and hominins considered. The differences were, 
however, in opposite directions: antilopins from eastern Africa had 

higher complexity values on average than those from southern Africa, 
whereas hominins from southern Africa had higher complexity averages 
than those from eastern Africa. The hominin pattern holds for both 
Australopithecus and Paranthropus samples.7 

Further, when we superimpose the fossil bovid data on a microwear 
texture plot for extant species (Figure 3), the ranges of values for extinct 
alcelaphins and antilopins from southern Africa overlap primarily with 
variable grazers, whereas that for antilopins from eastern Africa covers 
much of the extant browser space.

These results indicate that fossil alcelaphins, antilopins and hominins 
from southern Africa and those from eastern Africa do not show similar 
differences in microwear textures. Therefore, assuming bovid and 
hominin foods were subject to the same abrasive environments at sites 
within these regions, dust or grit alone does not explain the microwear 
differences observed. Given the mix of grazers and browsers among the 
fossil bovids, and the combination of C3 and C4 isotope signatures of the 
hominins31, it seems likely that these taxa overlapped in feeding height 
and concentration of exogenous abrasives on food. Further, the fact 
that the distributions of microwear texture values for fossil and extant 
samples closely approximate one another for both the antilopin and 
alcelaphin tribes (compare Figure 2 to Supplementary figure 1) further 
supports the idea that differences between southern and eastern African 
hominins are not explained by grit or dust load. Finally, while it is possible 
that differences in masticatory biomechanics, mineralisation and enamel 
microstructure could complicate interpretations of differences in patterns 
seen between hominins and bovids, it is unlikely that these explain the 
differences between the antilopins and alcelaphins given that microwear 
differences so strongly mirror diet differences in extant species of these 
tribes (Supplementary figure 1). 

a

c

b

Figure 1: Sample photomicrowear simulations for specimens from southern Africa (left) and eastern Africa (right) representing (a) Alcelaphini, (b) Antilopini 
and (c) Hominini. Each surface represents an area 138x102 μm.

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a

c

b

Figure 2: Anisotropy (epLsar) versus complexity (Asfc) plots for the fossil 
(a) Alcelaphini, (b) Antilopini and (c) Hominini. Eastern African 
specimens are clear and southern African ones are solid. 
Original data for all individual specimens are presented in 
Appendix 1 in the supplementary material. 

Table 1: Mean (s.d.) for microwear attributes by tribe and location

Eastern Southern

Asfc epLsar n Asfc epLsar n

Alcelaphini 1.873 (0.608) 0.005 (0.002) 44 1.788 (0.701) 0.005 (0.002) 27

Antilopini 3.349 (1.144) 0.003 (0.001) 30 1.772 (0.719) 0.004 (0.002) 20

Hominini 0.964 (0.676) 0.003 (0.002) 47 2.067 (1.417) 0.003 (0.002) 26

Table 2: Summary of results of the multivariate analysis of variance 
(MANOVA†) 

 Value F d.f. p

Interaction 0.938 3.062 4, 37 0.017

Antilopini 0.979 0.740 2, 68 0.481

Alcelaphini 0.565 18.062 2, 47 0.000

Hominini 0.712 14.171 2, 70 0.000

†A two-factor MANOVA model was used to analyse the data, with location (eastern 
versus southern Africa) and tribe (Antilopini, Alcelaphini and Hominini) as the factors, 
and Asfc and epLsar as the variables.

a

b
Obligate grazer
Variable grazer
Generalist
Browser-grazer
Browser
Frugivore

Figure 3: Anisotropy (epLsar) versus complexity (Asfc) plots for the 
fossil (a) Alcelaphini and (b) Antilopini compared with baseline 
specimens, with diets as indicated in the legend (extant bovid 
data from Scott29). The space represented by eastern African 
fossil specimens is depicted by the red polygon, whereas 
that represented by the southern African fossil specimens is 
depicted by the blue polygon. The polygons were constructed 
by connecting the farthest separated data points on both axes.

In sum, while grit undoubtedly impacts tooth wear9,13,14, the lack of a 
consistent location signal among the tribes suggests that differences 
in microwear between eastern and southern African hominins are likely 
not a result of abrasive load alone. Diet remains the most plausible 
explanation for the variation in dental microwear among species. 
While Sanson et al.32 and Lucas et al.9 argued that exogenous grit is 

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the operative wear agent for teeth because endogenous silicates within 
plant foods (phytoliths) are softer than enamel, it is clear that there is 
more to tooth wear than abrasive hardness. Because hydroxyapatite 
crystallites are attached to one another by a thin layer of protein ‘glue’, 
tissue removal requires only that contact pressure be sufficient to break 
the bonds holding enamel together. Indeed, tissue removal is achieved 
with particles much softer than enamel.33 In this light, it makes sense 
that primates known to consume phytolith-rich foods tend to have 
thicker tooth enamel34, that tell-tale siliceous plant opals have been 
found embedded in tooth enamel at the ends of microwear scratches35, 
and that experimental studies show cereals with different phytolith loads 
leave different microwear patterns36. 

Acknowledgements
The hominin data were collected originally in collaboration with 
Robert Scott, Fred Grine, Mark Teaford, Kristin Krueger and Alejandro 
Pérez-Pérez. Funding for data collection came from the US National 
Science Foundation (P.S.U. and J.R.S.) and the South African National 
Research Foundation, DST-NRF Centre of Excellence in Palaeosciences 
and Palaeontological Scientific Trust (C.M.S.). We thank three 
anonymous reviewers and Francis Thackeray for their helpful comments 
on an earlier version of this manuscript, and the curators at the various 
museums who allowed us to study specimens in their care.

Authors’ contributions
P.S.U., J.R.S. and C.M.S. gathered the data, analysed the results and 
wrote the manuscript. P.S.U. was the project leader.

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Note: This article includes supplementary material

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