Microwear evidence for Plio–Pleistocene bovid diets from Makapansgat Limeworks Cave, South Africa

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Abstract

Makapansgat Limeworks Cave is a well-known Australopithecus africanus bearing locality that has spawned a considerable amount of paleoecological research because of its hominin component. Most recently, the paleoecology of this Plio–Pleistocene site has been studied by determining the diet and habitat of other extinct taxa, particularly the bovids. The diets of seven bovids (Aepyceros sp., Gazella vanhoepeni, Makapania broomi, Parmularius braini, Redunca darti, Tragelaphus sp. aff. T. angasii, and Tragelaphus pricei) have now been classified using taxonomic uniformitarianism, ecomorphology, stable carbon isotopes, and mesowear analysis. Here, dental microwear is applied to the same bovids for additional comparison and to further elucidate the strengths and weaknesses of each method. The different dietary proxy methods noted provide a temporal continuum, with genetic signals such as ecomorphology and taxonomic uniformitarianism indicating behavioral adaptations over geologic time, while nongenetic data such as stable carbon isotopes and mesowear reflect different aspects of average diet over extended portions of an animal's life, and dental microwear provides dietary snapshots.

Microwear separated an extant baseline of ten bovid species into expected dietary categories and the Makapansgat bovids clearly fell into two groups with the same degree of separation as between extant grazers and browsers. The results indicate that a multidisciplinary approach produces a more accurate and robust reconstruction of past diets. In sum, the microwear analysis is in-line with the isotope and mesowear results, which suggest a stronger browsing component than either taxonomic uniformitarianism or ecomorphology imply.

Introduction

Mammalian paleoecology has traditionally focused on taxonomic uniformitarianism. This method is based on the assumption that fossil taxa evince the ecological preferences of their closest living relatives. While this technique is certainly of some value in analyzing relatively recent faunas, its utility in determining the paleoecology of extinct taxa is questionable. The main problems with this method are that it requires taxonomic groups to remain ecologically constant through time and it provides little or no information about extinct forms with no living relatives (Sponheimer et al., 1999).

A number of techniques have been developed in recent years that take a more empirical approach to dietary reconstruction, such as (1) ecomorphology, or morphological studies that reflect long-term ecological adaptations (e.g., Janis, 1988, Janis and Fortelius, 1988, Solounias and Moelleken, 1993a, Solounias and Moelleken, 1993b, Solounias et al., 1995, Spencer, 1995, Reed, 1996), (2) stable carbon isotopes (e.g., Aufderheide, 1989, Lee-Thorp et al., 1989, Sponheimer et al., 1999, Ambrose and Katzenberg, 2000, Lee-Thorp and Sillen, 2001), (3) dental microwear, the study of short-lived microscopic wear patterns on teeth (e.g., Solounias et al., 1988, Teaford, 1988a, Teaford, 1988b, Solounias and Moelleken, 1993b, Solounias and Hayek, 1993, Rose and Ungar, 1998, Solounias and Semprebon, 2002, Rivals and Deniaux, 2003, Merceron et al., 2004a, Merceron et al., 2004b), and (4) dental mesowear, the study of cusp wear patterns over an extended period of an animals lifetime (e.g., Fortelius and Solounias, 2000, Kaiser et al., 2000, Franz-Odendaal, 2002, Kaiser and Solounias, 2003, Kaiser and Fortelius, 2003, Franz-Odendaal and Kaiser, 2003, Franz-Odendaal et al., 2003, Schubert, in press). Researchers have also combined some of these techniques showing that multiple methods result in more solid paleodietary reconstructions (e.g., Solounias and Moelleken, 1993b, MacFadden et al., 1999, Sponheimer et al., 1999).

A great deal of research has focused on reconstructing the environment of Makapansgat. Methods for interpreting the paleoenvironment of the site have ranged from pollen analysis (Cadman and Rayner, 1989, Rayner et al., 1993, Zavada and Cadman, 1993) to taxonomic uniformitarianism (e.g., Wells and Cooke, 1956, Vrba, 1982) and ecomorphology (Reed, 1996, Reed, 1998). More recent work has focused on testing taxonomic uniformitarianism of bovids by comparing these results to ecomorphology and stable carbon isotopes (Sponheimer et al., 1999). This interdisciplinary study led Sponheimer et al. to suggest that two taxa (Aepyceros sp. and Gazella vanhoepeni), previously thought to be mixed feeders based on taxonomic uniformitarianism and ecomorphology, were in fact browsers.

This paper expands on the work of Sponheimer et al. (1999) by adding an additional proxy measure of diet for the same seven bovid taxa, dental microwear. The primary objectives of this project are: (1) to conduct dental microwear on an extant baseline of bovids with known diets and compare these results with the dental microwear of the Makapansgat bovids, grouping the fossil taxa into dietary categories, and (2) to compare the dietary classifications based on microwear, mesowear (Schubert, in press), stable carbon isotopes, ecomorphology, and taxonomic uniformitarianism for the seven Makapansgat bovids and address the importance of these results for paleoecology.

Section snippets

Makapansgat

Makapansgat Limeworks Cave (24°12′S, 29°12′E) is located northeast of Johannesburg some 15–20 km east–northeast of the town of Mokopane in the Makapansgat Valley, Limpopo Province, South Africa. Member 3 is the main fossil bearing unit at Makapansgat and dates to about 2.5–3.2 Ma based on biostratigraphic (Harris and White, 1979, Vrba, 1982, Delson, 1984) and paleomagnetic evidence (Partridge, 1979, Partridge et al., 2000, Herries, 2003). The faunal assemblage is extensive and diverse, consisting

Bovid diets and paleodiets

Bovids are often used as paleoenvironmental indicators because they are common in many Plio–Pleistocene fossil assemblages and can be readily separated into general dietary categories that reflect habitat preferences (e.g., Sponheimer et al., 1999). These conventional dietary categories reflect the percentages of monocotyledons (monocots) and dicotyledons (dicots) in their diets. The categories are (1) grazers, those species that eat mostly monocots and typically occur in more open habitats,

Dental microwear

The analysis of microscopic wear features on teeth (dental microwear) is considered to be one of the most effective ways of inferring the diets of past vertebrates. Dental wear is the result of abrasion and attrition. In bovids and other artiodactyls, chewing takes place in a one-phase upward and inward occlusal motion. This produces an occlusal surface that is relatively straight labio-lingually. Chewing of this type, also called translatory chewing, requires differential width of upper and

Materials and methods

For the extant bovid baseline analysis, casts of upper and lower second molars of wild caught museum specimens were used (Table 1). The dental molds from these specimens were collected from the American Museum of Natural History (AMNH), New York, the Harvard Museum of Comparative Zoology (MCZ), Cambridge, Massachusetts, the South African Museum (SAM), Cape Town, and the Transvaal Museum (TM), Pretoria. The sampled extant taxa were chosen because they vary widely in ecological preferences, with

Results

A total of 141 specimens from seventeen species were analyzed for dental microwear. Statistical analyses of these results are presented in Table 3, Table 4, and Appendix A.

Discussion and interpretation of results

Microwear results presented here indicate that extant bovids differ in the patterning of microscopic features on the occlusal surfaces of their teeth, which reflect dietary differences in the taxa. The extinct bovids from Makapansgat differ in their microwear features to the same degree as the extants. This presumably reflects similar dietary differences in these taxa.

Comparing dietary proxy measures

The paleodiets of seven Makapansgat bovids have now been analyzed using five different proxy measures. These dietary reconstructions are compared below. Table 5 summarizes the paleodietary interpretations.

Acknowledgments

We thank the curators and collections managers of the mammalogy collections at the Museum of Comparative Zoology (Harvard), American Museum of Natural History (New York), Transvaal Museum (Pretoria), and South African Museum (Cape Town), and the BPI paleontology collection at the University of the Witwatersrand (Johannesburg) for their assistance while making molds in their collections. Further, we thank Daryl DeRuiter and Lee Berger for their help and hospitality while in South Africa. For

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